Advanced Coastal Navigation
Coast Guard Auxiliary Association Inc. Washington, D. C.
First Edition...... 1987 Second Edition ...... 1990 Third Edition ...... 1999 Fourth Edition...... 2002
ii iii iv v vi Advanced Coastal Navigation
TABLE OF CONTENTS
Introduction...... ix
Chapter 1 INTRODUCTION TO COASTAL NAVIGATION ...... 1-1
Chapter 2 THE MARINE MAGNETIC COMPASS ...... 2-1
Chapter 3 THE NAUTICAL CHART ...... 3-1
Chapter 4 THE NAVIGATOR’S TOOLS & INSTRUMENTS ...... 4-1
Chapter 5 DEAD RECKONING ...... 5-1
Chapter 6 PILOTING ...... 6-1
Chapter 7 CURRENT SAILING ...... 7-1
Chapter 8 TIDES AND TIDAL CURRENTS ...... 8-1
Chapter 9 RADIONAVIGATION ...... 9-1
Chapter 10 NAVIGATION REFERENCE PUBLICATIONS ...... 10-1
Chapter 11 FUEL AND VOYAGE PLANNING ...... 11-1
Chapter 12 REFLECTIONS ...... 12-1
Appendix A GLOSSARY ...... A-1
INDEX ...... Index-1
vii Advanced Coastal Navigation
viii intRodUction
WELCOME ABOARD!
Welcome to the exciting world of completed the course. But it does marine navigation! This is the fourth require a professional atti tude, care- edition of the text Advanced Coastal ful attention to classroom presenta- Navigation (ACN), designed to be tions, and diligence in working out used in con cert with the 1210-Tr sample problems. chart in the Public Education (PE) The ACN course has been course of the same name taught by designed to utilize the 1210-Tr nau - the United States Coast Guard tical chart. It is suggested that this Auxiliary (USCGAUX). Portions of chart be readily at hand so that you this text are also used for the Basic can follow along as you read the Coastal Navigation (BCN) PE text. We recognize that students course. ACN is now used internally from all areas of the United States by USCGAUX as the navigation enroll in the course and that a better text in their member training classes. geographic “balance” to the exam - PE students who successfully com- ples might be attractive. Where nec - plete the ACN course (including essary as, for example, in the discus - necessary examinations) and who sion of polyconic charts of the Great elect to join are credited with com- Lakes in Chapter 3, illustrations pletion of the USCGAUX course. from other areas of the country are This fourth edition builds upon included. But the 1210-Tr chart con - the first three editions of this same tains a wide variety of features of text but has been updated to reflect interest to the navigator and, more - the helpful advice of numerous ded- over, contains a useful summary of icated USCGAUX instructors, stu- chart symbols printed on the reverse dent feedback, and recent technical side for ready reference. In short, developments in the field—particu- this is an ideal training chart. larly in the area of electronic navi - The ACN text has been designed, gation. Graphics and layout have for the most part, to teach you the been substantially improved from “classical” methods of coastal navi- earlier editions. gation applicable to small vessels. The ACN and BCN courses are Shortcuts, such as might be taken for not intrinsically difficult, nor do they routine cruises in very familiar have advanced educational require- waters, are men tioned only briefly. ments. Students from many walks of Experience, sometimes called the life and of widely varying education- “seaman’s eye”, teaches the naviga- al backgrounds have suc cessfully tor which shortcuts can safely be
ix Introduction
taken and under what circum- requires only seconds on a laptop ers who have a technical back - stances. But the basis for shortcuts computer? The answer is very sim - ground and are interested in a more should rest on a firm foundation/ ple. First, not all vessels are complete and detailed exposition. mastery of “the text book solution,” equipped with the latest in marine Students who lack the necessary and not simply arise from laziness, electronics; students come to the background or interest can omit lack of knowledge, or being out of ACN/BCN course owning every - these sections without loss of conti - practice. thing from runabouts equipped with nuity. Material so identified is not Over the past few years there little more than a compass to large included in the final examination for have been revolutionary develop- yachts equipped with virtually the the PE course, but may appear on ments in the field of marine elec- entire contents of one of the numer- the USCGAUX navigation course tronics. Modern Global Positioning ous catalogs of purveyors of marine examination. Additionally, a list of System (GPS) or Loran-C receivers, electronics. The ACN/BCN course ref erences is appended to chapters the fluxgate compass, radar, fuel is designed for skippers of both of for those who wish to learn more flow meters and computers, elec- these types of vessels. Second, and about particular topics. Sidebars are tronic charts, and autopilots serve as perhaps more important, even if a used to set off sum maries, provide examples. These devices, tied vessel is equipped with the latest in highlights, and add items of his - together with onboard navigational navigation systems, the reliability of torical interest that would otherwise computers, have revolutionized seaborne electronics is still far from disturb the flow of the narrative. both the art and science of marine perfect. The classical methods of Perhaps surprisingly, several navigation. Today it is literally true navigation are required to moni tor aspects of navigation (generally that, by merely pressing a few but- the performance of even the best- those relating to the “art” of naviga - tons, you can program an entire equipped vessel. And, should these tion) are controversial. For exam ple, voyage and simply sit back, watch systems fail, classical meth ods can there are those who advocate that all for traffic and be prepared to dock be used to bring you home safe and plotting should be done with respect the vessel at the conclusion of the sound. to magnetic, rather than true north. voyage. Alarms warn of the ACN does include material on Although this text takes a position approach of vessels within a prede- more sophisti cated marine electron- on many of these points of contro- fined exclu sion zone, passage into ics, such as GPS, Loran-C, and versy, books or articles that espouse shallow water, and arrival at way- radar. The coverage is not designed a contrary point of view are includ- points or the final destination. Once, to teach you how to operate any par- ed among the references. Therefore, such an “electronic voyage” would ticular make or model but, rather, to the student should not assume that have come from the dreams of Jules acquaint you with the general prin - either the United States Coast Guard Verne, or been impossibly out of ciples and techniques so that you (USCG) or the USCGAUX specifi- reach for most boaters. But recent can make better use of whatever cally endorse any work listed in the advances in the state of the art of equipment you own or elect to pur- references. These are included to marine electronics have brought sci- chase. add balance, perspective, and inter- ence fiction into the realm of the ACN also con tains a novel chap- est. Likewise, any mention or inclu- possible and affordable. ter on fuel plan ning, a subject usual- sion of pictures of particular makes These modern miracles have led ly given short shrift, or omitted or models of equipment does not some students to question the role of entirely, in the typ ical text on navi- imply that these are recommended classical methods of coastal nav - gation. Unfortunately, fuel starva- or endorsed by USCGAUX or igation, such as the use of visual tion and/or fuel exhaustion cause all USCG. fixes, dead reckoning plots, and the too many preventable Search and Thanks to the many firms like. Why, after all, learn the tedious Rescue (SAR) cases. that supplied pictures and/or proce dures required to calculate tide Several sections of this text are illustra tions for use in this text. height or tidal current, for example, identified as “more technical.” This Acknowledgments are included in when an hour-by-hour calculation material is included for those read - the caption for each illus tration. x Introduction
Although theory is not slighted, material is so valuable, and we apol- Remember that you have the the emphasis in the text is on prac - ogize in advance if the information choice of being the operator of tical, time-tested approaches to nav - referenced is not available. your vessel or merely an igation. The text contains numerous This text contains a glossary of occupant. Knowledge, skill, and discussions of practical methods terms, given in Appendix A. experience are required to trans form and numerical examples to provide Readers encountering an unfamiliar occupants into competent operators. a firm foundation in the art and sci- term or abbreviation may wish to Remember, also, that each voyage ence of coastal navigation. consult this appendix for a brief should be a learning experi ence. In In recent years, the amount of explanation. this sense, all of us should be per- useful material posted on the Each page of the logbook of petual students. Internet has increased substantially. Christopher Columbus was headed May you always have fair skies, Web Site addresses are included as with the title Como Dios Manda (As calm seas, fair currents, and follow- references at various points in the God Ordains), which was testi mony ing winds. But, more important, text. These addresses were valid at both to his religious faith and to the may you learn how to navigate safe - the time that this edition went to primitive state-of-the-art of naviga- ly and efficiently regardless of sea press. Addresses change, as does the tion at the time. This book is dedi- or wind conditions. material posted. We opted to include cated to the notion that you should this information, despite possible also have a hand in the out come of a changes, because the supplementary voyage.
xi Introduction
xii Chapter 1
INTRODUCTION TO COASTAL NAVIGATION
“And after this sort he proceedeth from place to place until he arrive unto his desired porte, which is a conclusion infallible if there be no other impediments (whereof there hath been good consideration had) which may breed errour, for from such negligence may arise many inconveniences.”
–The Seaman’s Secrets by John Davis, 1607, as quoted in Schofield, The Story of HMS Dryad
hat is coastal navigation? In equipment, such as the employment Wsimple terms, marine naviga - of methods to fix the vessel’s posi- tion is “getting your vessel from tion from observation of the sun, where you are to where you want to moon, or stars, coastal navigation go, safely and efficiently.” More often demands a greater degree of formally, it is the “process of direct - accuracy and attention to detail. On ing the movement of a vessel from a long ocean passage, for example, one point to another.” It is derived it may suffice to deter mine the ves- from the two Latin words, navis sel’s position only once or twice a (ship), and agere (to move). Coastal day, and to within a margin of navigation refers to navigation in uncertainty of several square miles. coastal (sometimes termed pilot) A well-found ocean going vessel waters, where the opportunity may afford the naviga tor a dry exists to determine or check the workstation, and numer ous elec- vessel’s position by refer ence to tronic aids, such as the Global navigational aids and obser vations Positioning System (GPS) receiver (by either visual or elec tronic and radar. A passing vessel would means) of the coast and its features. be a curiosity in seldom trav eled Coastal navigation is dis tinguished waters, rather than an object for from “blue water” or ocean naviga- collision-avoidance maneuvers. In tion, terms used to describe naviga- coastal waters, particularly in nar- tion out of sight of land and/or row channels, position fixes might coastal Aids to Navigation be required every 5 to 15 minutes, (ATONs). Although blue-water and required accuracy lim its could navigation may appear to require well be measured in yards. The more sophisticated techniques and navigator’s workspace could be
1-1 1 Introduction to Coastal Navigation
cramped, and the vessel’s naviga - Massachusetts, on Vineyard Sound sequences that are important for tional gear limited to a hand-bear- (at the far right of the chart). recognition and identification pur - ing compass. All this is to be done It is convenient to subdivide poses), while the USCP provides while dodging “heavy iron” (large navigation into two distinct, but useful “local knowledge” in narra - vessels) in busy shipping channels. related phases: voyage planning tive form. For example, following a and underway navigation. The route from Tiverton through
ST G A U O planning phase covers the initial A Buzzards Bay would require a tran - C R
S D What you Will U
A U Y X R ILIA learn in this shoreside paper-and-pencil or sit of the channel between Buzzards (increasingly) computer chores, and Bay and Vineyard Sound. The Chapter ends when the vessel’s anchor is USCP offers the following com - J How the course is weighed or the mooring lines are ments about this area: organized slipped. Underway navigation cov - “The passage through J Principles of voyage ers navigation and decision making Woods Hole, between planning and underway on the water. The overall steps in numerous ledges and shoals, navigation each phase are discussed below. is marked by navigational aids. However, tidal currents J Coordinate systems STEPS IN are so strong that the passage (latitude and longitude) VOYAGE PLANNING is dif ficult and dangerous J Measurement of Figure 1-1 highlights the princi - without some local knowl- direction pal steps in voyage planning. It edge. Buoys in the narrowest starts with the assembly of required part of the channel some- AN OVERVIEW reference materials and trip and times are towed under, and a OF THE COURSE vessel data. Such materials include: stranger should attempt pas- J Up-to-date (and corrected) nau- sage only at slack water.” This section provides an Such information is obviously overview of the Advanced Coastal tical charts at the right scale (discussed in Chapter 3), invaluable for planning purposes. Navigation (ACN) course in the Tide Tables are used to estimate J Tide and Tidal Current Tables context of the navigator’s tasks on a the height of the tides that would be and related materials (discussed typical voyage in coastal waters. To encountered on the voyage to in Chapter 8), make the discussion concrete, sup - ensure that a safe route is chosen. pose that you are the navigator for J Navigation reference materials, Tidal Current Tables provide infor - the 42-ft. trawler, Verloren, on a such as the Light List (LL), U. S. mation on the strength and direction voyage from Tiverton, on the Coast Pilot (USCP), and of the currents, information used to Sakonnet River in the state of J Cruising guides to the area (dis- estimate the vessel’s ground speed Rhode Island, to Woods Hole, cussed in Chapter 10). and the selection of the correct Massachusetts, approximately 40 The nautical charts are used to course to compensate for these cur- miles distant. This area is covered lay out the voyage, measure dis - rents. by the 1210-Tr chart, which is dis- tances and courses, identify land - Other information requirements tributed with the course materi als. marks or ATONs that will be used include operating data for the ves - Reach for this chart now (the first to fix the vessel’s position, ensure sel, such as the relation between of many times that you will be engine revolutions per minute called to do this in the chapters that the course avoids hazards to (RPM) and the speed through the ahead) and locate the place of navigation, and for many other pur - departure on the voyage, Tiverton poses. water (discussed in Chapter 5), and (roughly in the middle of the chart, The Light List is consulted to fuel capacity and consumption data near the top), Rhode Island, and the determine the characteristics of the (presented in Chapter 11). For destination, Woods Hole, relevant ATONs (such as color or example, at 2250 RPM, Verloren light characteristics and horn might make 8 knots (nautical miles
1-2 Introduction to Coastal Navigation 1
ASSEMBLE REQUIRED recreation, or fuel. Even for this distance (TSD) calculations are REFERENCE MATERIALS “simple” trip, there are several reviewed in Chapter 5, fuel con - alternatives that might be consid - sumption calculations in Chapter ll, ered. Time spent developing and the somewhat more com plex FORMULATE VOYAGE thoughtful voyage options is time task of allowing, and compen sating, ALTERNATIVES well spent. A good navigator thinks for currents in Chapter 7. and plans ahead, so that he/she Estimation of the probable currents doesn’t have to exercise extraordi - is discussed at length in Chapter 8, EVALUATE ALTERNATIVES nary seamanship! If, for example, As it happens, the currents in the more northerly route through Buzzards Bay and Vineyard Sound Buzzards Bay is chosen, the trip are often moving in opposite direc - schedule has to be worked out to tions, at speeds ranging from less SELECT BEST VOYAGE PLAN & PREPARE FLOAT PLAN minimize the hazards of transiting than one knot to 2 knots or more. the channel between Buzzards Bay So, depending upon the current pat - and Vineyard Sound. To someone terns prevailing on the day and time unfamiliar with these waters, the of the voyage, the two routes identi - COMPLETE PRE-UNDERWAY VESSEL CHECKS USCP indicates that it would be fied above could have significantly prudent to make this transit during different ETEs. daylight hours at or near slack cur - Moreover, as illustrated in rent. This can and should be figured Chapter 8, it is entirely possible that WEIGH ANCHOR out in advance, rather than “come the longer distance route would also upon” in failing light. be the shorter time route. As noted, L The third step in voyage plan - the length of the Buzzards Bay FIG. 1-1–Steps in Voyage Planning ning is to evaluate systematically route is approximately 37.5 miles, the alternatives identified in step compared to 40 miles for the per hour), and burn 7 gallons per two. Obviously, two important fac - Vineyard Sound route. But if the hour (GPH) of fuel from tanks that tors relevant to the voyage are average current along Vineyard can hold 400 gallons when topped Verloren’s speed and the distance to Sound were, say, 2 knots in the off (filled). be covered along each of the alter- direction of intended travel (a so- The second step in voyage plan - native routes. This distance is deter- called fair current), and that in ning is to consult the materials mined from a rough plot of the Buzzards Bay were 0.6 knots assembled and formulate voyage alternate routes on the nautical against the direction of travel (a so- options for later evaluation. Voyage chart by techniques revealed in called foul current), the time options relevant for this trip would Chapter 3. In this case, the route required for the trip through include the overall route to follow through Buzzards Bay (ap - Vineyard Sound would be approxi - (east through Buzzards Bay, or proximately 37.5 miles for one pos - mately 4 hours, compared to nearly south, then east through Vineyard sible route layout) is slightly short - 5 hours on the “shorter” route. (This Sound are obvious alternatives), er than that through Vineyard calculation must be refined to take departure time (which affects the Sound (approximately 40 miles). account of the fact that the first leg water currents and tide heights that Speed and distance determine the is common to both routes. Even a will be encountered and also how en route time required for the voy - more exact calculation, however, much of the voyage will be con - age (5 hours estimated time en route shows that the longer distance route ducted during daylight hours), the (ETE) to cover 40 miles at 8 knots is the shorter time route.) This ex - speed to be run (which affects the assuming no current), and the fuel ample is not hypothetical—the estimated en route time, fuel con - consumption (35 gallons required, assumed currents are, in fact, the sumption, and arrival time), and assuming 5 hours en route at 7 gal - estimated currents at one point in planned stopovers for amenities, lons per hour). Simple time-speed- the tidal current cycle. Additionally,
1-3 1 Introduction to Coastal Navigation
the Vineyard Sound route avoids the availability of suitable land - ing direction, speed, and, occasion - the trip through the channel next to marks or ATONs to fix the vessel’s ally, distance) and future positions Woods Hole. This benefit may not position or to mark channels all (termed dead reckoning positions) be important to someone with local need to be considered. Discussion at various times in a stylized for - knowledge, but might be a decisive of these important matters can be mat. The DR plot is maintained and factor otherwise. found scattered throughout this text updated throughout the underway For this voyage in Verloren, fuel in the examples used to illustrate portion of the voyage. certainly won’t be a problem, key points. The fifth step in voyage plan - assuming that the tanks are even The fourth step in voyage plan - ning is to complete prevoyage near to being full prior to departure. ning is to select a plan that is “best” checks on the vessel and its equip- But for longer trips, or in vessels in some sense, considering the ves - ment—much as aircraft pilots do in with higher fuel consumption or sel, navigational equipment aboard, the preflight inspection. For exam - lower fuel capacity, fuel planning is skill and local knowledge of the ple, the navigator would verify that often a singularly important activi - navigator and crew, and other rele - all communications and navigation ty. For vessels with what are termed vant factors. Included here is the equipment were functioning prop - “short legs” (limited fuel capacity), important task of making a “float erly and that the correct charts and fuel stopovers would need to be plan” that describes the route and other reference materials were considered, and/or the engine throt- estimated time(s) of arrival so that aboard. Weather information should tle setting altered to stretch fuel the Search and Rescue (SAR) per - be gathered and used as part of the reserves. sonnel can be promptly alerted if “go-no-go” decision. If all goes you become overdue. (The float well in this step, it is time to start plan should also include a descrip - engines, slip Verloren’s dock lines, tion of the vessel, number of per - note the departure time in the navi- sons on board, available safety and gator’s or ship’s log, and get under- radio equipment, and other relevant way. information.) The float plan is left in the care of a responsible person, STEPS WHILE UNDERWAY with instructions to notify the Coast Guard in the event that the vessel Figure 1-2 shows a simplified becomes overdue. The navigator summary of the key underway often prepares a more detailed voy - activities. As noted above, the navi - age plan in this step, identifying gator estimates the future position of the vessel at various times using
PHOTO PHOTO COURTESY OF MAINSHIP checkpoints and turnpoints for each L leg of the trip, courses to steer, time DR (see Chapter 5). But, these esti - A trawler moving serenely through the estimates, and fuel consumption mates are not error free. Neither water. The material in this course will estimates. wind nor current, for example, is enable you to navigate such vessels In this fourth step, the navigator considered in the determination of DR positions—for reasons that are with confidence. also plots the first “legs” (route seg - ments) of the voyage on a tactical apparent on reading Chapter 5. Option evaluation is not limited (underway) dead reckoning plot Therefore, it is very important to to questions of time, speed, or fuel (DR plot). Dead reckoning (DR), check and update the actual consumption. Many other factors explained in Chapter 5, is the name progress of the voyage at frequent need to be considered. For example, given to the process of predicting intervals in coastal waters. This is the difficulty of transiting channels the future position of a vessel from done with a series of “fixes,” points or inlets, availability of “bolt knowledge of its present (or start - in time at which the vessel’s posi - holes” (safe places to anchor or ing) position, the course steered, tion is accurately determined. moor in the event of mechanical and the speed maintained. A tactical The vessel’s position can be problems or adverse weather), and DR plot shows course legs (includ- fixed by three principal methods.
1-4 Introduction to Coastal Navigation 1
J First, visual observation of the START range or bearing of landmarks or ATONs can determine its position. For example, the navi - gator could determine the mag - UPDATE DR netic bearing of the abandoned PLOT lighthouse on Sakonnet Point, and that of the tower on Gooseberry Neck, which could SEARCH FOR fix Verloren’s position by tri - FIX OPPORTUNITIES angulation if the Buzzards Bay route were taken. This method FIX VESSEL’S for position fixing is termed POSITION piloting, and is discussed in Chapter 6. J Second, the vessel’s position can be fixed by use of electron- ELECTRONIC PILOTING CELESTIAL ic navigational systems, such as NAVIGATION GPS, loran, or radar. For exam - USE VISUAL USE SHIPBOARD ple, GPS could be used to read METHODS OBSERVATIONS the vessel’s latitude and longi - ELECTRONICS tude directly. Alternatively, radar could be used to measure the range and bearing to a rec - ognizable landmark. This is COMPARE FIX WITH COMPUTE termed electronic navigation, DR POSITION CURRENT SET & DRIFT and is discussed in Chapters 6 and 9. L J Third, the position of the ship FIG. 1-2–Steps in Underway Navigation can be fixed by observation of the angle (elevation) of heaven - ly bodies (here meant to mean fix with the vessel’s DR position siderably. In practice, the navi - the sun, moon, or stars). This can be used as a “plausibility” or gator’s underway tasks are often process is termed celestial navi - “reality” check on the fix and the more complex and varied. For gation. For various reasons, DR position. Absent blunders, any example, instead of merely estimat- including the limited opportuni - discrepancy between the fix and the ing the set and drift of the current, ties for fixes, and the possible DR position is due to current, so a the navigator would usual ly esti- error of celestial fixes, celestial comparison of these two positions mate a course (by the methods dis- navigation is not extensively can be used to estimate the actual cussed in Chapter 7) to compensate used in coastal waters and is not currents (the term set refers to the for these effects and ensure that the presented in this text. direction toward which the current vessel stays in safe water. On such a Once a fix is determined, this is is flowing, and drift refers to the short voyage, as is illustrated here, plotted on the tactical DR plot (see speed of the current) encountered en route decision making may be Chapter 5) and the plot is updated (the method for estimating set and relatively simple. But on other trips, with this fix. (The data for this fix drift is discussed in Chapter 7). the navigator would be continually are also entered into the navigator’s For introductory purposes, revising fuel consumption estimates or ship’s log.) A comparison of the Figure 1-2 has been simplified con- and the estimated time of arrival
1-5 1 Introduction to Coastal Navigation
in this text. Of course, not all voy- poles and bulges in the middle, as ages are sufficiently long or com- opposed to a prolate spheroid plex to require the formal use of all which resembles a football; but the techniques discussed above. For don’t go calling it prolate spheroid short voyages in familiar and well- ball, or you will wind up being marked waters, and when weather called an oddball!), but the differ- conditions are close to ideal (e.g., ence between the earth’s actual moderate seas, calm winds, and shape and that of a perfect sphere is good visibility), various short cuts not important for this course. The can be taken to simplify the naviga- average diameter of the earth is tor’s duties. This is termed naviga- approximately 6,880 nauti cal miles, tion by seaman’s eye and is and its circumference is approxi- PHOTO COURTESY OF UNITED STATES COAST GUARD COAST PHOTO COURTESY OF UNITED STATES addressed in Chapter 11. L mately 21,614 nautical miles. Since Navigation of high-speed vessels is there are 360 degrees (denoted with Navigation of faster boats and/or navi- both simpler and more difficult. the degree symbol °) of angular gation in rough waters requires greater Currents are less of a factor for measure in a circle, 1 degree of preplanning. Here is a United States high-speed vessels and these com- angular measure along the earth’s Coast Guard 44-ft patrol boat crashes putations are usually omitted. surface is approximately 60 nauti- through a wave. There is little time or However, there is less time to use cal miles. Degrees are fur ther sub- space to plot positions exactly. traditional methods and more pre- divided into minutes (denoted with planning is required. Navigation of (ETA). These revised estimates high-speed vessels is covered an apostrophe, e.g., 30 minutes is could signal the need to change the briefly in this text. written 30’), and sec onds (denoted voy age plan. For example, the In the above discussion, the con- with two apostro phes, e.g., 40 sec- discov ery that fuel consumption tents of two chapters were omitted. onds is written 40”). There are 60 was significantly higher than Chapter 2 covers the minutes in a degree (and 60 seconds planned could mean that the vessel marine magnetic compass, would have to be diverted to an and Chapter 4 provides a alternate destination. summary discussion of the NORTH NORTH MAGNETIC GEOGRAPHIC The navigator should also check navigator’s tools (other POLE POLE the accuracy of the navigation than the vessel’s compass). equipment in use by comparing, Before moving on to whenever possible, fixes deter - some of the interesting mined by various methods. For material in the chapters example, a comparison between an ahead, it is necessary to accurate visual fix and one deter - address two important intro- WEST EAST mined by GPS or Loran-C could be ductory topics: the earth’s EQUATOR used to verify that these systems coordinate system and were functioning properly. measure ment of direction. Likewise, a prudent navigator would make periodic checks on the BACK TO BASICS: accuracy of the vessel’s compass, THE PLANET EARTH perhaps by spot checks of the com- The earth is approxi- pass’ deviation table, as explained mately spherical, as illus- SOUTH SOUTH in Chapter 2. GEOGRAPHIC MAGNETIC trated in Figure 1-3. POLE POLE There you have it—a brief illus- Technically, the earth is L tration of the various navigator’s termed an oblate spheroid FIG. 1-3–The Earth and Its Poles tasks and where these are addressed (a sphere flat tened at the
1-6 Introduction to Coastal Navigation 1
in a minute), so 1 minute of angular GREAT AND measure is approximately equal to 1 SMALL CIRCLES nautical mile. A plane passed The earth rotates about a straight through the cen ter of the line called the axis of rota tion, or earth separates the earth polar axis. The earth com pletes one into two hemispheres, rotation every 24 hours (the solar and inter sects the surface day). The axis of rotation passes of the earth to pro duce a through the center of the earth, geometric figure termed a intersecting the surface at two great circle. On the sur- points, termed the north and south face of a sphere, the geographic poles (denoted Pn and shortest distance between L Ps, respectively). The earth rotates any two points lies along the great FIG. 1-5–A Parallel of Latitude from west to east, i.e., counterclock- circle that connects these two wise when viewed from a point in points. (On the slightly flat tened great circle is termed the equator, as space atop the North Pole. The surface of the earth, the short est dis- shown in Figure 1-4, and the two west-to-east rotation makes the sun tance between two points is techni- hemispheres formed are named the appear to rise in the east and set in cally termed a geodesic, but for the northern and southern hemi spheres. the west. The earth is also a mag- purposes of this course a great cir- A small circle results if a plane net—discussed below—and has cle and a geodesic are one and the is passed through the earth that does North and South Magnetic Poles. same.) not touch the earth’s center. Small These poles (shown also in Figure If the plane is passed so that it is circles parallel to the equator 1-3) are not coincident with the geo- perpendicular to the earth’s axis of (termed parallels) are one of the graphic poles, an important point rotation (i.e., equidistant from the two reference coordinates used to explored below. geographic poles), the resulting
L L FIG. 1-6–The Planes of the Meridians FIG. 1-4–The Equator (Longitude) Meet at the Polar Axis
1-7 1 Introduction to Coastal Navigation
define position on the earth’s sur - through the Naval face. Figure 1-5 shows the equator Observatory in Washing - LONGITUDE OF THREE LOCATIONS and another parallel of latitude. ton, DC, would be identi - Latitude is the angular measure of fied as Lo = 77° 03.9’ W TOKYO EAST the distance north or south of the (77 degrees, 3.9 minutes, equator and is measured in degrees west of the prime meridi- an) or, equivalently as 77 (0 to 90 degrees). PRIME A great circle that passes 03’ 54” (77 degrees, 3 Pn MERIDIAN through the polar axis or axis of minutes, 54 seconds west rotation is termed a meridian. It has of the prime meridian). The degree sign is some - two parts—that on the observer’s WEST side of the earth, which is called the times omitted. In some upper branch, and one on the other writings, E or W is omitted LOS ANGELES WASHINGTON side of the earth, which is called the when it is clear that the L longitude is east or west, lower branch of the meridian. The FIG. 1-7–Longitude for Three Locations on the but this practice should be planes of the meridians meet at the Earth’s Surface polar axis, as shown in Figure 1-6. discouraged. As other examples, the longi -
Meridians are used to define ST G A U O A C R
S D tude of the Griffin Observatory in U historiCal A U Y R the other major coordinate for spec- XI IA L ifying position on the earth’s Los Angeles, CA, is Lo = 118 18.1’ Footnote: surface –longitude. W, and that of the Tokyo Where is the Astronomical Observatory at reference Meridian? LONGITUDE AND LATITUDE Mitka, Japan, is Lo = 139 32.5’ E. As noted in the text, the prime Remember, longitude is always meridian passes through Green - The prime meridian (more specified as east or west of the wich, England. However, unlike specifically, its upper branch) passes prime meridian. Figure 1-7 shows the equator, its location is entirely arbitrary. Ptolemy, for example, through the original site of the Royal the longitudes of these three loca - Observatory in Greenwich, England. chose to place the prime meridian tions on the earth’s surface as through the Canary & Madeira Also called the Greenwich viewed from atop Pn. Islands. Later it was moved to the Meridian, it is used as the origin of It is not sufficient to identify a Azores and the Cape Verde Islands. measurement of longitude (see side- position on the earth’s surface by its Various governments have placed bar). More precisely, longitude it in Copenhagen, Jerusalem, longitude alone, because there are London, Paris, Philadelphia, Pisa, (abbreviated Lo, or sometimes writ - an infinite number of points that lie Rome, and St. Petersburg. At the ten λ, the Greek letter lambda) is the on any meridian. Another coordi - Third International Geophysical angular distance (in degrees, min- nate is necessary to specify position Con gress meeting in Venice in utes, and sec onds, or degrees and uniquely. 1881, several other proposals were deci mal minutes) between a position floated, including use of the Great As noted, this second coordinate Pyramid of Egypt as the prime on the earth and the prime meridian is termed latitude. More formally, meridian. In 1884, representatives mea sured eastward or west ward latitude (abbreviated L or Lat.) is from 26 countries to the through 180 degrees along the arc of the angular distance between a International Meridian Con - the equa tor to the meridian of the position on the earth’s surface and ference in Washington, DC, voted to select Greenwich as the official position. Because longi tude is mea- the equator, measured northward or prime meridian. The French con- sured only through 180 degrees, southward from the equator along a tinued to recognize the Paris rather than 360 degrees, from the meridian and labeled with an “N” Observatory as the “correct” loca- prime meridian, it is necessary to or an “S” to denote whether the tion of the prime meridian until include the word east (E) or west point is located in the northern or 1911. These and other stories are related in Sobel (1995) and (W) to define the longitude uniquely. southern hemispheres, respectively. O’Malley (1990). For example, the meridian passing (Sometimes, when the hemisphere
1-8 Introduction to Coastal Navigation 1
necessary to have some means for GREENWICH Lat 45o30.1’N N specifying direction on the earth’s o Lo 73 20.4’W 60oN surface. 50oN o Direction is not absolute but PARALLELS 40 N o must be keyed to some reference OF LATITUDE 30 N (TYPICAL) 20oN point. Three common reference W 10oN points are true north, magnetic 100o 80o 60o 40o 20o 20o north (discussed below), and the EQUATOR W E ship’s heading (relative bearings are discussed below). If direction is referenced to true MERIDIANS north (geographic north or the OF LONGITUDE North Pole), it is defined relative to (TYPICAL) the local meridian passing through the point of interest (also called the L local geographic meridian). The FIG. 1-8–Grid System of Latitude and Longitude local geographic meridian passes through the north geographic pole, is clearly implicit, the N or S will be along any meridian, is equal to 60 so this direction is relative to the omitted, but this practice is to be nautical miles, and 1 minute is north geographic pole or to north. discouraged.) Latitude ranges from equal to l mile. Note, however, that The direction of true north, or 0 degrees (for a point located at the this does not hold for longitude. northward along the upper branch equator) to 90 degrees N or S (for a Although 1 minute of longitude is of the local geographic meridian, is point at the north or south geo - approximately equal to 1 nautical defined as zero degrees and graphic pole). Lines of constant lat- mile at the equator, as the latitude becomes the reference direction. By itude are called parallels of latitude, increas es, the distance along any convention, the preci sion of angular or simply, parallels. parallel, between two meridians, measurement for courses or bear- Continuing the earlier examples, becomes smaller, reaching 0 miles ings is to the nearest degree. the latitude of the Naval at either pole. (The length of 1 Degrees are reported to three digits; Observatory in Washington, DC, is degree of longitude is approximate- so, for example, north has the direc- L (or Lat.) = 38 55.2’ N, that of the ly equal to 60 times the cosine of tion 000 degrees. Direction is spec- observatory in Tokyo, Japan, L = 35 the latitude. For example, at latitude ified clockwise from true north. 40.4’ N, and that of the Griffith of 41 30’ north, approximately the Thus, east is 090 degrees, south is Observatory, L = 34 06.8’ N. These midpoint of the latitudes given on 180 degrees, west 270 degrees, etc. two coordinates, latitude and longi - the 1210-Tr chart, the length of 1 The direction 360 degrees and 000 tude, are used to define locations on degree of longitude is approximate - degrees are one and the same and, the earth’s surface, as shown in ly 45 nautical miles rather than 60 by convention, this direction is usu- Figure 1-8. By convention, a point’s nautical miles on the equator.) ally written 000 degrees. Therefore, latitude is written first and its lon - Remember that latitude is measured it is said that direction is measured gitude second, so if there are no along a meridian (running north or clockwise from north, and ranges labels, the first number written is south), while longitude is measured from 000 degrees to 359 degrees. latitude, the second longitude (the along a parallel (running east or With a suitable device for mea - notation E or W, versus N or S also west) from the prime meridian. suring angles (see Chapter 4), define the coordinate). directions can be read from a chart One important attribute of lati - DIRECTION off the local meridian. However, for tude (noted implicitly above) is the Latitude and longitude are all reasons that are apparent in later fact that 1 degree of latitude, mea- that are required to specify location chapters, it is useful to have addi- sured up or down (north or south) on the earth’s surface. But, it is also tional sources of directional infor-
1-9 1 Introduction to Coastal Navigation
L FIG. 1-9–True and Compass Rose as Presented on the 1210-Tr Chart
1-10 Introduction to Coastal Navigation 1
of the geographic pole, a line is
ST G A U O A C R
S D
U formed that “spirals” around the
A U Y X R ILIA FaCtoiD globe, continually edging either According to records dating northward (for directions between 271 degrees and 359 degrees or 000 back to the 1700s, the appar- degrees and 089 degrees) or south - ent position of the north ward (for directions between 091 magnetic pole has shifted degrees and 269 degrees). This line, from a position north of termed a rhumb line or loxodrome, Scandinavia across Green - approaches either pole, as shown in land to its present position in Figure 1-10. This line drawn on the the Parry Islands in northern surface of a sphere, such as the earth, is actually curved, not L Canada. Over geo logic time, straight. (However, as noted in FIG. 1-10–A Rhumb Line or the shifts have been even Chapter 3, it will plot as a straight Loxodrome as Given in Bowditch more dra matic; it is believed line on the Mercator chart typically that 200 million years ago used for coastal navigation.) lar, a phenomenon caused by the the magnetic poles were near The earth has a weak magnetic nonuniform distribu tion of magnet- the equator! field, thought to be generated by the ic material through out the earth. flow of the liquid iron alloy core of The angular difference between the planet. This field, termed a dipole mation provided on the nautical the geographic and magnetic merid - field, is similar to the mag netic field chart. One common directional ref- ians at any point on the earth is that would be generated by a large erence is termed a compass rose, called the magnetic variation, or bar magnet located near the center of which provides directional informa - simply variation. (The term mag - the earth. The magnet ic flux lines tion relative to both true and to netic declination is also used.) diagramed in the styl ized and simpli- magnetic north (discussed below). Variation is said to be east if the fied representation of Figure 1-11 magnetic meridian points eastward Figure 1-9 shows a dual compass flow out from the core through the of the north geographic pole, or rose taken from the 1210-Tr chart. auroral zone of the South Pole, west if (as shown in Figures l-12 or Directions relative to true north are around the earth, and return through given on the outer circle of the rose. the auroral zone of the North Pole. True north is generally indicated More important to the mariner, the with a star symbol (presumably a magnetic poles on the earth differ reference to Polaris, the star that is, from the geographic poles. In 1984, to within a degree or so, aligned the North Magnetic Pole, for exam- with true north). The principal ple, was located in Canada’s advantage of printing compass Northwest Territories, at approxi- roses on nautical charts is that it is mately a latitude of 78.9 degrees relatively easy to transfer (i.e., north and longitude 103.8 degrees measure) these direc tions with par- west, several hundred miles removed allel rulers or a para line plotter (see from the geographic North Pole. Chapter 4). At the surface of the earth, lines When a direction other than of magnetic force are termed mag- exactly north, south, east, or west is netic meridians, analogous to geo- specified on the earth, and followed graphic meridians. However, unlike for any distance, such that each sub- geographic meridians, which have a sequent meridian is passed at the simple geometrical interpretation, L same angle relative to the direc tion the magnetic meridi ans are irregu- FIG. 1-11–The Earth is a Magnet
1-11 1 Introduction to Coastal Navigation
1-13) the north magnetic pole is still follows that variation is the able to convert from true to magnet - westward (to the left) of the north angular difference between true ic directions or the reverse. geographic pole as seen by the north and the direction that the ves- Variation data can be found in observer. sel’s compass would point, absent several sources. Perhaps most con - Incidentally, diagrams such as shipboard magnetic influence. Lines venient, variation data are printed Figures 1-12 and 1-13, are very of constant varia tion are termed iso- on the compass rose found on nau - helpful in understanding the con cept gonic lines, and the line where the tical charts, such as is illustrated in of variation but are not, strict ly variation is exact ly zero degrees is Figure 1-9. There the inner circle of speaking, accurate. This is because called the agonic line. These isogo- the compass rose shows magnetic they suggest that a com pass (free of nic lines arc chart ed and are pub- directions while the outer circle shipboard magnetic influences) lished on Chart #42 by the National shows true directions. In this illus - would always point toward the Imagery and Mapping Agency. tration, the magnetic meridian North Magnetic Pole. In fact, a The relevance of all this to the points to the left of the local geo - freely suspended magnetic compass mariner is that the magnets in the graphic meridian—and the varia - needle acted upon by the earth’s vessel’s compass (discussed in tion is approximately 15 degrees magnetic field alone will lie in a Chapter 2) tend to align with the west. (As noted above, the magnet - vertical plane known as the magnet- magnetic meridians, rather than the ic meridians shift around, and have ic meridian. These magnetic meridi- true or geographic meridians. (It is daily (diurnal) and longer term ans, however, do not neces sarily actually slightly more complicated (secular) changes, so, for this rea - point towards the magnetic poles, than that, but Chapter 2 straightens son, the important shifts are identi - because the earth’s magnetic field is out the details.) Therefore, it is nec - fied on the chart. Reference to irregular. This technicality aside, it essary to know the variation to be Figure 1-9, for example, shows that
VARIATION IS THE ANGULAR DIFFERENCE BETWEEN THE GEOGRAPHIC AND MAGNETIC MERIDIANS
GEOGRAPHIC OBSERVER’S NORTH POLE POSITION
MAGNETIC NORTH POLE
L FIG. 1-12–Variation: The Approximate Difference Between the Directions to the North Geographic Pole and the Magnetic Meridian
1-12 Introduction to Coastal Navigation 1
the variation at this location was 15 bearing compass, discussed in ally bear 345 degrees true. This is degrees west in 1985, and that it is Chapter 4, might be used to take a because, at this location, the varia - increasing at the rate of three min - bearing on a shore-based object, tion is 15 degrees west, or to the left utes per year.) and the navigator may wish to con - of true. A glance at the compass Within the continental United vert this to a true bearing for plot - rose shows that all bearings have States, variation ranges from about ting on the nautical chart. Alter - this fixed difference between mag - 20 W in northern Maine, through 0 natively, a mariner may measure a netic and true. Conversion from in portions of Florida, to 21 E in true course on the chart (discussed magnetic to true is, therefore, a northern Washington state. (On the in Chapter 3) and wish to convert simple matter of subtraction of a northern border between Alaska this to a magnetic course. west erly variation, or addition of and Canada, it is approximately 35 Conversion from one reference an easterly variation. Thus, for E as of this writing.) point to another is relatively simple. exam ple, an object bearing 090 Suppose, for example, that the vari- magnet ic, would bear 090 - 015 or CONVERSION FROM ation is 15 degrees west, as is 075 true. (Chapter 2 provides some TRUE TO MAGNETIC AND shown in Figure 1-9, as would handy memory aids to keep the VICE VERSA apply to one portion of the area addition and subtraction straight, It is often necessary to convert cov ered by the 1210-Tr chart. An but a simple one to remember is from direction expressed relative to object located in the direction of “magnetic or compass to true, add magnetic north to direction magnetic north from the perspec- east.”) As discussed in other chap - expressed relative to true north or tive of the observer (said to have ters, magnetic courses or bearings vice versa. For example, a hand- bear ing 000 magnetic) would actu- are identified as such by the use of
VARIATION CHANGES WITH THE OBSERVER’S LOCATION
GEOGRAPHIC NORTH POLE VARIATION WEST AT THIS LOCATION
MAGNETIC NORTH POLE
VARIATION EAST AT THIS LOCATION
L FIG. 1-13–Variation is the Angular Difference between the Geographic (True) Meridian and the Magnetic Meridian. Variation Changes with Locality.
1-13 1 Introduction to Coastal Navigation
RELATIVE BEARINGS
2 POINTS ON DEAD PORT BOW AHEAD 000o
BROAD ON PORT BOW 2 POINTS STARBOARD BOW
o 360 o 2 5 2. o BROAD ON THE 7 . 5 3 E BEAR STARBOARD BOW 2 POINTS FOR 3 TIV ING LA S o RE 0 5 4 FORWARD 1 5 o 3
WAR PORT BEAM
D 2 POINTS
o 0 6 STARBOARD BEAM 5 . 7 2 . 5 9 o 2
0
o
9
BROAD ON 0 BROAD ON
0
7
o
2
PORT BEAM STARBOARD BEAM
1
o
5 1
.
2
7
.
4 5
2 2 POINTS ABAFT
o
STARBOARD BEA
1
o
5
3
2
5
2 POINTS ABAFT 2
o
PORT BEAM
1
M
5
BROAD ON
5
. B 7 o
2
Y . 5
0 DE EES
2 GR
STARBOARD QUARTE 1
o 8 0
o
2 POINTS ON BROAD ON STARBOARD QUARTER
PORT QUARTER DEAD ASTERN R 2 POINTS ON
PORT QUARTER
BY COMPASS POINTS
There are 32 points on a compass each having 11 1/4 degrees. (32 x 11.25 = 360 degrees)
L FIG. 1-14–Relative Bearings by Degrees and Points
1-14 Introduction to Coastal Navigation 1
the word “magnetic,” or the writing dead ahead, directly off the bow, reciprocal bearing is one that differs of an “M” after the number. If no would bear 000 R. Note that rela- from the original by 180 degrees. such prefix or suffix is added, it is tive bearings relate to the fore-and- For example, if a fixed navigational assumed that the course or bearing aft or bow direction of the boat and aid, such as a lighthouse, were to is “true.” change direction as the boat bear 000 degrees true from your changes direction (heading) or posi - vessel (i.e., be directly north of RELATIVE DIRECTIONS tion. If the boat is underway, and your vessel), it could equally be (BEARINGS) the object observed is stationary, said that your vessel is directly It is convenient, from time to the relative bearing will change as south of the lighthouse. That is, time, for mariners to indicate direc - the boat approaches, passes, and your vessel would be on a recipro - tions referenced to objects other continues on. The relative bearing cal bearing from the lighthouse. To than the true and/or magnetic would also change if the boat were calculate a reciprocal bearing, all meridians. In fact, one of the most turned, increasing in a clockwise that is necessary is to add or sub - used direction systems is that refer - manner as the boat turned counter - tract 180 from the given bearing. In enced to the fore-and-aft line paral - clockwise. this example, the reciprocal of 000 lel to, or directly over, the keel of To convert from relative bearing degrees is 180 degrees (obtained by the observer’s vessel. to either a true or magnetic bearing, adding 180). (Helpful hint: in cal- If a direction “rose” were super - all that is necessary is to remember culating a reciprocal by addition or imposed over the vessel (plan view) the equation: ship’s heading + rela- subtraction, it may also be neces - with the 000 line directly forward, tive bearing = bearing to object. sary to add or subtract 360 degrees at the vessel’s bow, 090 on the ves- Thus, for example, if the vessel to the result to ensure that the sel’s starboard beam, 180 directly were heading 070 true, and you answer lies between 000 and 360.) aft, on the vessel’s stern, and 270 on observed an object bearing 135 R, The reciprocal of 270 degrees is the port beam, the relative bearing the object would bear 070 + 135 = 090 degrees, the reciprocal of 315 system is developed as illustrated in 205 true. Of course, because there degrees is 135 degrees, etc. (With a Figure 1-14. Objects relative to the are only 360 degrees of arc measure little practice you can do these in instantaneous direction of the bow in a circle, it may be necessary to your head quickly by first adding of the boat are indicated in degrees subtract 360 degrees from the cal- 200 and taking away 20, or sub - of angular measure, clockwise, just culated bearing of the object. For tracting 200 and adding 20! Thus, as directions are indicated for the example, if the ship’s heading were for example, the reciprocal of 121 true and magnetic direction sys - 315 degrees true and the object’s degrees is 301 degrees, obtained by tems. Shown also in Figure 1-14 are relative bearing were 135 degrees, quickly adding 200 to 121 to get relative bearings in the older “point the true bearing would be 315 + 321, and then subtracting 20 to get system,” in which the 360 degrees 135 = 450; subtracting 360 gives 301). are subdivided into 32 points. (The the correct answer of 090 degrees. If your compass is the top-read- older “point system” is included for The concept of relative bearings ing type (see Chapter 2) you can historical interest only, and is not is fundamental in the practice of read the reciprocal bearing directly. used in this text.) navigation. The concept should be Reciprocals can also be read from a An object 45° off the bow on the thoroughly understood. The three convenient compass rose. starboard side (broad on the star - direction systems will be linked Bearings, whether with respect board bow in the older system) together in the use of the magnetic to true north (true bearings) or mag- would have a relative bearing of (or compass and the practice of pilot- netic north (magnetic bearings), are would bear) 045 R (here the “R” ing. all bearings from the vessel to an denotes “relative”). If the object object. Reciprocal bearings are were 45° off the bow on the port RECIPROCAL BEARINGS bearings from an object to the ves- side, it would have a relative bear - Finally, we conclude with brief sel. ing of: 360 - 045 =315R. A vessel mention of reciprocal bearings. A
1-15 1 Introduction to Coastal Navigation
SELECTED REFERENCES
Bowditch, N., (1995). American Practical Navigator; Naval Training Command, (1972). A Navigation An Epitome of Navigation, Pub No. 9, Defense Compendium, NAVTRA 10494-A, U. S. Mapping Agency, Bethesda, MD. Government Printing Office, Washington, DC.
Brogdon, B., (1995). Boat Navigation for the Rest of Norville, W., (1975). Coastal Navigation. Step by Step, Us: Finding Your Way by Eye and Electronics, International Marine Publishing Co., Camden, ME. International Marine, Camden, ME. O’Malley, M., (1990). Keeping Watch, a History of Budlong, J. P., (1977). Shoreline and Sextant, Practical American Time, Viking Penguin, New York, NY. Coastal Navigation, Van Nostrand Reinhold Co., New York, NY. Queeney, T. E., (1986). “The Wandering Magnetic Pole,” Ocean Navigator, No. 9, pp. 3 et seq. Cline, D.A., (1990). Navigation in the Age of Discovery, Montfleury, Inc., Rogers, AR. Saunders, A. E., (1987). Small Craft Piloting and Coastal Navigation, Alzarc Enterprises, Departments of the Air Force and the Navy, (1983). Air Scarborough, Ontario, Canada. Navigation, AFM 51-40, NAVAIR49, 00—80V— 49, U. S. Government Printing Office, Washington, Schofield, Admiral B.B., (1977). Navigation and DC. Direction, The Story of HMS Dryad, Kenneth Mason, Homewell, UK. Eyges, L., (1989). The Practical Pilot: Coastal Navigation by Eye, Intuition, and Common Sense, Schufeldt, H. H., Dunlop, G.D., and A. Bauer, (1991). International Marine, Camden, ME. Piloting and Dead Reckoning, 3rd edition, Naval Institute Press, Annapolis, MD. Kals, W.S., (1972) Practical Navigation, Doubleday & Company, Inc., Garden City, NY. Sobel, D., (1995) Longitude the True Story of a Lone Genius who Solved the Greatest Scientific Problem Kielhorn, W. V., (1988). A Piloting Primer, privately of His Time. Walker and Company, NY. printed, Naples, FL. Tver, D. F., (1987). The Norton Encyclopedia Maloney, E. S., (1985). Dutton’s Navigation and Dictionary of Navigation, W.W. Norton & Piloting, 14th edition, Naval Institute Press, Company, New York, NY. Annapolis, MD. U.S. Coast Guard Auxiliary, (1983). Coastal Piloting, Markell, J., (1984) Coastal Navigation for the Small U.S. Coast Guard Auxiliary National Board, Inc., Boat Sailor, Tab Books Inc., Blue Ridge Summit, Washington, DC. PA. Wright, F.W., (1980). Coastwise Navigation, Jason Ministry of Defense (Navy), (1987). Admiralty Manual Aronson Inc., New York, NY. of Navigation, BR 45 (1), Volume l, Her Majesty’s Stationary Office, London, UK.
Moody, A. B., (1980). Navigation Afloat, A Manual for the Seaman, Van Nostrand Reinhold Co., New York, NY.
1-16 Chapter 2
THE MARINE MAGNETIC COMPASS
“Truth lies within a little and certain compass, but error is immense.”
–Henry St. John, Viscount Bolingbroke, Reflections upon Exile (1716)
INTRODUCTION determine compass courses from his second chapter of the true courses. TAdvanced Coastal Navigation Compass adjustment refers to (ACN) Course explores the marine the process of adjusting small mag- compass and its use. The compass nets contained in the compass to is one of the simplest and most use- remove as much error as possible. ful navigation instruments to be Many modern textbooks devote considerable space to compass carried aboard a vessel. Arguably, a adjustment, and the reader may competent navigator, well-found wonder why this topic is covered vessel, up-to-date charts, timepiece, only briefly here. The reason is and a good compass are the only simple. Although compass adjust- real requirements for a safe and ment is not impossibly complex, it efficient voyage. Columbus was is not trivial and needs to be done able to do this even without good right! Professional compass charts or timepieces! adjusters are available at reasonable This chapter provides a brief cost to perform this service and, history of the compass, a discussion unless the mariner is willing to of the types and parts of the modern devote a substantial amount of time compass, an exposition of the prin- and intellectual effort, this is a job ciple of operation of the compass, best left to experts. In addition to and finally, a discussion of possible adjusting the compass, a profes- compass errors and their measure- sional can provide good advice on ment so that the mariner can com- the placement of the compass, ship- pensate for these errors and steer board electronics, and other gear correct courses. In particular, this that may affect the compass. For chapter reviews so-called TVMDC those who disagree with this assess- computations, named for the ment and have the time and inclina- sequence True-Variation-Magnetic- tion to master the intricacies of Deviation-Compass that is used to compass adjustment, a brief
2-1 2 The Marine Magnetic Compass
description is included. Moreover, By the time of Columbus, the may revolutionize this field. (Gyro- the references included at the end of compass was well developed and scopes are not discussed in this text, this chapter provide a useful start- there is evidence (from the diaries as these are not presently available ing point for home study. of Columbus) that the phenomenon at reasonable cost to the typical The material in this chapter is of magnetic variation was at least boater.) not difficult. But teaching experi- partially understood. By the early During the mid-1920s, an elec- ence indicates that considerable 1700s, charts showing the locations tronic compass—termed a fluxgate practice is required in order to of lines of equal variation (isogonic compass—was developed for air- rapidly and reliably solve the prob- lines) were available. Likewise, craft to provide better directional lems discussed in this chapter. compass deviation, an important information in turns and during subject discussed below, was under- maneuvers. In recent years, this stood in qualitative terms at about ST G A U O technology has become available at A C R
S D What You Will U
A U Y this same time, although practical X R ILIA learn in this a reasonable cost to the mariner, means for compensating for devia- and for this reason is given passing Chapter tion were not developed until 1801 mention. J The “anatomy” of a by Captain Matthew Flinders (from The “electronics revolution,” a compass which the Flinders bar used in com- phrase used frequently in this text, pass adjustment takes its name). J Compass types also includes directional systems. The modern liquid-filled com- Outputs from a fluxgate compass J Compass deviation and pass, similar to those used on yachts can be “processed” by a wide vari- its measurement today, dates back to the period 1850 ety of computer systems and used J TVMDC calculations to 1860 when it was developed and for automated steering (autopilots), patented by E. S. Ritchie of Boston, J Compass errors and navigational computers (e.g., to Massachusetts. (The company compute current set and drift, as founded by Ritchie is still in busi- discussed in Chapter 7). Yet more ness today.) Since that time, there sophisticated developments are BRIEF HISTORY have been evolutionary rather than likely in the near future. The exact origin of the compass revolutionary developments in the For all these newer develop- is lost in antiquity. Although some magnetic (mechanical) compass. ments, the traditional magnetic accounts claim that the compass For example, new lightweight compass remains one of the most was invented well before the birth materials are used for compass important navigational instruments, of Christ (Hewson, 1983), docu- cards, improved magnets are avail- as evidenced by the fact that even mentary evidence of its use in able, and many other incremental the most sophisticated ship or air- Europe and China dates back only improvements have been made to to approximately 1100 AD (Aczel, increase the accuracy, stability, and craft in service today still has at 2001; Bowditch, 1995; Collinder, utility of the magnetic compass. least one magnetic compass aboard. 1955; Jerchow, 1987). (Incidental- Elmer Sperry, an American, and Its relative simplicity, reliability, ly, by convention the early Chinese Anschutz-Kampfe, a German, dur- and lack of dependence on electrical compasses were said to point south, ing the early part of the 20th centu- power sources will probably ensure as this was considered a more noble ry developed the modern gyrocom- its survival well into the future. aspect.) The modern compass card pass, an instrument capable of indi- (as opposed to needles used on the cating true rather than magnetic PARTS OF THE COMPASS earliest compasses) apparently orig- north. Gyroscopes were widely Over the years, the marine mag- inated with Flavio Gioia of Amalfi used in naval and merchant ships netic compass has evolved into a in southern Italy sometime around since the end of World War I. functional, easy-to-read, conve- 1300 AD (Collinder, 1955), Heretofore, gyroscopes have been nient, and relatively inexpensive although this is questioned by some electromechanical devices, but laser navigational instrument. The damp- (Aczel, 2001). gyros are now in development that ing system of a modern, spherical,
2-2 The Marine Magnetic Compass 2
RICTHIE POWERDAMP® SYSTEM…DETAIL
High Visibility Ultra-Light
PowerDamp Stabilizer Hardened DirectiveForce® Steel Pivot Magnets
Brass Counterbalance Triple Cup Hardened Steel and Sapphire Sapphire Jewel Pivot Jewel
L PHOTO COURTESY OF RITCHIE NAVIGATION FIG. 2-1–Damping System of Modern Compass liquid-filled marine magnetic com- and W) are also indicated on the mariners. Fortunately, mariners pass is shown in Figure 2-1. In this dial. Arrows or other marks are have rediscovered the joy of num- compass, a lightweight dial or com- sometimes used to designate the bers and the older point system is pass rose is graduated in degrees intercardinal points (e.g., NE, SE, now only of historical interest. (If increasing in a clockwise direction SW, and NW). Older compasses you have such a compass, mount it from 000 degrees to 359 degrees to were traditionally graduated in the in your den, not on your boat!) indicate the compass heading. The mariner’s “point” system, men- Attached to the dial are the increments shown on the compass tioned in Chapter 1, in which the “north-seeking” compass magnets. dial can be 1 degree, 2 degrees, or, circle was divided into 32 compass The dial is supported on a jeweled more typically for compasses used points, each of 11.25 degrees. bearing, which turns on a pivot. In on small vessels, 5 degrees. (Stud- These are named, in clockwise turn, the pivot is mounted in a gim- ies conducted just prior to World order from north: north, north by bal system, designed to keep the War II indicated that graduations east, north-northeast, northeast by dial level with the horizon if the every 5 degrees were significantly north, northeast, northeast by east, vessel pitches or rolls. Fastened to easier to read than finer graduations east-northeast, east by north, east, the gimbal is one (or more) lubber’s and, in practical terms, nearly as etc. Naming these points, termed line(s). The lubber’s line (also accurate.) Numbers are typically “boxing the compass,” was an termed lubber line [Moody, 1980]) spaced every 30 degrees, and the unpleasant and confusing task used is the index mark against which the cardinal points (north, south, east, historically in hazing rituals for dial graduations are read to deter- and west, or abbreviated N, S, E, midshipmen and other would-be mine the direction of the vessel rel-
2-3 2 The Marine Magnetic Compass
the magnets, so as dentally, the wires to the compass to reduce wear on light should be twisted to minimize the pivot. The ultra- magnetic effects.) lightweight dials in Many compasses come with a use can be damped hood (adjustable on some models) with fluids that are to reduce glare and improve read- not viscous (thick), ability. Removable protective cov- a combination that ers are also recommended if the provides stability compass is installed in a location and accuracy with- where it is exposed to the elements. out a tendency to “overshoot” and COMPASS DIAL DESIGN oscillate as the ves- There are two principal designs sel is turned to a for the compass rose or dial. These new heading. The are discussed briefly below. compass also con- J The first design is termed a top- tains an expansion reading compass (also a flat diaphragm to allow card compass by some manu- for the expansion facturers). With this design, the and contraction of mariner reads the heading or PHOTO PHOTO COURTESY OF RITCHIE NAVIGATION the damping fluid L bearing “across the card.” The with temperature or pressure lubber’s line is located behind FIG. 2-2–Combination Front and Top changes. A fill plug is used to the card. The numbers that indi- Reading Compass replace or “top off” the damping cate heading or bearing increase fluid. (It is important that there are in a clockwise direction—a cor- no air bubbles in the compass ative to that of the card. The lub- rect geometric representation. A fluid.) ber’s line (or principal lubber’s line heading of 030 degrees is to the if there are more than one) should The bowl is supported by a case be aligned with the fore-and-aft or holder, generally axis of the vessel. called a binnacle. The gimbals, card, and magnets Somewhere near the are enclosed in a bowl with a clear, bowl are found the transparent, hemispherical glass (or compensating mag- plastic) top, within which the card nets, used to adjust and gimbals are free to rotate inde- the compass to pendently of the attitude of the con- compensate for the tainer. The top (dome) may be vessel’s magnetic impregnated with inhibitors to environment. reduce any discoloration of the card Most compasses or fluid from ultraviolet radiation are lighted for night and may also magnify the readings, use. A low intensity so that the apparent card size is red lamp is pre- larger. The bowl is filled with a ferred to avoid or nonfreezing liquid to damp (slow minimize adverse
down) the motion of the dial for effects on the night PHOTO COURTESY OF RITCHIE NAVIGATION increased stability and to support vision of the helms- L much of the weight of the card and man or crew. (Inci- FIG. 2-3–Fluxgate Compass with Digital Readout
2-4 The Marine Magnetic Compass 2
right of a heading of 000 slightly more con- degrees, for example, and the fusing and requires a compass provides the same rep- bit more practice resentation. If the helmsman is before familiarity is asked to turn to 030 degrees assured. An inexpe- from a heading of north, it is rienced helmsman, clear that this must be a turn to asked to come to a the right. It is also relatively heading of 030 easy to read compass bearings degrees from north, over this compass dial. The could glance at the compass dial itself is unob- front-reading dial structed through 360 degrees, and see that this although its placement aboard heading is to the left, the vessel usually limits this and, therefore, begin range. A top-reading compass is a turn in the wrong installed forward of the steering direction before dis- mechanism and beneath the covering the error. From the perspective PHOTO COURTESY OF RITCHIE NAVIGATION helmsman’s eye level. L of ease of interpretation, the top- J The second design is termed a FIG. 2-4–Fluxgate Compass reading compass dial is greatly to front-reading compass (also with Digital Readout be preferred. But, it is also impor- called a direct reading compass tant to consider how the compass and Conventional Displays by some manufacturers). This will be viewed once installed. In the compass dial design is typical of typical powerboat installation (and most aircraft compasses and is in sailboats where the compass bin- graduated in 5-degree increments also used for marine compasses. nacle is integrated with the wheel), and a top-reading dial that omits a With this design, the lubber’s the compass is located on a panel numerical display of degrees. Some line is in front of the dial and immediately in front of the helms- compasses also include inclinome- indicates the direction toward man, and so a top-reading compass ters, to measure the angle of roll of which the vessel is heading. is easy to see. However, in a typical the vessel. However, the dial is graduated in light aircraft the compass is Yet other compass displays, typ- a counterclockwise direction. installed at the top of the cockpit ically those used with fluxgate Thus, for example, the 30-degree (where it is least likely to be affect- compasses, feature a direct digital graduation on the front-reading ed by magnetic interference from readout of the heading. Figure 2-3 dial is located to the left of 000. radios or other electronics), at or shows the display unit of a fluxgate This apparent reversal in direc- above the eye level of the pilot, compass with digital readouts. Dig- tion is made necessary because necessitating a front-reading ital readouts are generally shown to the lubber’s line is located in design. Similarly, in certain sail- the nearest degree, rather than 5 front of the dial. The mounting boats the compass is mounted on degrees as is common on conven- of a front reading compass usu- the outer cabin bulkhead—nearly at tional compasses. Although many ally precludes its use for obtain- eye level for the helmsman seated prefer digital displays, these also ing bearings. This is not a real several feet away—and a front- have limitations or disadvantages. detriment, since a hand-bearing reading compass is necessary. (For example, it is impossible to compass, discussed in Chapter 4, Some compass designs, such as take a bearing on any object that is is a ready substitute. that shown in Figure 2-2, combine not aligned with the vessel’s head- Either design correctly shows both types of compass displays in ing.) Moreover, the digital display the vessel’s actual heading, but the one unit. The model shown in Fig- provides less “situational aware- front-reading compass design is ure 2-2 shows a front reading dial ness” for the helmsman than does
2-5 2 The Marine Magnetic Compass
the top-reading compass. This dis- sels. On average, small vessels are meet, but this is sometimes more of advantage can be overcome if the significantly more “lively” than a problem in smaller craft. Consult fluxgate compass also incorporates a compass adjuster and read the
a conventional dial, as is shown in ST G owner’s manual (or product litera- A U O A C R
S D praCtiCal U
A U Y R Figure 2-4, which provides precise X A ture) for advice on this important ILI tip heading information and situational topic. awareness. The display shown in Carry at least one spare com- There are several types of com- Figure 2-4 cannot be used to take pass mounts, each with advantages bearings, however. pass aboard—if only a hand- and disadvantages. Compass Finally, some compasses— bearing compass. This is mounts include the bracket mount called telltale compasses—should (fast and versatile installation—par- be mounted in an upside down cheap insurance. According ticularly for angled surfaces), flush (overhead mount) position. The to Morrison (1942), early mount, deck or binnacle mount, and telltale compass is usually installed bulkhead/dash mount. in the ceiling of the navigator’s mariners carried plenty of berth, so that the navigator can read spare “needles” (compass PRINCIPLE OF OPERATION: the vessel’s heading when not on DEVIATION duty. Overhead-mount compasses needles) aboard. Ferdinand The modem magnetic compass are a favorite of “single handlers,” Magellan reportedly had is highly sensitive and is able to and can double as a backup com- align itself with weak magnetic pass. (Incidentally, the practice of thirty-five spare needles on fields, such as the earth’s magnetic “single-handing” (voyaging for his ship! field. The magnets underneath the long distances with only one person compass card will align with the aboard) is unsafe, a violation of the magnetic field and indicate direc- navigation rules (a proper lookout larger vessels. Larger and more tion relative to this field. But, the cannot be maintained by a sleeping expensive compasses have better magnetic field aboard a ship is actu- helmsman), and is strongly discour- gimbals and have larger and easier ally a combination (resultant) of aged.) to read dials. The saying “bigger is multiple magnetic fields—that of Whatever display is chosen, it is better” almost always applies to the the earth and those of the vessel and important that the numerals on the selection of a compass. Finally, it is its equipment. dial be large and easy to read. recommended that a vessel be Were the earth’s magnetic field Ornate displays, such as were found equipped with at least two com- acting alone, the compass would on older marine compasses, are less passes as a precaution against com- indicate direction in the magnetic readable than the simple, clean pass failure. A handheld compass direction system—that is, the com- designs of today. (discussed in Chapter 4) can serve pass would point in the direction of as a backup. magnetic north. (Please refer again BRIEF ADVICE ON to Chapter 1.) Determination of the COMPASS SELECTION COMPASS MOUNTING direction with respect to true north The best advice on compass Ideally, the compass should be would involve nothing more than selection is not to be miserly. With mounted where it can easily be adding or subtracting the local mag- compasses, as with other items of read, is protected from the ele- netic variation from the indicated equipment, you generally get what ments, and is free of any magnetic compass direction (more below). you pay for. Because the compass is influences aboard the vessel (see However, the magnetic field such an important navigational below). The lubber’s line should be aboard a vessel is not solely due to instrument, it is essential that it be precisely aligned with the fore-and- the earth’s magnetic field. Ship- of high quality. Incidentally, this aft axis of the vessel. On larger ves- board electronics, windshield wiper comment also applies to small ves- sels, these requirements are easy to motors, compressed-gas horns,
2-6 The Marine Magnetic Compass 2
The difference between these is
ST G A U O WARNING A C R
termed deviation. There are actual- S D U
A useful tip U Y X R Do not plaCe ly three “norths” that the mariner ILIA Metal oBJeCts need be concerned with: true north, It is important to empha size magnetic north, and compass north. near CoMpass Simply put, deviation is the differ- that deviation varies with the Do not use the area near ence between the direction that the vessel’s head ing. When con- compass actually points and the the compass as a resting direction that it would point if there verting a relative bearing to a place for metal objects, were no local magnetic fields true or magnetic bearing, aboard the vessel. Although statis- such as flashlights, cameras, tics on the deviation of uncompen- novices often make the mis- kitchen utensils, sated compasses aboard recreation- take of applying the devia- certain plotting instruments, al boats are not available, these deviations could be quite large, say tion appropriate to the rela- and even metal sunglasses. 10 degrees to 15 degrees, and possi- tive bearing rather than the These can affect the bly even more. It is precisely because of the vessel’s heading. Be careful accuracy of the compass deviation caused by the vessel’s not to make this error! readings and cause serious magnetic field that correcting mag- nets are found in all good compass- way to minimize possible course errors! es. A skilled compass adjuster can sources of deviation. move the adjusting magnets so as to J Second, follow the directions tachometers, electrical motors, tele- remove most of the deviation nor- given below to determine the vision sets, and other equipment mally caused by the vessel’s mag- also generate magnetic fields. netic field. (A good compass compass deviations on various Indeed, flashlights, camera light adjuster can also serve as a consul- headings. If these deviations are meters, tools, and even some tant on compass placement and can “acceptable” (a judgement call), kitchen utensils can also affect the advise the mariner how to stow then use the “For/Steer” table compass. (For skeptics, a simple other gear to minimize deviation in (see below) directly and do not experiment proves this and is high- the first place.) undertake compass adjustment. ly instructive. For example, note the If not, then either call a profes- Compass Adjustment— compass reading, then place a sional compass adjuster or use flashlight near the compass and A Brief Digression the following procedure. Read observe how the reading changes.) As noted above, the use of a the directions for compass The vessel itself—particularly steel professional compass adjuster is adjustment (contained in the vessels—may have magnetic fields recommended. This material is owner’s information supplied oriented in a variety of ways. The added for those interested in a do-it- with the compass) again to vessel’s magnetic field may even yourself project. The material in ensure that you are thoroughly depend upon the direction the ves- this section is adapted loosely from familiar with the procedure and sel was facing when it was con- the former AUXNAV specialty the location of the two adjusting structed or last laid up for the win- course (COMDTPUB P16798.16A) screws. ter (Kielhorn and Klimm, 1978). documentation: J Third, make the following work- These additional fields also affect J First, carefully read the direc- ing tool. Take a sturdy card- the compass, with the result that the tions that come with the vessel’s board and a dowel (a pencil will compass heading of the vessel may compass and ensure that the do). Make a hole for the dowel differ from its magnetic heading. compass is mounted in such a in the center of the cardboard
2-7 2 The Marine Magnetic Compass
and draw a straight line across make another compass devia- the magnetic heading to a true the cardboard through the cen- tion card as described below. heading. However, unlike variation, ter. Select a calm, sunny day which depends solely on the ves- For other perspectives, read (with minimal traffic to avoid) sel’s position, deviation varies with through appropriate sections of for this evolution, in mid-morn- the vessel’s heading. Therefore, it is Brogden (1995), Eyges (1989), ing or afternoon when the sun Denne (1979), and Kaufman (1978) necessary to use the deviation will cast a shadow on the dowel. included in the references at the end appropriate to the vessel’s compass Take the boat out and maintain a of this chapter. heading before it can be used to constant heading of north as It is seldom the case that all the convert to the correct magnetic indicated by the compass. Place effects of this magnetic field can be heading. Although, theoretically, the dowel in the hole and rotate compensated for by the adjusting this deviation could be different for the board until the shadow of the magnets, and usually a small resid- each possible heading, in practice dowel falls on the line. Now ual deviation (say 2 degrees to 4 the deviation is determined for each turn the boat in the opposite degrees, but sometimes more) 15-degree or 30-degree heading direction until the shadow falls remains after adjustment. The increment; then these values are on the other side of the line. You mariner has two options for dealing interpolated to estimate the devia- will have turned 180° (turn and with residual deviation. The first is tion on intermediate headings. This steady on the reciprocal course simply to ignore any residual error process of determining the devia- promptly because the sun moves and effectively compensate for its tion on various headings is termed about 1° in 4 minutes). Read the presence by fixing the vessel’s posi- swinging ship or swinging the com- compass on this heading. Most tion more often. As a rough rule of pass and is discussed below. probably, it will not read exactly thumb, an unrecognized error of 1° 180°. Now, use a stainless steel means that a vessel would be SWINGING SHIP or brass screwdriver on the approximately 1 mile off course Normally, professional compass athwartships (N-S adjustment) (termed cross-track error) if it adjusters will swing ship as part of adjusting screw; remove half of traveled a distance of 60 miles. their services to compensate the the difference between the com- Table 2-1 shows the cross track compass and provide a table of pass reading and 180°. For error as a function of the distance deviations to the mariner. In such example, if the compass were to traveled and the angular error or cases, the mariner will probably read 170°, use the adjusting residual deviation. For short dis- wish to spot-check this table peri- screw to set the compass to tances, small angular errors are odically to verify its continuing 175°. Turn back on the original practically insignificant and can accuracy. However, the procedures course until the shadow falls on sometimes be ignored. However, (discussed below) are the same the other side and take out half for longer distances or in conditions whether the entire deviation table is of the difference between the of poor visibility (which would pre- being prepared or individual values compass reading and 000°. vent detection and identification of are being spot-checked. J Fourth, repeat the process until landmarks, fixed aids to navigation In brief, the procedure for you can’t remove any more (ATONs), or buoys), simply ignor- swinging ship is to steady on a error. ing deviation cannot be recom- known compass course and then J Fifth, do the same thing on east- mended. take bearings on a distant object or west headings. Head 090° by The second, and generally range. The vessel is positioned so compass, align the shadow with preferable, option is to measure the that the magnetic bearing to the the line, turn 180°, read the compass deviation, and use this object to be observed is known. The compass, and take out half the measured value to correct the compass bearing is read directly, or error with the other (E-W) observed compass heading to a converted from a relative bearing adjusting screw. When no fur- magnetic heading in the same man- obtained using a pelorus and com- ther improvements can be made, ner as variation is used to “correct” pared with the object’s known mag-
2-8 The Marine Magnetic Compass 2
DistanCe anGular error (DeGrees) traVeleD Miles 1.00 1.50 2.00 2.50 3.00 4.00 5.00 7.50 10.00 1.00 0.02 0.03 0.03 0.04 0.05 0.07 0.09 0.13 0.18 2.00 0.03 0.05 0.07 0.09 0.10 0.14 0.17 0.26 0.35 3.00 0.05 0.08 0.10 0.13 0.16 0.21 0.26 0.39 0.53 4.00 0.07 0.10 0.14 0.17 0.21 0.28 0.35 0.53 0.71 5.00 0.09 0.13 0.17 0.22 0.26 0.35 0.44 0.66 0.88 6.00 0.10 0.16 0.21 0.26 0.31 0.42 0.52 0.79 1.06 7.00 0.12 0.18 0.24 0.31 0.37 0.49 0.61 0.92 1.23 8.00 0.14 0.21 0.28 0.35 0.42 0.56 0.70 1.05 1.41 9.00 0.16 0.24 0.31 0.39 0.47 0.63 0.79 1.18 1.59 10.00 0.17 0.26 0.35 0.44 0.52 0.70 0.87 1.32 1.76 12.50 0.22 0.33 0.44 0.55 0.66 0.87 1.09 1.65 2.20 15.00 0.26 0.39 0.52 0.65 0.79 1.05 1.31 1.97 2.64 17.50 0.31 0.46 0.61 0.76 0.92 1.22 1.53 2.30 3.09 20.00 0.35 0.52 0.70 0.87 1.05 1.40 1.75 2.63 3.53 22.50 0.39 0.59 0.79 0.98 1.18 1.57 1.97 2.96 3.97 25.00 0.44 0.65 0.87 1.09 1.31 1.75 2.19 3.29 4.41 27.50 0.48 0.72 0.96 1.20 1.44 1.92 2.41 3.62 4.85 30.00 0.52 0.79 1.05 1.31 1.57 2.10 2.62 3.95 5.29 35.00 0.61 0.92 1.22 1.53 1.83 2.45 3.06 4.61 6.17 40.00 0.70 1.05 1.40 1.75 2.10 2.80 3.50 5.27 7.05 45.00 0.79 1.18 1.57 1.96 2.36 3.15 3.94 5.92 7.93 50.00 0.87 1.31 1.75 2.18 2.62 3.50 4.37 6.58 8.82 60.00 1.05 1.57 2.10 2.62 3.14 4.20 5.25 7.90 10.58 70.00 1.22 1.83 2.44 3.06 3.67 4.89 6.12 9.22 12.34 80.00 1.40 2.09 2.79 3.49 4.19 5.59 7.00 10.53 14.11 90.00 1.57 2.36 3.14 3.93 4.72 6.29 7.87 11.85 15.87 100.00 1.75 2.62 3.49 4.37 5.24 6.99 8.75 13.17 17.63 L TABLE 2-1–Cross-track error as a function of distance traveled and residual deviation or other angular helm error. netic bearing, and the deviation is such as a prominent object or range. when conditions are nearly ideal, in calculated. Professional compass The object(s) selected for observa- calm waters and in good visibility. adjusters often use the sun for tion should be a good distance away The need for good visibility is obvi- observation, but most mariners are (e.g., 6 miles) to minimize parallax ous. The reason why calm waters unfamiliar with celestial navigation error in the calibration. It is impor- are preferred is to simplify steady- and elect to use something simpler, tant that swinging ship is done ing the vessel on a compass heading
2-9 310
L FIG. 2-5–The range formed by the spire in New Bedford and the Butler Flats light bears approximately 310 degrees. The Marine Magnetic Compass 2
and reading the compass. Experi- degree increments or bearings are from the south, these two objects ence shows it can take several hours not easily read throughout 360 are exactly in line (one behind the to swing ship, so the exercise degrees, then it is necessary to use a other or in range) on a bearing of should be planned with sufficient pelorus as well (discussed below). 310 degrees true from the vessel to time allowance to be completed the objects. The bearing can be read within the daylight hours. DIRECT OBSERVATION from the chart as discussed in The procedure for swinging ship USING A RANGE Chapter 3, but take the answer as depends upon the compass to be The easiest method for swinging given for the present. The variation examined and the ability to take ship, if circumstances permit, is to in this area, read from the nearest bearings on objects not directly use a range and read the compass compass rose, is approximately 015 aligned with the fore-and-aft axis of directly. A range consists of two degrees west; so the magnetic bear- the vessel. If the compass is gradu- charted objects that can be viewed ing of this range would be 310 + ated to the nearest degree, and and aligned from a distance. For 015 = 325 magnetic. (See below for designed and located so that an example, consider the spire in New a handy rule to remember whether unobstructed view is possible Bedford and the Butler Flats Light to add or subtract variation.) throughout all 360 degrees, then located south and east of New Bed- Suppose that the vessel were only a compass is necessary. (This ford shown in the l210-Tr chart and steadied on a compass course of is likely to be the case for relatively in Figure 2-5. Both of these objects 000 degrees (compass north) while few boats.) If, as is more common, are likely to be prominent and rela- the vessel was somewhere south of the compass is graduated only in 5- tively easy to identify. Approaching the line drawn on the chart. (This
Deviation (Degrees) 8 8 7 7 6 6 5 E 5 E 4 4 3 3 2 2 1 1 0 0 -1 -1 -2 -2 -3 -3 -4 -4 W -5 -5 W -6 -6 -7 -7 -8 -8 0 30 60 90 120 150 180 210 240 270 300 330 360 Compass Heading (Degrees)
Vessel: Auxiliary Facility 273007, All Radios and Electronics on, Data from 09-30-89 for Compass at Lower Helm Station. L FIG. 2-6–A Plot of Compass Deviations
2-11 2 The Marine Magnetic Compass
would, of course, be evident from are any “anom- the vessel because the Butler Flats alous” results Light would be to the right of the that do not fit the spire. At the precise instant that the pattern. Overall, light and the spire appeared to be in the line drawn line, the magnetic bearing of the through the mea- range would be 325 degrees from sured deviations the vessel. At this same instant, sup- should appear as pose that the compass bearing of a smooth curve the range (read over the compass) (actually a mix- was 323 degrees (while the com- ture of trigono- pass heading was 000 degrees). The metric functions deviation on this heading is the dif- for those techni- ference between the magnetic bear- cally inclined) L ing, 325 degrees, and the bearing free of “bumps” or observations FIG. 2-7–Relative Bearing read from the compass, 323 that appear discrepant. Such a curve degrees, or 2 degrees. But, is it 2 is drawn in Figure 2-6 and appears A pelorus consists of a graduated degrees east, or 2 degrees west? It generally to confirm the adequacy compass-like dial (l-degree incre- ments) and sighting vanes that can can, of course, be worked out from of the measurements, although the deviations on some headings, such be rotated around the dial to take first principles (refer to Chapter 1), as 240 degrees, should be bearings. Unlike the “north-seek- but it is easy to remember the sim- rechecked. (In Figure 2-6 easterly ing” compass dial, however, the ple phrase, “compass least, error deviations are shown with a plus position of the dial on the pelorus east.” That is, if the compass bear- sign, and westerly with a minus does not change with the vessel’s ing is less than the magnetic bear- sign.) Additionally, the deviations heading. The pelorus is mounted ing (as it is in this case, 323 degrees on some headings are relatively and the dial fixed so that the 000- is less than 325 degrees), then the large (5 or 6 degrees), so the com- degree mark on the dial is pointed deviation is “east.” (If not, then the pensation is far from perfect. (A so as to be parallel to the vessel’s error would, of course, be “west.”) more technical analysis, omitted bow, precisely aligned with the Thus, in this example, the estimated here, suggests that improved com- fore-and-aft axis of the vessel. compass deviation on a heading of pensation is possible. However, the (Consult the directions supplied 000 degrees is 002 degrees east. To example is continued for illustrative with the pelorus for mounting confirm this result, the process purposes.) instructions and pay particular might be repeated and the average attention to the alignment proce- deviation noted. USE OF A PELORUS dure.) The pelorus should be It is convenient to use a work- As noted, most marine compass mounted so that the navigator can sheet, such as is shown in Table 2-2 installations do not permit direct easily view objects throughout a to record the observations. This reading of compass bearings full 360 degrees. worksheet contains directions as through a full 360 degrees. Addi- The bearings read from the well, which makes it handy to use. tionally, many compasses are grad- pelorus are relative bearings (refer The process is now repeated on a uated only to 2 degrees or 5 to Chapter 1), rather than compass compass heading of 015 degrees, degrees, rather than in 1-degree bearings. For this reason it is neces- 030 degrees, etc., until all observa- increments. If either of the state- sary to calculate the compass bear- tions are recorded. ments is true, it is necessary to ing from the simple equation: modify the procedure given above Ship’s heading + Object’s relative PLOTTING THE RESULTS for swinging ship. The most conve- bearing = Object’s compass bear- The results should be plotted on nient solution is to use a pelorus, ing. Figure 2-7 illustrates this equa- a sheet of graph paper to see if there sometimes called a dumb compass. tion.
2-12 The Marine Magnetic Compass 2 Light notes or other source. This worksheet is designed to be used for determination of deviation where a range is available and can be sighted over the com- pass. The true bearing of the range can be determined from a nautical chart, List, Compass deviation should be determined every 15 degrees of heading, generally starting at 000 degrees. The “notes” section should identify the electronics on board, and operating at the time of the calibration. It is suggested that two tables be prepared, one with all electronics on, and the other with electronics off. Altair 5 2E 3E 5E 6E 5E 5E on this heading Deviation Column 3, estimated Deviation is If Column 4< Columns 3 and 4 Deviation “West” “East,” Otherwise Vessel: 4 per 323 322 320 319 320 320 Range as Compass of range Compass Direction Bearing of Difference Between Read Over LDM Determined from Nautical Chart or Other Source Determined from Nearby Compass Rose -East +West, +/- Variation, True 3 of 325 325 325 325 325 325 Above range Direction Magnetic Calculation Taken From Taken naViGator: 310 015 West 325 Magnetic 2 000 015 030 045 060 075 Directly Read From per per Compass Lubber’s Lubber’s Line Vessel’s head Vessel’s Spire in Spire New and Bedford Butler Flats Light and VHF Radio Loran, ON Radar, 10-15-99 1 entry Where Obtained ranGe: notes: true BearinG ranGe: of Variation: MaGnetiC BearinG ranGe: of Date: L 2-2 –Portion of TABLE Worksheet for Determination of Deviations from Range
2-13 2 The Marine Magnetic Compass
This extra step requires a slight check deviation at least a few times
ST G A U O A C R
S D praCtiCal tip: modification to the worksheet given U during the boating season, and
A U Y X R in Table 2-2 to prepare a compass ILIA use of a whenever a major voyage is deviation table. This modified CoMpass in planned. Deviation can change worksheet is shown in Table 2-3. To repeataBle MoDe whenever new electronic gear is clarify by example, suppose that a brought aboard (or moved), the compass deviation table is being Get in the habit of entering vessel is laid up for the winter, or someone inadvertently leaves prepared using the same range as compass headings in a log on given in Table 2-2. While on a com- a flashlight or camera near the pass heading of 015 degrees, the your trips—particularly compass. navigator sights over the vanes of when in good weather. If the Lightning strikes near the vessel the pelorus as the range is perfectly can also affect deviation, and the aligned. The navigator calls “mark- same trip is repeated in con- compass should be checked after mark-mark” to allow the helmsman ditions of reduced visibility, electrical storms have passed to make slight heading changes to through the area. these same compass head- bring the vessel back to the assigned 015-degree heading, and ings can be used—even if the DEVIATION ON INTERMEDIATE HEADINGS notes the relative bearing, say 307 compass has not been degrees. Alternatively, the helms- The deviation table consists of man sings out the vessel’s heading checked for deviation and entries spaced every 15 degrees or on hearing “mark-mark-mark,” and errors exist. This use of a every 30 degrees. Values for inter- the navigator notes this heading. mediate headings are obtained by navigation instrument is The compass bearing to the range interpolation. For example, if the is, therefore, 015 + 307 = 322 termed its use in repeatable deviation were 3 degrees east on a degrees (360 degrees will have to mode. If you return to the compass heading of 000 degrees be subtracted from this total if the and 0 degrees on a heading of 015 total exceeds 360). The deviation same readings of the com- degrees, it would be approximately on a compass heading of 015 pass (or other navigation 2 degrees on a heading of 005 degrees is, therefore, 3 degrees east degrees. Fancy formulas are not as in the earlier example (remem- instrument), you compensate warranted here; simply prorate the ber, compass least, error east). for its error. For an interest- deviation directly and round the calculation to the nearest degree. SPOT CHECKS ing discussion of this princi- To spot-check a previously pre- ple, refer to Brogden (1995). USE OF THE pared deviation table, all that is nec- DEVIATION TABLE essary is to take advantage of During a typical voyage there The deviation table is used for ranges that may appear near the are many opportunities for such two important purposes. First, it is vessel’s course. In this case, the spot checks, and these should be used to calculate the vessel’s actual helm is put over briefly to align the used to advantage. Throughout the magnetic heading when steering a vessel with the range, the compass known compass heading. Second, it navies of the world, it is common heading noted, and the deviation on is used to calculate the correct com- practice to check the compass at this heading calculated as discussed pass heading to steer to make good above. At a minimum, compass least once daily and to report the a desired magnetic heading. headings should be recorded in a results to the captain. For the aver- The deviation table solves the log (see sidebar) for later analysis age boater, it is not necessary to first objective directly. Refer to when the vessel is anchored or make such frequent or formal Table 2-4, for example, based upon docked. checks, but it is appropriate to the measurements discussed above.
2-14 The Marine Magnetic Compass 2 6 3E on this heading Deviation Column 5, estimated Deviation is If Column 4< Columns 4 and 5 Deviation “West” “East,” Otherwise Altair 5 of 325 Above range Direction Magnetic Calculation Vessel: 4 per 322 of range Compass Direction Bearing (3) Plus Relative (360° may have Vessel’s Head (2)Vessel’s From Taken Difference Between to be substracted) LDM Determined from Nautical Chart or Other Source Determined from Nearby Compass Rose -East) (+West, +/- Variation True 3 307 Read From range Pelorus relative Bearing of naViGator: 310 015 West 325 Magnetic 2 015 Directly Read From per per Compass Lubber’s Lubber’s Line Vessel’s head Vessel’s Spire in Spire New and Bedford Butler Flats Light and VHF Radio Loran, ON Radar, 10-15-99 1 entry Where Obtained ranGe: notes: true BearinG ranGe: of Variation: MaGnetiC BearinG ranGe: of Date: L 2-3 –Portion of TABLE Worksheet for Determination of Deviations Using Relative Bearings
2-15 2 The Marine Magnetic Compass
CoMpass to MaGnetiC MaGnetiC to CoMpass
(a) (B) (C) (D) Compass Magnetic heading Deviation heading Deviation 000 2E 000 2E 015 3E 015 3E 030 5E 030 4E 045 6E 045 6E 060 5E 060 5E 075 5E 075 5E 090 3E 090 3E 105 3E 105 3E 120 2E 120 1E 135 1W 135 1W 150 2W 150 2W 165 3W 165 2W 180 4W 180 4W 195 5W 195 5W 210 6W 210 6W 225 5W 225 5W 240 4W 240 4W 255 5W 255 5W 270 4W 270 4W 285 3W 285 3W 300 2W 300 2W 315 1W 315 1W 330 1E 330 1E 345 2E 345 2E 360 2E 360 2E L TABLE 2-4–Sample Deviation Table [All Values in Degrees(°)]
Suppose that the vessel’s compass heading to a magnetic heading is rected or magnetic heading corre- heading were 045 degrees. From often termed “correcting,” because sponding to a compass heading of the first two columns of this table this process removes (corrects for) 045 would be 045 + 006 = 051 (headed by the phrase “compass to the deviation error. A simple rule to degrees magnetic. Similarly, a com- magnetic”), the deviation corre- remember is “correcting add east,” pass heading of 030 degrees corre- sponding to a compass heading of meaning that in converting from a sponds to a magnetic heading (refer 045 degrees is 6 degrees east. The compass heading to a magnetic to Table 2-4) of 035 degrees. magnetic heading is the compass heading, easterly deviation is added Frequently, however, it is neces- heading plus or minus the devia- (westerly deviation is, therefore, sary to reverse the process. That is, tion. Converting from a compass subtracted). Using this rule, the cor- to find the appropriate compass
2-16 The Marine Magnetic Compass 2
course to steer to make good a par- on a 045 degree heading is approxi- which completes the deviation ticular magnetic heading. For this mately 6 degrees (5 + 10(6-5)/16 = table. Use the left half of the table task it is necessary to reverse the 5.625, rounded to 6). Therefore, the when correcting from compass to logic discussed above. For example, approximate deviation on a magnet- magnetic, and the right half when suppose that the mariner wants to ic heading of 045 degrees is 6 “uncorrecting” from magnetic to make good a course of 045 magnet- degrees east, as shown in Table 2-4. compass. (Unless the deviations are ic. What compass course should be When making interpolations, quite large, the two halves of the steered? From the above discussion, remember that deviations are only table are virtually identical and, in note that on a magnetic heading of measured to the nearest degree. A practice, these differences are often 035 degrees the deviation is 5 calculation is only as accurate as the neglected.) Incidentally, the data degrees east, whereas on a magnetic least accurate number, so round all presented in the right hand side heading of 051 degrees, the devia- interpolated numbers to the nearest (RHS) of Table 2-4 are often used tion is 6 degrees east. A simple degree. to make a simple “For/Steer” cor- interpolation (rounded to the nearest Continuing the process leads to rection card. Entries for this table degree) indicates that the deviation the results shown in Table 2-4, can be computed as follows. Sup-
NAME BRIEF DESCRIPTION REMARKS
Northerly Turning Error Applies principally when vessel is on north- Of principal concern to aircraft, but erly or southerly headings and the compass of relevance to all fast boats. Arises card is tilted with respect to the horizon. from magnetic dip. Phenomenon de - Effect is for compass to lag the turn, or scribed for northern hemisphere only. momentarily show a turn in the opposite direction when turning from north. In turns from south, the compass leads the turn, i.e., shows the vessel turning more rapidly than it actually is. The effect is greatest in a rapid, steeply banked turn.
Acceleration Error Also due to dip, this error is greatest on head- Effect greatest with vessels capable ings of east or west and zero on north or of large accelerations, e.g., speed south. If the vessel is accelerated on either of boats. Also seen with aircraft. Often these headings, the compass will indicate an observed when boat butts into head apparent turn to the north. When decelerating, sea, or planes down a swell while on the compass indicates a turn to the south. an east or west heading. A memory aid to remember the word “ANDS,” for Acceleration – North, Deceleration – South.
Oscillation Error Though listed as a separate error in some texts, this is actually a combination of the above errors. Results from erratic movements of the compass card caused by rough seas or abrupt helm changes. Helmsman has to “av- erage’’ out oscillations mentally for precise steering.
Heeling Error Of particular relevance to sailing vessels, this Adjusted for by heeling magnets on error arises from change in the horizontal some compasses.Adjustment is par- component of the induced or permanent tially a function of the magnetic magnetic fields at the compass due to rolling latitude of the vessel. or pitching of the ship. To a lesser extent heeling errors may be affected by the angle of plane of a powerboat.
note: See article by Kielhorn for details on some of these errors. L TABLE 2-5–Additional Compass Errors Which Arise if Vessel is not Straight and Level, and at Constant Speed
2-17 2 The Marine Magnetic Compass
pose that the mariner wishes to fol- courses to compass courses, and netic course. Since the variation low a magnetic heading of 000. vice versa. Although these calcula- is west, it is added to the true Reference to Table 2-4 shows that tions are quite simple, practice is course. The magnetic course is, on a magnetic heading of 000 the necessary to ensure familiarity. For therefore, 060 + 015 = 075. deviation is 2° east. Therefore, the this reason, the following text and J Second, from Table 2-4, the compass heading in this case would examples are given. deviation corresponding to a be 358. So, for a course of 000 It is often necessary to convert magnetic heading of 075 magnetic, the mariner should steer from true to compass headings or degrees is 5 degrees east. From 358. Under the heading “For” is bearings. As discussed in later the simple rule to add west in placed the magnetic course 000 and chapters, courses are laid out on this sequence, it follows that a under the heading “Steer” is placed nautical charts and, typically, mea- 5-degree easterly deviation 358. The table is completed to cre- sured with respect to true north. But would be subtracted. to undertake the voyage, the navi- ate a For/Steer card that is normally J Third, from the above steps, gator needs to determine how to posted next to the compass. the required compass course is convert this true course to a com- 075 - 005 = 070 degrees. pass course to steer. The overall COMPASS CALCULATIONS The important points to remem- sequence for this conversion is to Navigators need to become ber are the sequence of calculations start with the true course, add or familiar with the calculations nec- and whether to add or subtract vari- subtract variation to calculate a essary for converting from true ation and deviation. If all else fails, magnetic course, and then again reference to the nearest compass add or subtract deviation to calcu- ST G A U O A C R rose on the nautical chart will
S D Variation anD U
A U Y R late a compass course: True, Varia- X ILIA DeViation enable you to figure out whether to tion, Magnetic, Deviation, Com- add or subtract variation (or devia- pass, or as it is sometimes said, Variation is the angular tion). TVMDC. In addition to learning Sometimes it is necessary to difference between true the sequence of calculations, it is reverse the process, and convert useful to have a handy rule to and magnetic north—see from compass to true. For example, remember whether to add or sub- a bearing on a distant object may be Chapter 1. Variation is a tract variation and deviation. taken from the vessel’s compass, Throughout history there have function of the vessel’s loca- and it is necessary to convert this been a series of “salty” mnemonics bearing to true, before plotting on a tion on the earth. It can be used to help remember the TVMDC nautical chart. The sequence of cal- sequence. The current politically found on the nautical chart. culations is just the opposite of that correct mnemonic is TeleVision discussed above, i.e., CDMVT. As Deviation is the difference Makes Dull Children; Avoid Watch- well, the sign to apply to east or ing. Decoded, it reveals the between magnetic north and west variation or deviation is also sequence of calculations TVMDC reversed. That is, east is added, and compass north. It is particu- and the reminder (AW) to add west west is subtracted. Although this is when converting from true to com- lar to each vessel and is simple enough to remember, some pass. For example, what is the com- prefer to use the additional memory a function of the heading of pass heading to steer if the true aid: Can Dead Men Vote Twice? At course is 060, variation is 015 west, the vessel. Although related, Elections! The first letters are the and the deviation table is as given memory aid to the sequence: Com- these are distinct concepts. in Table 2-4? The answer is calcu- pass, Deviation, Magnetic, Varia- lated as follows: Do noT ConFuse tion, True, and Add East. (Some air- J First, start at the true course, craft pilots were taught the phrase: These TWo TerMs. 060, and convert it to the mag- Can Ducks Make Vertical Turns?)
2-18 The Marine Magnetic Compass 2
To illustrate, suppose that the compass heading of the vessel is
ST G A U O A C R
065 degrees and an object is sighted S D U loCal MaGnetiC DisturBanCe A U Y X R bearing directly ahead per the ves- ILIA sel’s compass in an area where the notes indicating magnetic disturbance are variation is 015 degrees west. What is the true bearing? Assuming that printed in magenta on u. s. charts. Where space the deviation table is as given in permits, these notes are printed in the specific area Table 2-4, the deviation on a com- pass heading of 065 degrees is 5 of local magnetic disturbance. here are some degrees east and, therefore, the examples of how these are shown: magnetic heading of the vessel is 065 + 005 = 070 degrees (add east). loCal MaGnetiC DisturBanCe In turn, the true heading is the mag- netic heading plus or minus varia- Differences from normal variation of as much tion. If east is to be added, then as 5° have been observed in Gastineau Channel west should be subtracted for this calculation, so the true heading is in the vicinity of Lat. 58° 15'. 070 – 015 = 055 true. That’s all there is to it. Practice until you are loCal MaGnetiC DisturBanCe proficient. Differences of 12° or more from normal varia- tion may be expected in X Channel in the vicin- ity of Z Point. Where limited by space, the full note is placed else- where on the chart and the following reference note shown (in magenta) in the area of the disturbance:
loCal MaGnetiC DisturBanCe PHOTO PHOTO COURTESY OF INDUSTRIES, KVH INC. L (see note) FIG. 2-8–Fluxgate Digital Compass. Mariners should exercise particular vigilance Both the fluxgate sensor and the Liquid Crystal Display (LCD) are enclosed in when operating in these areas. one watertight unit.
ADDITIONAL POINTERS introduced, as shown in Table 2-5. substantial acceleration (e.g., ON THE COMPASS It is not a good idea to use compass speedboats), and substantial angles It is important to remember that readings obtained while the vessel of heel or bank. (Consult the refer- compass readings are most accurate is heeling, turning, or accelerat- ences at the end of this chapter for only when the vessel is level (as ing/decelerating. The effects of more details.) Directional gyros or opposed to heeling), traveling at a these errors are to make the com- gyrocompasses are less prone to constant speed, and maintaining a pass difficult to read and/or to give these errors and sometimes favored constant course. Otherwise, a series erroneous indications. These errors by mariners for this reason (among of additional compass errors is are largest for vessels capable of others).
2-19 2 The Marine Magnetic Compass
LOCAL MAGNETIC mine if there are areas of local mag- the same, or different, units.) If sep- DISTURBANCES netic disturbance located along arate from the display unit, the sen- In some areas of the world, the your proposed route. Exercise extra sor can be located remotely, in an measured values of magnetic varia- vigilance when transiting these area of the vessel where magnetic tion differ from the expected (chart- areas. Do not rely entirely on the disturbances are at a minimum. The ed) values by several degrees. The compass; steer by reference to land- display unit is small and can be sources of these discrepancies are marks and/or ATONs, if possible, mounted for optimum visibility. termed local magnetic distur- and fix your position frequently. Most modern fluxgate systems are bances, local attractions, or mag- Obviously, you should not attempt integrated with microprocessors, netic anomalies. Magnetic distur- to calibrate a compass in an area of which can perform many useful bance notes identify such areas on known local magnetic disturbance. functions. The model, pictured in U. S. nautical charts where errors (Local magnetic disturbances are Figure 2-8, automatically compen- are greater than or equal to 2° (3° in not a compass error, per se. sates for deviation (to within +/- 1 Alaska). The note will indicate the Nonetheless, this magnetic phe- degree, in most cases) by simply location and magnitude of the dis- nomenon does affect the compass making a 360 degree turn with the turbance. The indicated magnitude and should be noted.) vessel! Other models can also dis- should not be considered as the play headings in either true or mag- largest possible value that may be THE FLUXGATE COMPASS netic (variation data are stored in encountered. Large disturbances Finally, any modern discussion the microchip) and can furnish elec- are more frequently encountered in of compasses would be incomplete tronic inputs to other navigation the shallow water areas near land- without, at least, a passing mention systems such as the Global Posi- masses (particularly mountains) of the fluxgate compass. The flux- tioning System (GPS), Loran-C, or than on the ocean. Fortunately, the gate compass senses the earth’s radar. effect of a local magnetic distur- magnetic field electronically, rather An electronic compass is very bance typically diminishes rapidly than with magnets. (Readers wish- convenient. However, it does not with distance. However, in some ing a more complete discussion eliminate the need for a magnetic locations there are multiple sources should refer to the bibliography.) compass, because electronics are of disturbances and the effects may The fluxgate compass consists of a dependent upon a reliable power be distributed for many miles. Read sensor and a display unit. (The sen- supply and are easily damaged in the nautical chart carefully to deter- sor and the display unit may be in the marine environment.
2-20 The Marine Magnetic Compass 2
SELECTED REFERENCES
Aczel A. D., (2001). The Riddle of the Compass, The Fuson, R. H. (Translator), (1987). The Log of Invention That Changed the World, Harcourt, Inc., Christopher Columbus, International Marine New York, NY. Publishing Company, Camden, ME.
Anon., (1988). The Magnetic Compass, Principles, Ganssle, J. G., (1989). Anatomy of a Fluxgate, Ocean Selection, Navigation, E. S. Ritchie & Sons, Inc., Navigator, September/October. Pembroke, MA. Hempstead, R. L., (1987). Magnetic Compasses in the Bowditch, N. (1995). American Practical Navigator, Small Boat Environment, Ocean Navigator, No. 12, An Epitome of Navigation, Pub. No. 9, Defense March/April, pp. 21 et seq. Mapping Agency Hydrographic/Topographic Center, Bethesda, MD. This publication is avail- Hewson, J. B., (1983). A History of the Practice of able electronically from the National Imagery and Navigation, Second Edition, Brown, Son & Mapping Agency (NIMA) Marine Navigation Ferguson, Ltd. Publishers, Glasgow, Scotland, UK. Department web site (http://www.nima.mil/). Jerchow, E., (1987). From Sextant to Satellite Brogden, B., (1995). Boat Navigation for the Rest of Navigation, 1837-1987, 150 Years, C. Plath, Ham- Us, Finding Your Way by Eye and Electronics, burg, Germany. International Marine, Camden, ME. Kaufman, S., (1978). Compass Adjusting for Small Cohan, L. S., (1988). Compass Deviation Affected Craft, Surfside Harbor Associates, Surfside, FL. by Lightning, Ocean Navigator, No. 17, Kielhorn, W. V., (1988). A Piloting Primer, privately January/February. printed at Naples, FL.
Collinder, P. A., (1955). History of Marine Navigation, Kielhorn, W. V., (1957). The Northerly Turning Error, St. Martin’s Press, Inc., New York, NY. The Rudder, Vol. 73, No. 2, pp. 40-42.
Dahl, N., (1983). The Yacht Navigator’s Handbook, Kielhorn, W. V., and H. W. Klimm, (1978). A Hearst Books, New York, NY. Preliminary Study of the Changes of Magnetic Defense Mapping Agency, Hydrographic/Topographic Structure in a New Steel Trawler, Navigation, Center, (1980). Handbook of Magnetic Compass Journal of the Institute of Navigation, Vol. 6, No. 6, Adjustment, Fourth Edition, Pub. No. 226, pp. 365 et seq. Washington, DC. Moody, A. B., (1980). Navigation Afloat: A Manual for Denne, W., revised by Cockcroft, A. N., (1979). the Seaman, Van Nostrand Reinhold, New York, Magnetic Compass Deviation and Correction, A NY. Manual of the Theory of the Deviations and Morrison, S. E., (1942). Admiral of the Ocean Sea, A Mechanical Correction of Magnetic Compasses in Life of Christopher Columbus, Little, Brown and Ships, Brown, Son & Ferguson, Ltd., Glasgow, Company, Boston, MA. Scotland. Queeney, T. E., (1985). Beyond the Lodestone, Ocean Department of Transportation, Federal Aviation Navigator, No. 3, September/October, pp. 33 et seq. Administration, (1987). Instrument Flying Hand- book, AC61-27C, Washington, DC. Queeney, T. E., (1987). Future Heading Systems, Are Lasers The Next Step, Ocean Navigator, No. 12, Eyges, L., (1989). The Practical Pilot, Coastal March/April, pp. 35 et seq. Navigation by Eye, Intuition and Common Sense, International Marine Publishing Co., Camden, ME.
2-21 2 The Marine Magnetic Compass
SELECTED REFERENCES
Rousmaniere, J., (1989). The Annapolis Book of Seamanship, Simon and Schuster, New York, NY.
Saunders, A. E., (1987). Small Craft Piloting and Coastal Navigation, Alzarc Enterprises, carborough, Ontario, Canada.
Van Heyningen, M. A. K., (1987). The Evolution of the Modern Electronic Compass, NMEA News, January/February.
2-22 Chapter 3
THE NAUTICAL CHART
“It would appear that on some [of the Marshall Islands]…these charts were considered so precious that they might not be taken to sea. This was partly because they might be damaged in the canoes and partly, perhaps, because the people might never come back, in which case the tribe’s precious property would be lost forever”. [Emphasis added]
–Per Collinder, A History of Marine Navigation
INTRODUCTION DIFFERENCES BETWEEN his chapter provides an intro- CHARTS AND MAPS Tduction to the nautical chart, At the outset, get in the habit of how it is constructed, how to deter- calling this a chart—not a map. A mine position, course, and distance map depicts information relevant to on the chart, how to read the chart, terrestrial travel and provides the and, finally, some practical ideas answers to such questions as: about chart interpretation and use. J What are the route numbers? The material in this chapter is not J difficult, but there is a lot to learn. Where do the roads lead? Read this chapter with a nautical J What are the distances between chart, preferably the 1210-Tr, close cities and towns? at hand. Refer to the chart often. J Which roads are improved and Don’t despair, it takes a great deal which are limited access roads? of experience to become fully J Where can you find services familiar with the wealth of relevant information depicted on the nauti- such as fuel, food, and lodging? cal chart! This chapter provides an J Where are the entrances to introduction to the nautical chart. national parks? As you work the homework prob- It is useful to know the answers lems throughout the course, you to these questions if you plan to will gradually become more famil- take a family camping vacation or a iar with the nautical charts and how business trip by automobile. The they are used. map generally emphasizes land-
3-1 PHOTO COURTESY OF UNITED STATES COAST GUARD 3 The Nautical Chart
forms (sometimes including the deal of information, much is omit- used, but also treated with rever- representation of relief) and high- ted—the height of a tower, for ence and care. To this group, a map ways with the shoreline represented example, or the precise locations of is something that can be purchased as an approximate delineation, usu- church spires, water towers, monu- at a gasoline station vending ally at mean sea level. Maps do not ments, and conspicuous dwellings, machine, located next to advertise- usually present detail on water would normally not be shown on a ments for recaps, a cooler full of hot areas. Maps depict roads but, typi- map because this information is of soda, and a dog with an infected cally, do not provide information on limited utility to the map user. ear. If you haven’t guessed already, the condition of any road, although The practice of marine naviga- mariners are snobs. (For that matter, this can sometimes be inferred by tion has unique information so are aircraft pilots, who refer to collateral information (e.g., requirements. Water depths, aids to their maps as “aeronautical whether or not a road is part of the navigation (ATONs) and their rele- charts.”) So, don’t risk being interstate system). vant attributes (radio frequencies, branded a “landlubber”; refer to a Although maps provide a great light colors, sectors, and character- chart by its proper name. istics), landmarks, unmarked haz-
ST G A U O A C R
S D What you Will U ards to navigation, land outlines, A SOURCE OF A U Y X R ILIA learn in this bridge clearances, distance, and VITAL INFORMATION Chapter direction, are all pertinent to marine As noted above, a marine chart J Chart projections navigation. The nautical chart is a depicts information of use for graphic portrayal of the marine marine navigation. This includes a J How to establish a posi- environment. Together with sup- host of data on navigable (and not- tion on a nautical chart plemental navigational aids, it is so-navigable) water and the con- J How to measure direc- used to define courses, fix a vessel’s tiguous land. As you read through tion and distance on a position, ensure the vessel does not the material in this chapter, think nautical chart stray into dangerous waters, and about why cartographers chose to J navigate vessels by a safe and effi- include this information on the Chart scales and their chart and how you could use it to significance cient route. A chart is normally a working advantage. In very broad terms, J Types of nautical document. Courses, lines of posi- information depicted on charts can charts tion (LOPs), fixes, waypoints, and be used to: J How soundings and other relevant data and information J orient the mariner and help bottom characteristics are plotted on the chart. In use, a to establish (fix) the position are depicted nautical chart normally has numer- of the vessel: Landmarks (e.g., ous marks, courses, LOPs, fixes, J spires, buildings, water towers, How heights are and annotations made by the depicted and tanks), geographic features mariner. And, unlike the practice of (e.g., mountains, elevation con- J How to read the early mariners in the Marshall tours), and ATONs (e.g., buoys, General Information Islands (see introductory quota- range markers) are depicted, Block on a chart tion), charts are intended to be car- inter alia (among other things), J Practical pointers on ried on board! In contrast, a map is to help fix the vessel’s position finding your position generally a static document, used as and mark the location of various on a chart a reference guide. channels. Parallels of latitude, Marine navigation, being both meridians of longitude, and J ATONs and dangers to an ancient art and science, has compass roses are included to navigation evolved its own prejudices and jar- enable the user to determine J Chart storage gon. To a mariner, a chart is a veri- geographic coordinates and to table treasure—something to be measure courses and distances.
3-2 The Nautical Chart 3
J highlight and locate possible The above list is by no means
ST G A U O A C R
S D
hazards to navigation: Water complete. It provides instructive U
A U Y X R ILIA Caution notes depths and the location of examples to stimulate your think- obstructions, shoals, rocks, ing. The amount, complexity, and Caution notes are included on sunken wrecks, and fish trap diversity of material presented on nautical charts to alert the areas are included to warn the typical nautical chart is astound- mariner to certain hazards. ing! Nautical cartography is a high- mariners of both marked and Examples of caution notes ly developed art and science. unmarked hazards to navigation. taken from several charts Presenting the required information Some of these data may have include: in easy-to-understand and compact multiple uses. For example, J Extremely heavy tide rips water depths can be used in voy- format requires integrating the efforts of those in numerous disci- and strong currents may be age planning to identify possible encountered in the vicinity “shortcuts” for the trip. Wrecks plines to select the “right” method of chart projection, appropriate of the islands shown on this may be of intrinsic interest to chart. divers and anglers. Nautical choice of scale, chart symbols, J Improved channels shown charts are annotated with a abbreviations, lettering styles, col- series of “caution” notes (see ors, paper, and printing techniques by broken lines are subject to shoaling, particularly at sidebar) that warn the mariner to produce today’s high-quality the edges. about various hazards to naviga- nautical chart. J tion. Mariners are warned that REPRESENTATION OF A J Facilitate voyage planning: numerous uncharted duck SPHERICAL SURFACE UPON blinds and fishing struc- Much information is provided A PLANE OR FLAT SURFACE tures, some submerged, may that facilitates voyage planning exist in the fish trap area. and/or the practice of good sea- It is impossible to represent a Such structures are not manship. For example, symbols spherical surface upon a flat surface charted unless known to be that identify the nature of the without introducing some distor- tion—in distance, direction, shape, permanent. bottom (sand, mud, rocks, grass) J provide information regarding and/or area. Even the school refer- Mariners are warned to stay ence globe made out of paper or the suitability of a possible clear of the protective riprap plastic printed on flat or rotary anchorage area and/or the type surrounding navigational presses is made up of gores of of anchor necessary to optimize light structures. essentially flat surfaces cut to bend holding power. J St. Lucie Inlet: The channel and fit upon a spherical surface. If J is subject to continual identify and locate areas of the globe were disassembled and its regulatory significance: change. Entrance buoys separate pieces laid out, one would and lights are not shown Restricted areas, prohibited have a flat surface where areas areas, and other related informa- because they are frequently would be “correct,” but there would shifted in position. tion is provided to alert the be huge gaps between the gores; mariner to areas that are subject and direction, shape, and distances Where space permits, caution to certain restrictions. would have no meaning in the notes are shown near to the J identify areas/objects of spe- spaces between, nor continuity hazard noted. However, space cific interest to particular user from one gore to another, except at constraints may make this groups: The location of desig- the equator where all gores are impossible. Read the chart nated anchorage areas, pilot joined. carefully to find all applicable operating areas, piers, and oil caution notes. platforms are of interest to spe- CHART PROJECTIONS cialized user groups. Throughout the history of navi-
3-3 3 The Nautical Chart
gation, there have been numerous one line) cones to provide the THE MERCATOR attempts to depict a round surface Mercator and the polyconic projec- PROJECTION with a flat one. Some have been tions, respectively. These are shown This projection has been one of remarkably successful under certain in Figure 3-2 as are the two key the most useful for navigation for conditions, but all such projections nautical chart projections. Each of over 400 years. It was developed by suffer some limitations. The goal of these projections has its particular a brilliant Flemish geographer by the various projections, a sampling utility and each has limitations. A the name of Gerhard Kremer of which is given in Figure 3-1, is to particular projection is chosen (latinized to Gerhardus Mercator) balance and minimize the distor- based upon the intended use. A who published a world chart con- tions to produce a representation Mercator projection, for example, structed by his method in 1569. The that preserves (to the extent possi- distorts areas (particularly near the Mercator projection is a cylindrical ble) direction, distance, shape, area, poles) substantially, and is unsuit- projection, ingeniously modified by and correct angular relationships. A able for depicting the relative size expanding the scale at increasing projection that preserves correct of countries. (Generations of stu- latitudes, to preserve shape, direc- angular relationships is termed con- dents have grown up believing that tion, and angular relationships. formal. This property, or a close Greenland, for example, is larger This projection is conformal, approximation to it, is essential if than the United States, because they the chart is to be used for naviga- have studied Mercator projections but distance and area relationships tion. where this is apparently true. In are distorted. Both the meridians No chart projection is fully ade- actual fact, the United States is and the parallels are expanded at quate over a large area, but several more than 4.3 times larger than the same ratio with increasing lati- are sufficiently so to be useful to the Greenland.) tude. For the technically minded the small craft navigator. For naviga- These projections, their devel- expansion is equal to the secant of tion charts, the spherical surface of opment and use for small craft nav- the latitude (secant H = 1/cos H), the earth has been projected on a igation are discussed in some detail with a small correction to reflect the cylinder and, also, on a series of in this section. fact that the earth is not a perfect coaxial, tangent (touching the sphere. The projection does not earth’s surface at one point or along include the poles and usually not even the uppermost 15° of latitude, because the value of the secant at GENERAL CHARTS Azimuthal-Equidistant these angles is too large, being Gall-Peters infinity at Lat. 90° (N or S). Since Goode Homolosine Lambert Azimuthal Equal Area the expansion is the same for all Lambert Conformal directions and angular relationships Miller Cylindrical are correctly indicated, the projec- Mollweide tion is conformal and compass Orthographic directions (rhumb lines or loxo- Polar Stereographic dromes) are shown as straight Polar Gnomonic lines—properties of value to the Robinson mariner. Simple Conic Sinusoidal Distances can be measured Van der Grinten directly, but not by a single distance scale for the whole chart (unless a CHARTS OF PARTICULAR Mercator large-scale chart is used, see below) INTEREST TO THE MARINER Polyconic or for large areas. Instead, the lati- tude scale is used along any merid- L FIG. 3-1–Illustrative Projections
3-4 The Nautical Chart 3
L FIG. 3-2– Mercator and Conic Projections ian. (Remember, 1° Lat. = 60 M, 1’ COORDINATES FOR THE example, sell Mercator projections Lat. = 1 M.) Great circles appear as MERCATOR PROJECTION in novelty shops with south at the curved lines on the Mercator pro- The format for the Mercator top of the chart! Closer to home, jection except for the meridians and projection is rectangular. Latitude some nautical charts of rivers are the equator, which appear as and longitude are the coordinates typically not aligned north up in the straight lines. Note: The Mercator used for the Mercator projection. interests of saving space.) projection may also be made as an The parallels of latitude usually The meridians appear as oblique projection (at an angle to appear as horizontal, straight lines, straight, parallel lines running from the bottom of the chart to its top. the equator or meridian), using any running from the right to the left (in The scale for the meridians great circle (rather than the equator) the western hemisphere), with the projections oriented such that north (longitude scale) is indicated on the for the base line. Such a projection is at the top of the chart and south at top and bottom margins of the is termed an oblique Mercator pro- the bottom, east at the right margin, chart. The scale for the parallels jection and is used for special navi- and west at the left. (There are some (latitude scale) is provided on the gation applications, which are nautical charts based on Mercator right- and left-hand margins, and is beyond the scope of this course. projections where, for various rea- also used for distance measure- sons, north does not appear at the ment. Compass roses, indicating top of the page. The Australians, for true and magnetic directions, are
3-5 3 The Nautical Chart
and draw a light pencil line from and closed”—with one edge
ST G A U O A C R
S D historiCal U this point across the chart paral- along a parallel of latitude
A U Y X R ILIA Footnote lel to the top, bottom, and other shown on the chart. Holding the Mercator was active in the parallels on the chart. (Use of a base ruler along the parallel, parallel rule or paraline plotter swing the other ruler to the Protestant Reformation. His makes this easy.) Every point on desired latitude value on the left career nearly came to an end this line has that same latitude. or right scale. A light pencil line in 1544 when Mary, Queen J To specify the position uniquely, is drawn only in the vicinity of Dowager of Hungary, had now use the longitude scale at the approximate longitude, him imprisoned as a heretic. the top or the bottom of the chart which is “eyeballed” or estimat- (these scales are along parallels) ed from the longitude scale at She issued an edict that all the top or bottom of the chart. heretics should be put to to locate the desired longitude value and strike another light J After the latitude line has been death. Mercator was one of pencil line up or down, parallel drawn, take the dividers and set forty-three persons con- to the meridians and the sides of their points so that one point demned at Louvain but was the chart. All points on this line falls on the nearest meridian of saved by the intercession of (itself, a meridian) are at the longitude and the other at the value of longitude desired. Now, the parish curate, reportedly same longitude. Where the two light pencil lines intersect, the bring the dividers, carefully so a clever man and shrewd position is uniquely specified. as not to disturb the setting, debater. Fortunately for down along the meridian until modern mariners, Mercator USE OF PARALLEL RULERS the desired latitude line (paral- stuck to making maps after AND DIVIDERS TO PLOT lel) is encountered. If the line crosses the meridian, simply this experience. For more A POSITION ON THE MERCATOR PROJECTION measure along the latitude line information, see Wilford (parallel) with the dividers from (1982) in the references at Parallel rulers and the dividers the meridian. Where the other help to minimize unnecessary the end of this chapter. point of the dividers falls is the marks on the chart while plotting a desired longitude. The two coor- position. (Interrupt your reading of dinates now specify the vessel’s placed at convenient locations on this chapter to take a few minutes to position, uniquely. If the latitude the chart. read about parallel rules and line (parallel) does not cross the dividers in Chapter 4.) meridian, simply swing the par- ESTABLISHING A POSITION A common task in navigation is allel rulers (keeping the base USING THE MERCATOR to plot a position on the chart. For ruler along the parallel) so that PROJECTION example, a navigator may read the the other ruler falls along the Since the Mercator projection vessel’s present position in latitude desired parallel and crosses the results in a rectangular presenta- and longitude from a Global meridian, as well. Then, as tion, a rectangular coordinate sys- Positioning System (GPS) or Loran- above, measure the increment of tem using latitude and longitude C receiver (see Chapter 9) and wish longitude from the meridian makes establishing a specific posi- to plot this position on the chart. along the parallel ruler to the tion on the globe an easy process on The technique is simple and is illus- position. the chart: trated in Figure 3-3: J The process can also be used J Using the latitude scale at the J Place the parallel rulers—which with the meridian first, and the right or left margins (these are two straight edges con- dividers set off of the parallel scales are along meridians), strained to remain parallel as and the latitude scale. In addi- simply take the latitude value they are “walked” or “opened tion, the dividers may be used
3-6 The Nautical Chart 3
to the top or the bottom of the Long. 77˚ 40' W Longitude Scale chart and measure from the meridian along the longitude 78˚ 77˚ 76˚ scale to determine the value of Parallel the longitude increment. Read 34˚ the longitude directly under the point of the dividers. J The dividers can be used alone, without the rulers, keeping them Lat. 33˚ 19' N Lat. 33˚ 19' N parallel by eye, as above. Long. 77˚ 40' W Parallel Practice with the rulers/dividers will develop sufficient confi- dence and familiarity with the 33˚ process, to the point that the Parallel rulers will no longer be