OCEANOGRAPHY JOINS HYDROGRAPHY by Desmond P
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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. -
The Life and Letters of a Royal Navy Surgeon, Edward Lawton Moss MD
REVIEWS • 109 why they are the crème de la crème. Chapters 7a and 7b pic- plateau of Washington Irving Island off the entrance to ture and describe some of these items. Chapter 7c, entitled Dobbin Bay on the east coast of Ellesmere Island. Much to “Gems Showcase,” is a visual feast. No fewer than 43 pages their surprise, they discovered two ancient-looking stone are devoted to images, almost all in colour, of polar material cairns on the plateau, but failed to locate any evidence of such as notices of various kinds, postcards, covers, and let- who might have built them. Moss made a quick sketch of ters. This section alone is worth the price of the book. the two cairns, a sketch he later back in England turned into The ultimate goal of many philatelists is to exhibit their a colour painting, now kept at the Scott Polar Institute in collections and, they hope, to earn a commensurate award. Cambridge. The drawing and the mention of the cairns in Chapter eight outlines the differences between showing one’s the expedition diaries resulted in our own investigation of collection and exhibiting it. Although many of the processes the plateau in July 1979. By then, numerous finds of Norse involved in showing a polar exhibit are the same as those artifacts in nearby 12th century Inuit house ruins strongly of exhibiting a general postal history collection, the author suggested that the builders of the old cairns could have been explains the differences in some detail. If an exhibit is to Norse explorers from Greenland (McCullough and Schled- do well in competition, planning, deciding what to include, ermann, 1999). -
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. -
Salty Dogs and 'Philosophers': a Saga of Seafaring Scientists and Sailors Helen Rozwadowski [email protected]
University of Connecticut OpenCommons@UConn Wrack Lines University of Connecticut Sea Grant July 2003 Salty Dogs and 'Philosophers': a Saga of Seafaring Scientists and Sailors Helen Rozwadowski [email protected] Follow this and additional works at: https://opencommons.uconn.edu/wracklines Recommended Citation Rozwadowski, Helen, "Salty Dogs and 'Philosophers': a Saga of Seafaring Scientists and Sailors" (2003). Wrack Lines. 6. https://opencommons.uconn.edu/wracklines/6 Salty Dogs and 'Philosophers' a Saga of Seafaring Scientists and Sailors Helen M. Rozwadowski ne definition of an oceanogra- fields–physics, chemistry, biology, and More than land-based institutions, pher, at least until recently, is a geology–on the project of understand- ships function tightly as units. Oscientist who goes to sea. Now, ing the oceans. Its practitioners did not Scientists traveling on ships, especially satellite data collection and remote sens- share a common set of intellectual ques- those whose primary mission was not ing may be permanently changing the tions, nor do they today. Instead, they science, fit only uneasily into the ship’s ocean-going culture of marine sciences. shared the experiences of boarding ves- bounded universe. They had to seek the Oceanography as it emerged in the last sels, meeting sailors, and wrestling with cooperation of captains, officers, and q u a rter of the nineteenth century the maritime gear used to retrieve data common sailors who had priorities and focused the attention of many scientific or specimens from the restless sea. interests quite distinct from their own. Producing scientific knowledge about the ocean during the nineteenth cen- tury required scientists to integrate their work with existing maritime practices, traditions, and technologies. -
ARCTIC Exploration the SEARCH for FRANKLIN
CATALOGUE THREE HUNDRED TWENTY-EIGHT ARCTIC EXPLORATION & THE SeaRCH FOR FRANKLIN WILLIAM REESE COMPANY 409 Temple Street New Haven, CT 06511 (203) 789-8081 A Note This catalogue is devoted to Arctic exploration, the search for the Northwest Passage, and the later search for Sir John Franklin. It features many volumes from a distinguished private collection recently purchased by us, and only a few of the items here have appeared in previous catalogues. Notable works are the famous Drage account of 1749, many of the works of naturalist/explorer Sir John Richardson, many of the accounts of Franklin search expeditions from the 1850s, a lovely set of Parry’s voyages, a large number of the Admiralty “Blue Books” related to the search for Franklin, and many other classic narratives. This is one of 75 copies of this catalogue specially printed in color. Available on request or via our website are our recent catalogues: 320 Manuscripts & Archives, 322 Forty Years a Bookseller, 323 For Readers of All Ages: Recent Acquisitions in Americana, 324 American Military History, 326 Travellers & the American Scene, and 327 World Travel & Voyages; Bulletins 36 American Views & Cartography, 37 Flat: Single Sig- nificant Sheets, 38 Images of the American West, and 39 Manuscripts; e-lists (only available on our website) The Annex Flat Files: An Illustrated Americana Miscellany, Here a Map, There a Map, Everywhere a Map..., and Original Works of Art, and many more topical lists. Some of our catalogues, as well as some recent topical lists, are now posted on the internet at www.reeseco.com. -
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 .......................................................................................................................................... -
On the Navigation of Smith Sound, As a Route to the Polar Sea Author(S): G
On the Navigation of Smith Sound, as a Route to the Polar Sea Author(s): G. S. Nares Source: Proceedings of the Royal Geographical Society of London, Vol. 21, No. 4 (1876 - 1877), pp. 274-287 Published by: Wiley on behalf of The Royal Geographical Society (with the Institute of British Geographers) Stable URL: http://www.jstor.org/stable/1799958 . Accessed: 12/06/2014 17:35 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Wiley and The Royal Geographical Society (with the Institute of British Geographers) are collaborating with JSTOR to digitize, preserve and extend access to Proceedings of the Royal Geographical Society of London. http://www.jstor.org This content downloaded from 185.44.78.31 on Thu, 12 Jun 2014 17:35:09 PM All use subject to JSTOR Terms and Conditions 274 THE NAVIGATIONOF S}IITH SOUND [AI.KR.2G, 1877-. coast in any quarterof the worldwhere he llad not done lTaluablework, and provedhis scientificaccura,cy, and the laboriousmode ill which he carriedout his sllrveys. Such men werenot easily replaced. There were but few in a generation,and when one of them passed away, those who lrnew what they had done were bound to pay them the tribute of affectionateregret. -
Memoirs of Hydrography
MEMOIRS 07 HYDROGRAPHY INCLUDING Brief Biographies of the Principal Officers who have Served in H.M. NAVAL SURVEYING SERVICE BETWEEN THE YEARS 1750 and 1885 COMPILED BY COMMANDER L. S. DAWSON, R.N. I 1s t tw o PARTS. P a r t II.—1830 t o 1885. EASTBOURNE: HENRY W. KEAY, THE “ IMPERIAL LIBRARY.” iI i / PREF A CE. N the compilation of Part II. of the Memoirs of Hydrography, the endeavour has been to give the services of the many excellent surveying I officers of the late Indian Navy, equal prominence with those of the Royal Navy. Except in the geographical abridgment, under the heading of “ Progress of Martne Surveys” attached to the Memoirs of the various Hydrographers, the personal services of officers still on the Active List, and employed in the surveying service of the Royal Navy, have not been alluded to ; thereby the lines of official etiquette will not have been over-stepped. L. S. D. January , 1885. CONTENTS OF PART II ♦ CHAPTER I. Beaufort, Progress 1829 to 1854, Fitzroy, Belcher, Graves, Raper, Blackwood, Barrai, Arlett, Frazer, Owen Stanley, J. L. Stokes, Sulivan, Berard, Collinson, Lloyd, Otter, Kellett, La Place, Schubert, Haines,' Nolloth, Brock, Spratt, C. G. Robinson, Sheringham, Williams, Becher, Bate, Church, Powell, E. J. Bedford, Elwon, Ethersey, Carless, G. A. Bedford, James Wood, Wolfe, Balleny, Wilkes, W. Allen, Maury, Miles, Mooney, R. B. Beechey, P. Shortland, Yule, Lord, Burdwood, Dayman, Drury, Barrow, Christopher, John Wood, Harding, Kortright, Johnson, Du Petit Thouars, Lawrance, Klint, W. Smyth, Dunsterville, Cox, F. W. L. Thomas, Biddlecombe, Gordon, Bird Allen, Curtis, Edye, F. -
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 -
On the Achievements of Scotsmen During the Nineteenth Century in the Fields of Geographical Exploration and Research
Scottish Geographical Magazine ISSN: 0036-9225 (Print) (Online) Journal homepage: http://www.tandfonline.com/loi/rsgj19 On the achievements of Scotsmen during the nineteenth century in the fields of geographical exploration and research Arthur Silva White F.R.S.E. To cite this article: Arthur Silva White F.R.S.E. (1889) On the achievements of Scotsmen during the nineteenth century in the fields of geographical exploration and research, Scottish Geographical Magazine, 5:10, 540-549, DOI: 10.1080/00369228908732403 To link to this article: http://dx.doi.org/10.1080/00369228908732403 Published online: 27 Feb 2008. Submit your article to this journal Article views: 8 View related articles Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=rsgj20 Download by: [137.189.171.235] Date: 10 June 2016, At: 16:53 540 ACHIEVEMENTS OF SCOTSMEN DURING THE NINETEENTH CENTURY fitted out with the necessary sounding apparatus, thermometers, areo- meters, zoological capturing gear, etc., not to mention accurate compasses and logging machines for the exact determination of the direction and rate of the currents. For the physical, chemical, and biological researches on shore, as well as for the working up of the observations collected at sea and on shore, there is required a special board or commission, with a laboratory and scientifically trained workers. To a country like Norway, with its extended and rich home fisheries, such an institution would be an immense benefit. It would cost much money, of course, but there is no short cut conducting to the goal. -
Geography, Hydrography and Climate 5
chapter 2 Geography, hydrography and climate 5 GEOGRAPHY 2.1 Introduction This chapter defines the principal geographical characteristics of the Greater North Sea. Its aim is to set the scene for the more detailed descriptions of the physical, chemical, and biological characteristics of the area and the impact man’s activities have had, and are having, upon them. For various reasons, certain areas (here called ‘focus areas’) have been given special attention. 6 Region II Greater North Sea 2.2 Definition of the region 2.3 Bottom topography The Greater North Sea, as defined in chapter one, is The bottom topography is important in relation to its effect situated on the continental shelf of north-west Europe. It on water circulation and vertical mixing. Flows tend to be opens into the Atlantic Ocean to the north and, via the concentrated in areas where slopes are steepest, with the Channel to the south-west, and into the Baltic Sea to the current flowing along the contours. The depth of the North east, and is divided into a number of loosely defined Sea (Figure 2.1) increases towards the Atlantic Ocean to areas. The open North Sea is often divided into the about 200 m at the edge of the continental shelf. The relatively shallow southern North Sea (including e.g. the Norwegian Trench, which has a sill depth (saddle point) of Southern Bight and the German Bight), the central North 270 m off the west coast of Norway and a maximum depth Sea, the northern North Sea, the Norwegian Trench and of 700 m in the Skagerrak, plays a major role in steering the Skagerrak.