The Blue God Ktdjstizu V Suwvula..T P Jnogv Ganuu Inq `Usvaijs Ijng Dill Vv Umouq Jud.Un7 Uva.)O Jva.2

Total Page:16

File Type:pdf, Size:1020Kb

The Blue God Ktdjstizu V Suwvula..T P Jnogv Ganuu Inq `Usvaijs Ijng Dill Vv Umouq Jud.Un7 Uva.)O Jva.2 By William H. MacLeish The Blue God Ktdjstizu v suwvula..t p jnogv ganuu inq `usvaiJs Ijng dill vv umouq Jud.un7 uva.)o Jva.2.. aqj uo sapz.c pagapzq aavq s.tdu. uvul saunjuaa 2OJ First of a two-part series "Look for a tide rip in about 90 minutes," the captain search program to see how its ships could best use the of the chemical carrier Exxon Wilmington told his Stream's currents to cut fuel consumption and save deck officer. "It'll be setting southeast to northwest." time on the voyage north, Wonson worked with marine The captain, Larry Wonson, was looking for markers scientists assigned to his vessel. that would set him up for a free ride on the most Now to help him search for the west wall, the spectacular current system in the world. The tide Wilmington's captain has Coast Guard reports on cur- rip was one of them. Another lay ahead: the west rent location and velocity. But he still relies more on any wall, which is the inshore edge of the current, nearest hunter's truest friend, instinct built from experience. Florida. Once he'd found that, he would set a parallel Ragged lines of drifting weeds tell him something of course about a dozen miles out to sea, and we would what is going on at the surface and below. The current probably be close to where the current flows fastest. often runs dark blue, and so he keeps an eye out for in- With summer coming on, the west wall is likely to be digo. He looks for lines of squalls that sometimes build pretty close to shore. Maybe. over the west wall where different water masses meet. The Wilmington was running through the Straits of And he runs regular checks on the temperature of sea- Florida, the narrow sea separating the Florida penin- water in the engine intake. Especially near the surface, sula from Cuba and the broad shallows that surround the Gulf Stream system railroads enormous amounts of the Bahama Islands. She shuttles lubricating oils and warm water northward; if the temperature at the intake plasticizers from Exxon's refinery in Louisiana to New drops, you've probably missed your best connection. Jersey. When I boarded at Baton Rouge, we ran down Wonson started hitchhiking back when we were still the Mississippi to the Gulf of Mexico. I watched the in the Gulf of Mexico, taking advantage of an exten- river roiling its load of stolen silts and thought of the names it has carried. Indians had called it the Father of Waters, others simply Old Man River. The metaphor for me came from T. S. Eliot, who lived by the Mississippi as a boy. "I do not know much about gods," Eliot wrote in The Dry Salvages, "but I think that the river / Is a strong brown god-sullen, untamed and intractable." Why are there palm trees on the Scilly Isles? I was looking for a god of another color. A blue god. I was working on a hook about the Gulf Stream, the mysterious current that has also been called a river in the ocean, about its effect on the North Atlantic and the climate and civilizations of the lands bordering it. For almost five centuries the Stream has served sailors crossing the Atlantic, determining trade routes and landfalls. Yet even as early mariners used it, they did not understand it. We do not even fully understand it today. The long held and seemingly logical notion that the warming Stream, running against the shore, helps palm trees grow in Ireland, the Scilly Isles and Brittany has proved not quite true. My reporting would mean several years of voyaging, not all of it on the Gulf Stream itself. I would also sail on, dive in and fly over sister currents that form a great swirl in the ocean, called a gyre. The Wilmington was a good ship to set out in. Every two weeks she enters the Stream. Her skipper is on speaking terms with the blue god. His crew calls him the Gulf Stream guru. Wonson grew up in Rockport, Massachusetts, minored in oceanography at the Maine Maritime Academy and has been on the Exxon East- Winslow Homer's theatrical painting Gulf Stream coast run for 15 years. When the company began a re- stirred viewers' worry over fate of drifting mariner. 46 sion of the Gulf Stream system that scientists call the and small desk way over to starboard, and there I sat, Loop Current. The Loop pokes up between Cuba and 86 feet above the sea and almost 500 aft of the bow. A Mexico through the Yucatan Channel, shedding eddies perfect place for reading and jotting down notes, and that swirl off into the Gulf. Most skippers rounding the sending the mind out to settle on the sea. thumb of Florida pull out of the current at a point I was disappointed by what I saw. During a decade of from which they can steam a geographically direct work editing a magazine of oceanography, I had devel- course. By contrast, Exxon captains follow the Loop oped some idea of the Gulf Stream's power. By now, for 10 or 15 miles beyond that point. Then they head the Wilmington was well into the Florida Current, up for the Dry Tortugas, west of the Florida Keys, to which runs from the Straits up the coast to Cape get an optimal push from this tributary of the blue Hatteras. It is there, according to many oceanogra- god. The Wilmington did that and saved half an hour, phers, that the current becomes the true Gulf Stream, maybe a little more. Then she skirted the Keys and flowing out eastward toward the Grand Banks of New- closed on Miami, making 20.5 knots as against the foundland. The Florida Current, in fact, transports 16.5 she can do in slack water. Larry Wonson grinned water at a rate of about 30 million cubic meters per as he read the speed indicator and said, "I sense the second. (A cubic meter of seawater would fill a giant presence of external assistance." claw-foot bathtub to overflowing.) The current con- When you're an observer aboard a working ship, it's stantly changes speed and direction. At its fastest it best to stay on the bridge, if the captain will allow it, does five knots or a bit more. On land, a jogger can out of the way in some corner where you can watch go much faster. But try swimming against a five-knot and be forgotten. Wonson let me take over a high chair current. Faced with less than a knot of flow, divers wearing swim fins cannot move against it for long unless there is bottom nearby to crawl along. Such a giant of motion should show itself, I thought, muscling up as a big river does, a multiplication of Mississippis. But no. To my untutored eye at least, we could have been running through just about any part of the subtropical Atlantic. Wonson found his west wall and pointed it out to me. It turned out to be just a slick on the surface a couple of miles off, puny for the boundary of a god's domain. "If we were to cross the edge head-on," he said, "you'd see your wake in the distance moving north with the main current and your near wake moving south in the countercurrent." The edge, in fact, is often so sharp that you can cross it in a ship's length or two. More flow than all the rivers in the world Up near the Grand Banks, the Stream is somewhat cooler and runs slower, but the volume of water it transports increases to at least 150 million cubic meters per second, something like 100 times the flow of water in all the rivers in all the countries of the world. A great-grandfather of waters, indeed, yet a flow often masked by fogs created by its passage under the cold air coming off the Canadian Maritime Provinces. Storms can make the Stream dramatically visible. A northeaster blowing down against the current combs it into nasty steep waves that make sailors miserable. The Wilmington ran into such a storm on a recent trip. Nothing of consequence got bent, but the crew took a beating, and the ship lost a lot of time. On this passage, though, the sea simply dozed. Swells on their "He was not eaten by sharks," Homer asserted, "and way to the sands of Florida slipped across the bow in was rescued by a passing ship not in the picture." close order, following on in a rhythm slow as sleep. In 47 The Stream and its mysteries such a duck pond, it was difficult to believe that there was a giant below, carrying me along as the demon beneath the keel carried the Ancient Mariner. It was even more difficult during the first days of European exploration . Ships then were blocky and slow. They could run before the wind or reach across it, but could beat toward it only obliquely and only with great difficulty. Against a wind and current, they were all but helpless. If the blue god caught them, escape could be difficult. There was little they could do but wait for a breeze from the right quarter . Chris- topher Columbus made the first reported crossing of the North Atlantic, running before the trade winds along the southern arc of the Gulf Stream's gyre (see map on pp.
Recommended publications
  • The Gulf Stream
    The Gulf Stream Prepared by Distribution Branch Physical Science Services Section October 1985 (Educational Pamphlet No. 11) U.S. DEPARTMENT OF COMMERCE National Oceanic And Atmospheric Administration National Ocean Service U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Ocean Service Rockville, Maryland The Gulf Stream, a vast and powerful Atlantic Ocean cutrent, is first discernible in the Straits of Florida. In this area, the Stream is like a river 40 miles wi~e, 2,000 feet deep, flowin~ at a velocity of five miles an hour, and discharging 100 billion tons of water per hour. From the Straits of Florida, it takes a very narrow course up the North American coast to Newfoundland and then veers toward Europe (Fig. 1). Within the Straits, the lateral boundaries of the Gulf Stream are fairly well fixed, but when it flows into the open sea its boundaries become indefinite. Northeast of Cape Hatteras, the Stream often forms great looping meanders which change position with time. The major axis of the Stream within the Straits of Florida is known to mi~rate laterally; that is, it moves closer to or farther from the coast. As with most large natural phenomena, the Gulf Stream has given rise to a number of amazing legends--the products of much imagination and only a little knowledge. Early ideas were restricted by the very crude description of the Stream then available and, more importantly, by the fact that there was no well-developed knowledge of t'his physical characteristics--the velocity, volume, position, andvariation of flow.
    [Show full text]
  • Lesson 8: Currents
    Standards Addressed National Science Lesson 8: Currents Education Standards, Grades 9-12 Unifying concepts and Overview processes Physical science Lesson 8 presents the mechanisms that drive surface and deep ocean currents. The process of global ocean Ocean Literacy circulation is presented, emphasizing the importance of Principles this process for climate regulation. In the activity, students The Earth has one big play a game focused on the primary surface current names ocean with many and locations. features Lesson Objectives DCPS, High School Earth Science Students will: ES.4.8. Explain special 1. Define currents and thermohaline circulation properties of water (e.g., high specific and latent heats) and the influence of large bodies 2. Explain what factors drive deep ocean and surface of water and the water cycle currents on heat transport and therefore weather and 3. Identify the primary ocean currents climate ES.1.4. Recognize the use and limitations of models and Lesson Contents theories as scientific representations of reality ES.6.8 Explain the dynamics 1. Teaching Lesson 8 of oceanic currents, including a. Introduction upwelling, density, and deep b. Lecture Notes water currents, the local c. Additional Resources Labrador Current and the Gulf Stream, and their relationship to global 2. Extra Activity Questions circulation within the marine environment and climate 3. Student Handout 4. Mock Bowl Quiz 1 | P a g e Teaching Lesson 8 Lesson 8 Lesson Outline1 I. Introduction Ask students to describe how they think ocean currents work. They might define ocean currents or discuss the drivers of currents (wind and density gradients). Then, ask them to list all the reasons they can think of that currents might be important to humans and organisms that live in the ocean.
    [Show full text]
  • Documenting Inuit Knowledge of Coastal Oceanography in Nunatsiavut
    Respecting ontology: Documenting Inuit knowledge of coastal oceanography in Nunatsiavut By Breanna Bishop Submitted in partial fulfillment of the requirements for the degree of Master of Marine Management at Dalhousie University Halifax, Nova Scotia December 2019 © Breanna Bishop, 2019 Table of Contents List of Tables and Figures ............................................................................................................ iv Abstract ............................................................................................................................................ v Acknowledgements ........................................................................................................................ vi Chapter 1: Introduction ............................................................................................................... 1 1.1 Management Problem ...................................................................................................................... 4 1.1.1 Research aim and objectives ........................................................................................................................ 5 Chapter 2: Context ....................................................................................................................... 7 2.1 Oceanographic context for Nunatsiavut ......................................................................................... 7 2.3 Inuit knowledge in Nunatsiavut decision making .........................................................................
    [Show full text]
  • A Changing Nutrient Regime in the Gulf of Maine
    ARTICLE IN PRESS Continental Shelf Research 30 (2010) 820–832 Contents lists available at ScienceDirect Continental Shelf Research journal homepage: www.elsevier.com/locate/csr A changing nutrient regime in the Gulf of Maine David W. Townsend Ã, Nathan D. Rebuck, Maura A. Thomas, Lee Karp-Boss, Rachel M. Gettings University of Maine, School of Marine Sciences, 5706 Aubert Hall, Orono, ME 04469-5741, United States article info abstract Article history: Recent oceanographic observations and a retrospective analysis of nutrients and hydrography over the Received 13 July 2009 past five decades have revealed that the principal source of nutrients to the Gulf of Maine, the deep, Received in revised form nutrient-rich continental slope waters that enter at depth through the Northeast Channel, may have 4 January 2010 become less important to the Gulf’s nutrient load. Since the 1970s, the deeper waters in the interior Accepted 27 January 2010 Gulf of Maine (4100 m) have become fresher and cooler, with lower nitrate (NO ) but higher silicate Available online 16 February 2010 3 (Si(OH)4) concentrations. Prior to this decade, nitrate concentrations in the Gulf normally exceeded Keywords: silicate by 4–5 mM, but now silicate and nitrate are nearly equal. These changes only partially Nutrients correspond with that expected from deep slope water fluxes correlated with the North Atlantic Gulf of Maine Oscillation, and are opposite to patterns in freshwater discharges from the major rivers in the region. Decadal changes We suggest that accelerated melting in the Arctic and concomitant freshening of the Labrador Sea in Arctic melting Slope waters recent decades have likely increased the equatorward baroclinic transport of the inner limb of the Labrador Current that flows over the broad continental shelf from the Grand Banks of Newfoundland to the Gulf of Maine.
    [Show full text]
  • The Benjamin Franklin and Timothy Folger Charts of the Gulf Stream
    The Benjamin Franklin and Timothy Folger Charts of the Gulf Stream Philip L Richardson Woods Hole Oceanographic Institution Woods Hole, MA 02543 [email protected] [email protected] 1 Introduction In September 1978 I found two prints of the first Franklin-Folger chart of the Gulf Stream in the Bibliothèque Nationale in Paris. Although this chart had been mentioned by Franklin in 1786, all copies of it had been “lost”1 for many years. The Franklin-Folger chart was not only excellent for its time,2 but it remains today a good summary of the general characteristics of the Gulf Stream. Because of its historical role in our understanding of the Stream and in the development of oceanography, I would like to discuss its depiction of the Gulf Stream relative to later charts and recent measurements. There are three versions of the Franklin-Folger chart; the first was printed in 1769 by Mount and Page in London, the second was printed circa 1780- 1783 by Le Rouge in Paris, and a third was published in 1786 by Franklin in Philadelphia. The last is the most widely known and reproduced of the three. However, its projection is different from the first two, and the Gulf Stream has been modified. Since no copies of the first version had been located, some historians had doubted it had ever been printed (Brown 1938). Indeed, until a print of the first chart was discovered, the oldest known Gulf Stream chart was not by Franklin and Folger but one published by De Brahm in 1772. 1 A note describing the discovery and showing a facsimile of the whole chart was published by Richardson (1980).
    [Show full text]
  • Seasonal Variations of Sea Surface Height in the Gulf Stream Region*
    VOLUME 29 JOURNAL OF PHYSICAL OCEANOGRAPHY MARCH 1999 Seasonal Variations of Sea Surface Height in the Gulf Stream Region* KATHRYN A. KELLY,1 SANDIPA SINGH, AND RUI XIN HUANG Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts (Manuscript received 2 October 1996, in ®nal form 12 March 1998) ABSTRACT Based on more than four years of altimetric sea surface height (SSH) data, the Gulf Stream shows distinct seasonal variations in surface transport and latitudinal position, with a seasonal range in the SSH difference across the Gulf Stream of 0.14 m and a seasonal range in position of 0.428 lat. The seasonal variations are most pronounced west (upstream) of about 638W, near the Gulf Stream's warm core. The changes in the SSH difference across the Gulf Stream are successfully modeled as a steric response to ECMWF heat ¯uxes, after removing the large SSH variations due to seasonal position changes of the Gulf Stream. A phase shift between predicted and observed SSH changes in the Gulf Stream suggests that advection may be important in the seasonal heat budget. Consistent with the interpretation of SSH variations as steric, comparisons with hydrographic data suggest that the fall maximum SSH difference is from the upper 250 m of the water column. The maximum volume transport is in the spring. Zonally averaged indices are used to quantify seasonal changes in the Gulf Stream, which are analogous to changes in the atmospheric jet stream. 1. Introduction inverted echo sounders suggest that the SSH ¯uctuations do re¯ect changes in upper-layer transport (Teague and Sea surface height (SSH), as measured by a radar Hallock 1990; Kelly and Watts 1994; Hallock and altimeter, contains the signature of several ocean pro- Teague 1993).
    [Show full text]
  • The Antarctic Circumpolar Ocean Current
    The Antarctic Circumpolar Ocean Current A review of its influence on global ocean currents and climate within Antarctica and Europe James S. B. Mason GCAS Class 2006-7 Department of Antarctic Studies and Research University of Canterbury Abstract This review examines the operation of the Antarctic Circumpolar ocean current, its role in the so-called ‘great ocean conveyor belt’ of worldwide ocean currents and its influence on climate, particularly in northern Europe. The development in the understanding of ocean currents and their driving forces is described using historical sources, starting from the observations of early explorers to modern scientific analysis. The interaction of the Antarctic Circumpolar current within the ocean conveyor belt and its influence on worldwide oceanic flow is reviewed with reference to its effect on the Gulf Stream The associated implications for climate change within Antarctica and Europe are discussed in the context of recently proposed scenarios. 2 Introduction The Antarctic Circumpolar Current ( ACC ) encircles Antarctica, flowing from west to east, and stretches over twenty thousand kilometers forming the world’s largest ocean current. The average flow rate is estimated (1) at 135 million cubic metres of water per second ( 135x106 m3 s-1 ) or 135 Sverdrup ( Sv ) with 1 Sv being the estimated flow of all the world’s rivers combined. Although the flow rate of the current is low, less than 20 cm s-1, the current can reach a width of 2000km and depths of 2000-4000m which accounts for the huge flow rate. The absence of any continental landmass allows the ACC to circulate around the globe allowing water transfer between oceans.
    [Show full text]
  • Lecture 4: OCEANS (Outline)
    LectureLecture 44 :: OCEANSOCEANS (Outline)(Outline) Basic Structures and Dynamics Ekman transport Geostrophic currents Surface Ocean Circulation Subtropicl gyre Boundary current Deep Ocean Circulation Thermohaline conveyor belt ESS200A Prof. Jin -Yi Yu BasicBasic OceanOcean StructuresStructures Warm up by sunlight! Upper Ocean (~100 m) Shallow, warm upper layer where light is abundant and where most marine life can be found. Deep Ocean Cold, dark, deep ocean where plenty supplies of nutrients and carbon exist. ESS200A No sunlight! Prof. Jin -Yi Yu BasicBasic OceanOcean CurrentCurrent SystemsSystems Upper Ocean surface circulation Deep Ocean deep ocean circulation ESS200A (from “Is The Temperature Rising?”) Prof. Jin -Yi Yu TheThe StateState ofof OceansOceans Temperature warm on the upper ocean, cold in the deeper ocean. Salinity variations determined by evaporation, precipitation, sea-ice formation and melt, and river runoff. Density small in the upper ocean, large in the deeper ocean. ESS200A Prof. Jin -Yi Yu PotentialPotential TemperatureTemperature Potential temperature is very close to temperature in the ocean. The average temperature of the world ocean is about 3.6°C. ESS200A (from Global Physical Climatology ) Prof. Jin -Yi Yu SalinitySalinity E < P Sea-ice formation and melting E > P Salinity is the mass of dissolved salts in a kilogram of seawater. Unit: ‰ (part per thousand; per mil). The average salinity of the world ocean is 34.7‰. Four major factors that affect salinity: evaporation, precipitation, inflow of river water, and sea-ice formation and melting. (from Global Physical Climatology ) ESS200A Prof. Jin -Yi Yu Low density due to absorption of solar energy near the surface. DensityDensity Seawater is almost incompressible, so the density of seawater is always very close to 1000 kg/m 3.
    [Show full text]
  • Global Ocean Surface Velocities from Drifters: Mean, Variance, El Nino–Southern~ Oscillation Response, and Seasonal Cycle Rick Lumpkin1 and Gregory C
    JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS, VOL. 118, 2992–3006, doi:10.1002/jgrc.20210, 2013 Global ocean surface velocities from drifters: Mean, variance, El Nino–Southern~ Oscillation response, and seasonal cycle Rick Lumpkin1 and Gregory C. Johnson2 Received 24 September 2012; revised 18 April 2013; accepted 19 April 2013; published 14 June 2013. [1] Global near-surface currents are calculated from satellite-tracked drogued drifter velocities on a 0.5 Â 0.5 latitude-longitude grid using a new methodology. Data used at each grid point lie within a centered bin of set area with a shape defined by the variance ellipse of current fluctuations within that bin. The time-mean current, its annual harmonic, semiannual harmonic, correlation with the Southern Oscillation Index (SOI), spatial gradients, and residuals are estimated along with formal error bars for each component. The time-mean field resolves the major surface current systems of the world. The magnitude of the variance reveals enhanced eddy kinetic energy in the western boundary current systems, in equatorial regions, and along the Antarctic Circumpolar Current, as well as three large ‘‘eddy deserts,’’ two in the Pacific and one in the Atlantic. The SOI component is largest in the western and central tropical Pacific, but can also be seen in the Indian Ocean. Seasonal variations reveal details such as the gyre-scale shifts in the convergence centers of the subtropical gyres, and the seasonal evolution of tropical currents and eddies in the western tropical Pacific Ocean. The results of this study are available as a monthly climatology. Citation: Lumpkin, R., and G.
    [Show full text]
  • Atlantic Ocean Equatorial Currents
    188 ATLANTIC OCEAN EQUATORIAL CURRENTS ATLANTIC OCEAN EQUATORIAL CURRENTS S. G. Philander, Princeton University, Princeton, Centered on the equator, and below the westward NJ, USA surface Sow, is an intense eastward jet known as the Equatorial Undercurrent which amounts to a Copyright ^ 2001 Academic Press narrow ribbon that precisely marks the location of doi:10.1006/rwos.2001.0361 the equator. The undercurrent attains speeds on the order of 1 m s\1 has a half-width of approximately Introduction 100 km; its core, in the thermocline, is at a depth of approximately 100 m in the west, and shoals to- The circulations of the tropical Atlantic and PaciRc wards the east. The current exists because the west- Oceans have much in common because similar trade ward trade winds, in addition to driving divergent winds, with similar seasonal Suctuations, prevail westward surface Sow (upwelling is most intense at over both oceans. The salient features of these circu- the equator), also maintain an eastward pressure lations are alternating bands of eastward- and west- force by piling up the warm surface waters in the ward-Sowing currents in the surface layers (see western side of the ocean basin. That pressure force Figure 1). Fluctuations of the currents in the two is associated with equatorward Sow in the thermo- oceans have similarities not only on seasonal but cline because of the Coriolis force. At the equator, even on interannual timescales; the Atlantic has where the Coriolis force vanishes, the pressure force a phenomenon that is the counterpart of El Ninoin is the source of momentum for the eastward Equa- the PaciRc.
    [Show full text]
  • Ocean Surface Circulation
    Ocean surface circulation Recall from Last Time The three drivers of atmospheric circulation we discussed: • Differential heating • Pressure gradients • Earth’s rotation (Coriolis) Last two show up as direct forcing of ocean surface circulation, the first indirectly (it drives the winds, also transport of heat is an important consequence). Coriolis In northern hemisphere wind or currents deflect to the right. Equator In the Southern hemisphere they deflect to the left. Major surfaceA schematic currents of them anyway Surface salinity A reasonable indicator of the gyres 31.0 30.0 32.0 31.0 31.030.0 33.0 33.0 28.0 28.029.0 29.0 34.0 35.0 33.0 33.0 33.034.035.0 36.0 34.0 35.0 37.0 35.036.0 36.0 34.0 35.0 35.0 35.0 34.0 35.0 37.0 35.0 36.0 36.0 35.0 35.0 35.0 34.0 34.0 34.0 34.0 34.0 34.0 Ocean Gyres Surface currents are shallow (a few hundred meters thick) Driving factors • Wind friction on surface of the ocean • Coriolis effect • Gravity (Pressure gradient force) • Shape of the ocean basins Surface currents Driven by Wind Gyres are beneath and driven by the wind bands . Most of wind energy in Trade wind or Westerlies Again with the rotating Earth: is a major factor in ocean and Coriolisatmospheric circulation. • It is negligible on small scales. • Varies with latitude. Ekman spiral Consider the ocean as a Wind series of thin layers. Friction Direction of Wind friction pushes on motion the top layers.
    [Show full text]
  • The Gulf Stream Structure and Strategy W.Frank Bohlen Mystic, Connecticut [email protected]
    The Gulf Stream Structure and Strategy W.Frank Bohlen Mystic, Connecticut [email protected] January, 2012 For the Newport-Bermuda racer the point at which the Gulf Stream is encountered is often considered a juncture as important as the start or finish of the Race. The location, structure and variability of this major ocean current and its effects presents a particular challenge for every navigator/tactician. What is the nature of this challenge and how best might it be addressed ? The Gulf Stream is a portion of the large clockwise current system affecting the entire North Atlantic Ocean. Driven by the wind field over the North Atlantic and the associated distributions of water temperature and salinity, the Gulf Stream is an energetic boundary current separating the warm waters of the Sargasso Sea from the cooler continental shelf waters adjoining New England. The resulting thermal boundary represents one of the most striking features of this current and one that is most easily measured. From Florida to Cape Hatteras the Gulf Stream follows a reasonably well defined northerly track along the outer limits of the U.S. continental shelf. Beyond, to the north of Hatteras, Stream associated flows proceed along a progressively more northeasterly tending track with the main body of the current separating gradually from the shelf. Horizontal flow trajectories in this area, which includes the rhumb line to Bermuda, become increasingly non-linear and wavelike with characteristics similar to those observed in clouds of smoke trailing downwind from a chimney. The resulting large amplitude meanders in the main body of the Stream tend to propagate downstream, towards Europe, and grow in amplitude.
    [Show full text]