Manual on Hydrography
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School of Ocean and Earth Science and Technology
School of Ocean and Earth Science and Technology Administration established in SOEST under the U.S.- Japan Common Pacific Ocean Science and Technology 802 Agenda. The center is jointly supported by the state, Japanese, 1680 East-West Road and federal funds. Honolulu, HI 96822 Although the Department of Ocean and Resources Engi- Tel: (808) 956-6182 neering offers several undergraduate courses, baccalaureate Fax: (808) 956-9152 degrees are not offered in this area. The Department of Web: www.soest.hawaii.edu/ Oceanography offers the BS in global environmental science. Baccalaureate degree programs are offered in the Department of Dean: C. Barry Raleigh Geology and Geophysics and the Department of Meteorology. E-mail: [email protected] Those with long-range plans for graduate work in oceanogra- phy or ocean and resources engineering should prepare Interim Associate Dean: Patricia A. Cooper themselves with an undergraduate course of study that will E-mail: [email protected] satisfy the entry requirements for admission to these graduate programs. Information on entrance and degree or certificate requirements for all SOEST graduate programs (MS and PhD General Information in geology and geophysics, meteorology, ocean and resources The School of Ocean and Earth Science and Technology engineering, and oceanography, and a certificate in Graduate (SOEST) was established in 1988. It combines and integrates Ocean policy) is in this Catalog. Candidates for advanced the Departments of Geology and Geophysics, Meteorology, degrees and the graduate certificate program apply through the Ocean and Resources Engineering, and Oceanography, as well Graduate Division of the University. The school has developed as the Hawai‘i Institute of Geophysics and Planetology, the a number of interdisciplinary courses at both the undergradu- Hawai‘i Institute of Marine Biology, and the Hawai‘i Natural ate and the graduate levels, which are listed under OEST Energy Institute. -
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. -
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. -
GIS Best Practices GIS for Nautical Organizations
GIS Best Practices GIS for Nautical Organizations September 2010 Table of Contents What Is GIS? 1 GIS for Nautical Organizations 3 NOAA Modernizes Nautical Chart Production 5 Shifting Shorelines 11 A Geospatial Foundation 19 Making Standards Shipshape—Esri's Rafael Ponce Discusses Working with International Hydrographic Organizations 27 Remote Communities Prevail with GIS 33 Enterprise Product on Demand Services 43 Keeping Nature and Man in Balance 47 RAN Directorate of Oceanography and Meteorology 53 Taking NEXRAD Weather Radar to the Next Level in GIS 57 Maritime and Coastguard Agency Case Study toward a More Effi cient Tendering Process 65 NATO Maritime Component Command HQ Northwood, UK, Supporting Maritime Situational Awareness 71 i What Is GIS? Making decisions based on geography is basic to human thinking. Where shall we go, what will it be like, and what shall we do when we get there are applied to the simple event of going to the store or to the major event of launching a bathysphere into the ocean's depths. By understanding geography and people's relationship to location, we can make informed decisions about the way we live on our planet. A geographic information system (GIS) is a technological tool for comprehending geography and making intelligent decisions. GIS organizes geographic data so that a person reading a map can select data necessary for a specifi c project or task. A thematic map has a table of contents that allows the reader to add layers of information to a basemap of real-world locations. For example, a social analyst might use the basemap of Eugene, Oregon, and select datasets from the U.S. -
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. -
National Hydrography Data Content Standard for Coastal and Inland Waterways Public Review Draft, January 2000
FGDC Data Committee FGDC Document Number National Hydrography Data Content Standard for Coastal and Inland Waterways Public Review Draft, January 2000 NSDI National Spatial Data Infrastructure National Hydrography Data Content Standard for Coastal and Inland Waterways – Public Review Draft Bathymetric Subcommittee Federal Geographic Data Committee January 2000 Federal Geographic Data Committee i FGDC Data Committee FGDC Document Number National Hydrography Data Content Standard for Coastal and Inland Waterways Public Review Draft, January 2000 Established by Office of Management and Budget Circular A-16, the Federal Geographic Data Committee (FGDC) promotes the coordinated development, use, sharing, and dissemination of geographic data. The FGDC is composed of representatives from the Departments of Agriculture, Commerce, Defense, Energy, Housing and Urban Development, the Interior, State, and Transportation; the Environmental Protection Agency; the Federal Emergency Management Agency; the Library of Congress; the National Aeronautics and Space Administration; the National Archives and Records Administration; and the Tennessee Valley Authority. Additional Federal agencies participate on FGDC subcommittees and working groups. The Department of the Interior chairs the committee. FGDC subcommittees work on issues related to data categories coordinated under the circular. Subcommittees establish and implement standards for data content, quality, and transfer; encourage the exchange of information and the transfer of data; and organize the -
Modeling Groundwater Rise Caused by Sea-Level Rise in Coastal New Hampshire Jayne F
Journal of Coastal Research 35 1 143–157 Coconut Creek, Florida January 2019 Modeling Groundwater Rise Caused by Sea-Level Rise in Coastal New Hampshire Jayne F. Knott†*, Jennifer M. Jacobs†, Jo S. Daniel†, and Paul Kirshen‡ †Department of Civil and Environmental Engineering ‡School for the Environment University of New Hampshire University of Massachusetts Boston Durham, NH 03824, U.S.A. Boston, MA 02125, U.S.A. ABSTRACT Knott, J.F.; Jacobs, J.M.; Daniel, J.S., and Kirshen, P., 2019. Modeling groundwater rise caused by sea-level rise in coastal New Hampshire. Journal of Coastal Research, 35(1), 143–157. Coconut Creek (Florida), ISSN 0749-0208. Coastal communities with low topography are vulnerable from sea-level rise (SLR) caused by climate change and glacial isostasy. Coastal groundwater will rise with sea level, affecting water quality, the structural integrity of infrastructure, and natural ecosystem health. SLR-induced groundwater rise has been studied in coastal areas of high aquifer transmissivity. In this regional study, SLR-induced groundwater rise is investigated in a coastal area characterized by shallow unconsolidated deposits overlying fractured bedrock, typical of the glaciated NE. A numerical groundwater-flow model is used with groundwater observations and withdrawals, LIDAR topography, and surface-water hydrology to investigate SLR-induced changes in groundwater levels in New Hampshire’s coastal region. The SLR groundwater signal is detected more than three times farther inland than projected tidal flooding from SLR. The projected mean groundwater rise relative to SLR is 66% between 0 and 1 km, 34% between 1 and 2 km, 18% between 2 and 3 km, 7% between 3 and 4 km, and 3% between 4 and 5 km of the coastline, with large variability around the mean. -
The Sea Floor an Introduction to Marine Geology 4Th Edition Ebook
THE SEA FLOOR AN INTRODUCTION TO MARINE GEOLOGY 4TH EDITION PDF, EPUB, EBOOK Eugen Seibold | 9783319514116 | | | | | The Sea Floor An Introduction to Marine Geology 4th edition PDF Book Darwin drew his inspiration from observations on island life made during the voyage of the Beagle , and his work gave strong impetus to the first global oceanographic expedition, the voyage of HMS Challenger Resources from the Ocean Floor. This textbook deals with the most important items in Marine Geology, including some pioneer work. Outline of geology Glossary of geology History of geology Index of geology articles. About this Textbook This textbook deals with the most important items in Marine Geology, including some pioneer work. This should come as no surprise. Geologist Petroleum geologist Volcanologist. Geology Earth sciences Geology. They also are the deepest parts of the ocean floor. Stratigraphy Paleontology Paleoclimatology Palaeogeography. Origin and Morphology of Ocean Basins. Back Matter Pages It seems that you're in Germany. Add to Wishlist. Marine geology has strong ties to geophysics and to physical oceanography. Some of these notions were put forward earlier in this century by A. Springer Berlin Heidelberg. They should allow the reader to comment on new results about plate tectonics, marine sedimentation from the coasts to the deep sea, climatological aspects, paleoceanology and the use of the sea floor. Uh-oh, it looks like your Internet Explorer is out of date. Back Matter Pages Coastal Ecology marine geology textbook plate tectonics Oceanography Environmental Sciences sea level. Seibold and W. The deep ocean floor is the last essentially unexplored frontier and detailed mapping in support of both military submarine objectives and economic petroleum and metal mining objectives drives the research. -
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 .......................................................................................................................................... -
Marine Geosciences 1
Marine Geosciences 1 MARINE GEOSCIENCES https://www.graduate.rsmas.miami.edu/graduate-programs/marine-geosciences/index.html Dept. Code: MGS The Marine Geosciences (MGS) graduate program is focused on studying the geology, geophysics, and geochemistry of the Earth system. Students work closely with faculty at the forefront of research on sedimentary systems, earthquakes, volcanoes, plate tectonics, and past and present climate. MGS faculty and students also emphasize interdisciplinary study where geological phenomena interact with, or are influenced by, processes generally studied in other disciplines, such as ocean currents, climate, biological evolution, and even social sciences. MGS research uses pioneering remote sensing techniques to assess the Earth’s crustal movement and sedimentation in coastal zones and beyond. MGS degree programs are at the forefront of understanding carbonate depositional systems, modern and ancient reefs, and deep-sea sediments to learn more about past environmental change. Degree Programs • Post-Bachelor's Certificate (p. 1) • Offered for working professionals who seek specialization in Applied Carbonate Geology. • Requires 16 course credit hours for successful completion. • Master of Science (M.S.) • Requires 30 credit hours, including 24 course credit hours and 6 research credit hours. • Interdisciplinary studies with expertise in physics, chemistry, mathematics, and/or biology are encouraged. • Doctor of Philosophy (Ph.D.) (p. 1) • Requires 60 credit hours, including a minimum of 30 course credit hours and a minimum of 12 research credit hours. • Interdisciplinary studies with expertise in physics, chemistry, mathematics, and/or biology are encouraged. Post-Bachelor's Certificate Program The goal of the certificate program is to provide first-rate continuing education to professionals or Earth science students who aspire to become experts in carbonate geology. -
Hydrographic Surveying Resources at ODOT
Hydrographic Surveying Resources @ ODOT David Moehl, PLS, CH Project Surveyor, ODOT Geometronics What is hydrography? • Hydrography is the measurement of physical features of a water body. • Bathymetry is the foundation of the science of hydrography. • Hydrography includes not only bathymetry, but also the shape and features of the shoreline; the characteristics of tides, currents, and waves; and the physical and chemical properties of the water itself. What is bathymetry? • The name is derived from Greek: • Bathus = Deep • and Meton = Measure • Dictionary: “The measurement of the depths of oceans, seas, or other large bodies of water, also: the data derived from such measurement.” • Wikipedia: “is the underwater equivalent to topography.” • NOAA: “The study of the ‘beds’ or ‘floors’ of water bodies, including the ocean, rivers, streams, and lakes and currently means ‘submarine topography’.” Source: https://www.ngdc.noaa.gov The lost city of Atlantis? Source: Google Earth How do we measure water depths? • Manual How do we measure water depths? • Manual How do we measure water depths? • Manual How do we measure water depths? • Manual • Sound • Echosounders • Determines the depth by measuring the two way travel time of sound through the water • Different types of echosounders Singlebeam echosounders • This is the tool that ODOT utilizes • Benefits of this system: • Most affordable and widely used • Less ongoing training, software and maintenance costs • Useful for: • Cross section data acquisition for hydraulic modeling • Uniform topography -
AGY 514 – Marine Geology COURSE PARTICULARS COURSE
AGY 514 – Marine Geology COURSE PARTICULARS Course Code: AGY 514 Course Title: Marine Geology No. of Units: 3 Course Duration: Two hours of theory and three hours of practical per week for 15 weeks. Status: Compulsory Course Email Address: Course Webpage: Prerequisite: AGY 301, AGY 304 COURSE INSTRUCTORS Dr. S. O. Olabode SEMS Building, Dept. of Applied Geology, The Federal University of Technology, Akure, Nigeria. Phone: +2348033783498 Email: [email protected] COURSE DESCRIPTION This course is an applied, final year course designed primarily for students in applied geology and other relevant disciplines. However, it also meets the need of students in other fields, as a course that provides introduction to world oceans, basic understanding in the physical, chemical and biological aspects of these oceans and various geological processes that is going on in the oceans. As a course that integrates theory and practical, the purpose is to expose the students to a better understanding of the world oceans and impart useful skills on the mineral resources of the ocean, how these minerals could be accessed and management of coastal environment. Topics to be covered include world ocean and physical, chemical and biological oceanography; physiography of world oceans; plate tectonics as it relates to oceans; ophiolite complexes; coastal processes, deep sea sediments; mineralisation in the oceans and methods of ocean floor sampling. COURSE OBJECTIVES 1 The objectives of this course are to: introduce students to the basic and applied knowledge of the world oceans; intimate the students with basic mineral resources of the world oceans and how these minerals can be exploited; and management of coastal environments in terms of pollution and natural hazards.