Comprehensive Guide to Hydrographic Surveying Credits: 5 PDH

Total Page:16

File Type:pdf, Size:1020Kb

Comprehensive Guide to Hydrographic Surveying Credits: 5 PDH Comprehensive Guide to Hydrographic Surveying Credits: 5 PDH Course Description Hydrography is the science of measuring and describing the topographical features and the entire aquatic environment as a whole, beneath the surface of water bodies. These subsurface features affect bridge scour, flood mitigation, erosion control and siltation transport, maritime navigation, marine construction, dredging, offshore oil exploration and offshore oil drilling, among many other activities. Hydrographic surveying does not strictly apply to coastal and oceanic regions of the US. Hydrographic surveying has many applications inland. Many environmental and civil engineering project in and around bodies and channels of water (streams and rivers, lakes and ponds, wetlands) can all benefit from hydrographic surveys and analysis. Topics Intro and overview of hydrographic surveying History and early methods of measurement Sounding poles, lead lines, wire drags Echo sounders and fathometers Agencies which perform hydrographic surveys: office of coast survey, NOAA, USGS, COE, IHO, NOO Marine magnetometry DC resistivity imaging Radar altimetry GPR for marine applications SONAR devices: side scan, single beam, multi beam sonar Light Pulse (LIDAR) devices US maritime limits and boundaries Sources of existing bathymetric datasets Types of tidal datums (sounding and chart) and tidal cycles Online-PDH 1265 San Juan Dr. AUV, ROV and UAS technologies Merritt island, FL 32952 Crowdsourced bathymetric surveying Fisheries acoustics Original Courseware by: Donald W. Parnell, PE All rights reserved Chapter 1: Introduction Hydrographic Surveys for Safe Navigation There are numerous reasons to conduct a hydrographic survey, but the most common Page 1: Hydrographic Surveying objective is for compiling nautical data along What is Hydrography? navigational channels, with an emphasis on the Hydrography is a branch of physical oceanography measurement and profiling of the subsurface or applied science which deals with the measuring physical features that may affect safe navigation and description of the configuration of the bottoms and travel by marine vessels. and adjacent land areas of oceans, lakes, rivers, harbors, and other water forms. What are Hydrographic Surveys? A hydrographic survey deals with measuring and description of features of a water area and the bed configuration; however, it may also encompass a wide variety of other objectives such as the measuring of tides, currents, gravity, Earth magnetism, and for determining the physical and chemical properties of water. The image above shows a dredging operation Bathymetric Surveying consisting of a clamshell bucket dredge on a barge The label of hydrographic surveying is often synonymously applied to bathymetric surveying. Documenting the Geomorphic Changes However, the Routine hydrographic surveys are essential to latter actually documenting the transportation of silt and Bathymetry refers to the sedimentation, in order to unsure safe lanes of The term "bathymetry," originally study and shipping in rivers and along coastlines. nautical in origin, referred to the ocean's depth relative to the sea measurement of level (free surface), although it the bottom or Natural currents and storm events such as has since come to refer to the “bed” of a hurricanes tends to shift the silt on the sea or river “submarine topography,” or the navigable water beds, potentially accumulating in previously depths and shapes of the body (whether it dredged channels, causing dangerous conditions or underwater earthen terrain. is an ocean, river, obstructions. lake or other body or channel of water.) In other Locating Submerged Obstacles words it deals with the topography of the solid In addition to the surveying of geomorphic earth, beneath a body of water. changes, hydrographic surveys may be utilized to locate submerged vessels and other hazardous Below are various types of hydrographic surveying debris along river and sea beds. methods. A hydrographic survey can be used to facilitate offshore oil and gas exploration, drilling operations, marine construction, dredging, installation of subsea cables and more. Other Applications Other applications for hydrographic surveying: to generate the data needed to create and update nautical charts to verify that navigational channels are This agency was established when then President, clear and accurate Thomas Jefferson and Congress authorized a port and harbor maintenance (dredging), survey to be taken of coasts of the newly formed expansion, and re-design “United States of America." coastal engineering and geomorphological First Head of the US Coast Survey evaluations The first person to officially head the US Coast beach erosion and replenishment studies Survey was Ferdinand Rudolph Hassler, who coastal zone management assembled a number of skilled professionals from offshore resources development various scientific communities, to survey and chart oil and gas exploration out the coastlines of the US. volumetric studies erosion and siltation studies pre- and post-dredge evaluations Types of Professionals at river crossing profiles and evaluations the USCS aquatic vegetation design mathematicians cartographers flood studies geodesists to locate and verify the integrity of meteorologists submerged cabling and piping hydrographers for determining fisheries habitat and topographers understanding marine geologic processes sailors and laborers administrators to determine seabed and riverbed materials (i.e. sand, mud, rock) preliminary bed analysis for anchoring, The first official US survey - 1834 construction of marine structures, and The first official hydrographic survey performed in pipeline and cable routing the US was conducted along the southern shore of Long Island in 1834. disaster response following storm events; looking for changes in depth or debris in The first official US nautical chart – 1839 navigational channels In 1839, the US government produced its first nautical chart. However, many privately commissioned charts of the Americas were known Page 3: History of Hydrographic Surveying to exist prior to this date. Origins The history of hydrographic and bathymetric surveying likely dates back to the origins of sailing. As long as people have sailed the oceans, there has been the need to chart pathways for safe travel to avoid vessel groundings, and to document regional and seasonal oceanic currents and meteorological patterns. US Coast Survey Establishment of the US Coast Survey – 1807 Navigational chart of the Potomac estuary In the US, the first officially sanctioned (created in 1838 by the Alex’a Canal Company) hydrographic surveying office began in 1807, with the establishment of the “US Coast Survey”, which is one of the oldest scientific agencies in the US. Page 4: Early Hydrographic Surveying and other bathymetric methodologies, they are still Methods – Sounding Poles and Lead Lines sold by some “Mark Twain” survey supply Prior to 1900s – Poles and Lines In modern literature, Samuel companies, and Shallow water surveys – In early hydrographic Clemens took his pen name from may be used in practice, shallow water surveys consisted of depth his early employment as a areas where leadsman on the Mississippi River. measurements conducted by use of sounding The leadsman was the person large amounts of poles. who used a sounding pole or lead vegetation or line to measure the river depths thick mud would Deep water surveys – Sounding Lines to ensure the boat was staying tend to distort In greater depths, a sounding line (or lead line) was away from the shallow banks. To the electronic "mark twain" referred to marking used to make measurements of river channel, returns of estuarial and oceanic navigational pathways. a depth of the water of two fathoms, or 12 feet. modern Positions were determined by three-point sextant equipment. fixes to mapped reference points. A more sophisticated means of measuring deep water at Lead Lines this time was through the use of sounding Lead line systems consisted of ropes or lines, with machines, which were simply reel or drum based depth markings and line devices. lead weights attached (see image). The lead Sounding poles weights were usually A sounding pole (see image below) is simply a long conical in shape, rod, (usually made of wood, or aluminum in weighing around 12- present day use), that is used to measure 14 lbs., and navigational channel depths. Though mainly used occasionally had a to measure water depth, they may be used to small amount of wax measure the depths of boreholes, snow piles, or or lard on the base to loose soil stockpiles as well. collect a small sample of the surface sedimentary deposits. This A typical length of a sounding pole is about 20 feet, rudimentary but effective system could reportedly marked in one inch increments. They might have a provide reliable soil samples to depths of 100 circular plate at one end to ensure that the location fathoms or 600 ft. being measured is somewhat level and normalized, The “Fathom” and to prevent inaccuracies due to the pole sinking The line was lowered too deep into the In the early days of until it hit bottom, hydrographic surveying, a muck or silt bottom. then read manually in fathom was used to The pole technician a tedious, painstaking measure water depth. A would drop the pole process. These initial fathom is a linear unit of until there is adequate measurement, equal to 6 depth soundings were feet. resistance at the soil
Recommended publications
  • REPORT on the CONDUCT of the 2021 WORLD HYDROGRAPHY DAY CELEBRATION in NIGERIA-1.Pdf
    Advancements and the Future Outlook of Charting the Nigerian Navigation Channel Chukwuemeka C. Onyebuchi1, Franklin E. Onyeagoro2 and Peter O. Aimah3 1Polaris Integrated and Geosolutions Limited, [email protected] 2Federal University of Technology Owerri, [email protected] 3Polaris Integrated and Geosolutions Limited, [email protected] ABSTRACT The need for achieving safe waterways for navigation, engineering, exploration, security and other marine operations cannot be overemphasized and should be attained using precise methods and equipment. The Hydrographic process still remains the only systematic means through which spatial information about our marine environment (oceans, seas, rivers etc.) are acquired for charting purposes so as to aid analysis and decision making. In Nigeria today, most marine operations and mostly the Nigerian Navy is dependent on the Hydrographic process for smooth operations required for security, trading, engineering etc. therefore maintaining the integrity of the hydrographic process is of uttermost importance. To maintain the integrity of the hydrographic process used for charting our navigational channels, the progressive evolution of this process shall be assessed: from the earliest methods that directly sounded navigational channels using weighted lead lines and graduated poles to provide water depths to Wire Drag methods used to identify physical features on the marine environment, then to the 1930s when acoustic waves were applied in the Echo Sounder to indirectly ascertain seabed profile, and the use of instruments like Multi Beam Echo Sounders, Magnetometer, Side Scan Sonar, etc. for detailed Bathymetric and Geophysical Survey Projects, and presently to the use of Remotely Operated Vehicles (ROV) and satellites in space to monitor sea level rise.
    [Show full text]
  • Chapter 5 Water Levels and Flow
    253 CHAPTER 5 WATER LEVELS AND FLOW 1. INTRODUCTION The purpose of this chapter is to provide the hydrographer and technical reader the fundamental information required to understand and apply water levels, derived water level products and datums, and water currents to carry out field operations in support of hydrographic surveying and mapping activities. The hydrographer is concerned not only with the elevation of the sea surface, which is affected significantly by tides, but also with the elevation of lake and river surfaces, where tidal phenomena may have little effect. The term ‘tide’ is traditionally accepted and widely used by hydrographers in connection with the instrumentation used to measure the elevation of the water surface, though the term ‘water level’ would be more technically correct. The term ‘current’ similarly is accepted in many areas in connection with tidal currents; however water currents are greatly affected by much more than the tide producing forces. The term ‘flow’ is often used instead of currents. Tidal forces play such a significant role in completing most hydrographic surveys that tide producing forces and fundamental tidal variations are only described in general with appropriate technical references in this chapter. It is important for the hydrographer to understand why tide, water level and water current characteristics vary both over time and spatially so that they are taken fully into account for survey planning and operations which will lead to successful production of accurate surveys and charts. Because procedures and approaches to measuring and applying water levels, tides and currents vary depending upon the country, this chapter covers general principles using documented examples as appropriate for illustration.
    [Show full text]
  • Depth Measuring Techniques
    EM 1110-2-1003 1 Jan 02 Chapter 9 Single Beam Acoustic Depth Measurement Techniques 9-1. General Scope and Applications Single beam acoustic depth sounding is by far the most widely used depth measurement technique in USACE for surveying river and harbor navigation projects. Acoustic depth sounding was first used in the Corps back in the 1930s but did not replace reliance on lead line depth measurement until the 1950s or 1960s. A variety of acoustic depth systems are used throughout the Corps, depending on project conditions and depths. These include single beam transducer systems, multiple transducer channel sweep systems, and multibeam sweep systems. Although multibeam systems are increasingly being used for surveys of deep-draft projects, single beam systems are still used by the vast majority of districts. This chapter covers the principles of acoustic depth measurement for traditional vertically mounted, single beam systems. Many of these principles are also applicable to multiple transducer sweep systems and multibeam systems. This chapter especially focuses on the critical calibrations required to maintain quality control in single beam echo sounding equipment. These criteria are summarized in Table 9-6 at the end of this chapter. 9-2. Principles of Acoustic Depth Measurement Reference water surface Transducer Outgoing signal VVeeloclocityty Transmitted and returned acoustic pulse Time Velocity X Time Draft d M e a s ure 2d depth is function of: Indexndex D • pulse travel time (t) • pulse velocity in water (v) D = 1/2 * v * t Reflected signal Figure 9-1. Acoustic depth measurement 9-1 EM 1110-2-1003 1 Jan 02 a.
    [Show full text]
  • Hydrographic Surveys Specifications and Deliverables
    HYDROGRAPHIC SURVEYS SPECIFICATIONS AND DELIVERABLES March 2019 U.S. Department of Commerce National Oceanic and Atmospheric Administration National Ocean Service Contents 1 Introduction ......................................................................................................................................1 1.1 Change Management ............................................................................................................................................. 2 1.2 Changes from April 2018 ...................................................................................................................................... 2 1.3 Definitions ............................................................................................................................................................... 4 1.3.1 Hydrographer ................................................................................................................................................. 4 1.3.2 Navigable Area Survey .................................................................................................................................. 4 1.4 Pre-Survey Assessment ......................................................................................................................................... 5 1.5 Environmental Compliance .................................................................................................................................. 5 1.6 Dangers to Navigation ..........................................................................................................................................
    [Show full text]
  • Landsat Continuing to Improve Everyday Life
    How Landsat Helps: BATHYMETRY Avoiding Rock Bottom: How Landsat Aids Nautical Charting | Laura E.P. Rocchio On the most recent nautical chart of territorial waters in the U.S. Exclusive hydrographic surveying capabilities (the Above: Chart inlay of the Dry Tortugas, a grouping of islands Economic Zone (EEZ), a combined area ability to measure and map water depths). Tortugas Harbor which that lies seventy miles west of Key West, of 3.4 million square nautical miles that The job is sizable and expensive. While the Florida, Landsat data provided the extends 200 nautical miles offshore from Army Corps of Engineers is responsible surrounds Garden Key where estimated water depths for areas too the nation’s coastline. The U.S. has the for maintaining the depth of shipping Fort Jefferson is located. shallow and difficult to be reached by the largest EEZ of all nations in the world channels, providing bathymetry everywhere The depth measurements around the key (within National Oceanographic and Atmospheric but, as of 2015, it ranked behind 18 other else in U.S. waters is NOAA’s duty. } Administration’s (NOAA) surveying ships. nations in the number of vessels with the thick purple line) were made using Landsat data. It was sometime between 1840 and 1939 that the sections of water surrounding In-page: The most recent the islands were last formally surveyed. NOAA nautical chart of Since that time, Dry Tortugas National Florida’s Dry Tortugas Park was established and the park—along (Chart 11438). The purple with its hundreds of shipwrecks, pristine polygons, including the area beaches, and clear water—has become around Garden Key where popular with recreational boat cruisers.
    [Show full text]
  • Measuring the Water Level Datum Relative to the Ellipsoid During Hydrographic Survey
    Measuring the Water Level Datum Relative to the Ellipsoid During Hydrographic Survey Glen Rice LTJG / NOAA Corps, Coast Survey Development Laboratory 24 Colovos Road, Durham NH 03824 [email protected] ; 603‐862‐1397 Jack Riley Physical Scientist, NOAA Hydrographic Systems and Technology Program 1315 East West Hwy, SSMC3, Silver Spring MD 20910‐3282 [email protected] ; 301‐713‐2653 x154 Abstract Hydrographic surveys are referenced vertically to a local water level “chart” datum. Conducting a survey relative to the ellipsoid dictates a datum transformation take place before the survey is used for current navigational products. Models that combine estimates for the tide, sea surface topography, the geoid, and the ellipsoid are often used to transform an ellipsoid referenced survey to a local water level datum. Regions covered by these vertical datum transformation models are limited and so would appear to constrain the areas where ellipsoid referenced surveys can be conducted. Because areas not covered by a vertical datum transformation model still must have a tide model to conduct a hydrographic survey, survey‐ time measurements of the ellipsoid to water level datum can be conducted through the vessel reference point. This measured separation is largely a function of the vessel ellipsoid height and the standard survey tide model and thus introduces limited additional uncertainty than is typical in a water level referenced survey. This approach is useful for reducing ellipsoid reference surveys to the water level datum, examining a tide model, or for evaluating a vertical datum transformation model. Prototype tools and a comparison to typical vertical datum transformation models are discussed.
    [Show full text]
  • 3 Hydrographic Positioning
    HYDROGRAPHIC SURVEYS SPECIFICATIONS AND DELIVERABLES April 2017 U.S. Department of Commerce National Oceanic and Atmospheric Administration National Ocean Service Contents 1 Introduction ......................................................................................................................................1 1.1 Change Management ............................................................................................................................................. 1 1.2 Changes from March 2016 .................................................................................................................................... 2 1.3 Definitions ............................................................................................................................................................... 6 1.3.1 Hydrographer ................................................................................................................................................. 6 1.3.2 Navigable Area Survey .................................................................................................................................. 6 1.4 Pre-Survey Assessment ......................................................................................................................................... 8 1.5 Environmental Compliance .................................................................................................................................. 8 1.6 Dangers to Navigation ..........................................................................................................................................
    [Show full text]
  • Manual on Hydrography
    INTERNATIONAL HYDROGRAPHIC ORGANIZATION MANUAL ON HYDROGRAPHY Publication C-13 1st Edition May 2005 (Corrections to February 2011) PUBLISHED BY THE INTERNATIONAL HYDROGRAPHIC BUREAU M O N A C O INTERNATIONAL HYDROGRAPHIC ORGANIZATION MANUAL ON HYDROGRAPHY Publication C-13 1st Edition May 2005 (Corrections to February 2011) Published by the International Hydrographic Bureau 4, Quai Antoine 1er B.P. 445 - MC 98011 MONACO Cedex Principauté de Monaco Telefax: (377) 93 10 81 40 E-mail: [email protected] Web: www.iho.int © Copyright International Hydrographic Organization [2010] This work is copyright. Apart from any use permitted in accordance with the Berne Convention for the Protection of Literary and Artistic Works (1886), and except in the circumstances described below, no part may be translated, reproduced by any process, adapted, communicated or commercially exploited without prior written permission from the International Hydrographic Bureau (IHB). Copyright in some of the material in this publication may be owned by another party and permission for the translation and/or reproduction of that material must be obtained from the owner. This document or partial material from this document may be translated, reproduced or distributed for general information, on no more than a cost recovery basis. Copies may not be sold or distributed for profit or gain without prior written agreement of the IHB and any other copyright holders. In the event that this document or partial material from this document is reproduced, translated or distributed under the terms described above, the following statements are to be included: “Material from IHO publication *reference to extract: Title, Edition] is reproduced with the permission of the International Hydrographic Bureau (IHB) (Permission No ……./…) acting for the International Hydrographic Organization (IHO), which does not accept responsibility for the correctness of the material as reproduced: in case of doubt, the IHO’s authentic text shall prevail.
    [Show full text]
  • Hydrographic Survey Using Real Time Kinematic Method for River Deepening
    CORE Metadata, citation and similar papers at core.ac.uk Provided by Universiti Teknologi Malaysia Institutional Repository Geoinformation Science Journal, Vol. 11, No. 1, 2011, pp: 1-14 HYDROGRAPHIC SURVEY USING REAL TIME KINEMATIC METHOD FOR RIVER DEEPENING Nor Aklima Bte Che Awang and En. Rusli Othman Department of Geomatic Engineering, Faculty of Geoinformation Science and Engineering, Universiti Teknologi Malaysia, 81310, Skudai, Johor, Malaysia. Email: [email protected],[email protected] ABSTRACT There is many surveys’s method in hydrographic surveying due to development of technologies. The latest development in technologies for example Global Positioning System (GPS) gives new challenges in surveying field. Surveyors use GPS technology for simple tasks or complex tasks. In hydrographic survey, the important data required are position, tidal reading and depth value. Normally, tidal reading is obtained at tidal station established near to survey area by using instrument like automatic or self-recording tide gauge. Depth of seabed is measured by using single beam or multi beam echo sounder without add up tidal value at the same time. The latest technique of getting position and depth simultaneously is by using RTK method. Key words: Real-Time Kinematic GPS, Hydrographic surveys. 1.0 INTRODUCTION Hydrographic is the science of marine surveying that determines the position of points and objects on the globe's surface and also depths of the sea. In the 1920s the technology of hydrographic changed when they found possible way to measure depths. There are many instruments have been designed to achieve better standard of surveying. With that advanced instruments, surveyor able to perform better and simple data acquisition of observation in surveying and at the same time achieve better accuracy in their observations.
    [Show full text]
  • Office of Coast Survey Contributions to a National Ocean Mapping Strategy
    Mapping U.S. Marine and Great Lakes Waters: Office of Coast Survey Contributions to a National Ocean Mapping Strategy July 2020 Office of Coast Survey National Oceanic and Atmospheric Administration MESSAGE FROM THE DIRECTOR I am pleased to release this Office of the Coast Survey plan for contributions to a National Ocean Mapping Strategy. This timely report articulates our ongoing commitment and approach to meeting our core surveying and nautical charting mission while supporting broader societal needs to fill fundamental gaps in seafloor mapping. This is an exciting and pivotal time to be leading the nation’s primary marine mapping program. National and international interest has never been higher. Leaders are increasingly recognizing the value – indeed the necessity – of understanding the basic contours of the seafloor and marine environment to support the Blue Economy and successfully balance marine resource conservation and uses. This is clearly reflected in the June 2020 National Strategy for Mapping, Exploring, and Characterizing the United States Exclusive Economic Zone (EEZ).1 One of the most important goals in this Strategy is to map the U.S. EEZ, “larger than the combined land area of all 50 states, … containing 3.4 million square nautical miles of ocean.” With 54 percent of U.S. waters essentially unmapped, we have a great opportunity to conduct regional mapping campaigns, using a mix of survey techniques and technologies above, on and in the water. It is also important to make the resulting data usable and available in standard formats wherever possible. Adding emphasis to global interest in mapping the oceans, the United Nations has proclaimed a Decade of Ocean Science for Sustainable Development (2021-2030), calling for an increase in ocean research to support the sustainable management of marine resources and the Blue Economy.
    [Show full text]
  • Hydrographic Survey Validation and Chart Adequacy Assessment Using Automated Solutions G
    US HYDRO 2019, MARCH 18-21 Hydrographic Survey Validation and Chart Adequacy Assessment Using Automated Solutions G. Masetti1,*, T. Faulkes2, C. Kastrisios1 1 Center for Coastal and Ocean Mapping / NOAA-UNH Joint Hydrographic Center - Durham, NH, USA 2 NOAA Office of Coast Survey, Pacific Hydrographic Branch - Seattle, WA, USA Within the HydrOffice framework, NOAA’s Office of Coast Survey and the UNH Center for Coastal and Ocean Mapping have jointly developed (and made publicly available) a pair of software solutions - QC Tools for quality control and CA Tools for chart adequacy - that collect algorithmic implementations to automate and standardize a large portion of the quality controls used to analyze hydrographic data. After having described what is Pydro Universe, the community surrounding these tools and the relevant feedback from a recent customer satisfaction survey, this work describes a new chart adequacy algorithm and an experimental approach for bathymetric anomaly detection and classification. Introduction The rising trend in automation is constantly pushing the hydrographic field toward the exploration and the adoption of more effective approaches for each step of the ping-to-public workflow [1-6]. However, the large amount of data collected by modern acquisition systems - especially when paired with the force multiplier factor provided by autonomous vessels - conflicts with the increasing timeliness expected by today’s final users [7-9]. As such, it is not that surprising that both an improved hydrographic data accuracy and a faster throughput from acquisition to publicly-available data (e.g., chart application) are current priorities for any hydrographic office (HO)(e.g., [10]). Such priorities represent a processing challenge for the largely human-centered solutions that are currently available, and the adoption of automated and semi-automated data quality procedures seems the only scalable and long-term solution to the problem [11-13].
    [Show full text]
  • Standards for Hydrographic Surveys (S-44)
    S-44 Edition 6.0.0 International Hydrographic Organization Standards for Hydrographic Surveys International Hydrographic Organization Standards for Hydrographic Surveys Published by the International Hydrographic Organization 4b quai Antoine 1er Principauté de Monaco Tel: (377) 93.10.81.00 Fax: (377) 93.10.81.40 [email protected] www.iho.int ii IHO Standards for Hydrographic Surveys © Copyright International Hydrographic Organization 2020 This work is copyright. Apart from any use permitted in accordance with the Berne Convention for the Protection of Literary and Artistic Works (1886), and except in the circumstances described below, no part may be translated, reproduced by any process, adapted, communicated or commercially exploited without prior written permission from the International Hydrographic Organization (IHO). Copyright in some of the material in this publication may be owned by another party and permission for the translation and/or reproduction of that material must be obtained from the owner. This document or partial material from this document may be translated, reproduced or distributed for general information, on no more than a cost recovery basis. Copies may not be sold or distributed for profit or gain without prior written agreement of the IHO and any other copyright holders. In the event that this document or partial material from this document is reproduced, translated or distributed under the terms described above, the following statements are to be included: “Material from IHO publication [reference to extract: Title, Edition] is reproduced with the permission of the Secretariat of the International Hydrographic Organization (IHO) (Permission No ……./……) acting for the International Hydrographic Organization (IHO), which does not accept responsibility for the correctness of the material as reproduced: in case of doubt, the IHO’s authentic text shall prevail.
    [Show full text]