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Submarine topography
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Most popular at the top

  • Seabed Fluid Flowby Alan Judd; Martin Hovland

    Cambridge University Press 2007; US$ 84.00

    Describes seabed fluid flow processes for research scientists and professionals in the marine environment. more...

  • Sound Images of the Oceanby Peter Wille

    Springer-Verlag Berlin and Heidelberg GmbH & Co. KG 2005; US$ 209.00

    Offers a comprehensive overview of acoustic imaging applications in the various fields of marine research, utilization, surveillance, and protection. This book employs 400 sound images of the sea floor and of processes in the sea volume, contributed by more than 120 marine experts from 22 nations. more...

  • Seamountsby Tony J. Pitcher; Telmo Morato; Paul J. B. Hart; Malcolm R. Clark; Nigel Haggan; Ricardo S. Santos

    John Wiley & Sons, Ltd. 2008; US$ 84.95

    Seamounts are ubiquitous undersea mountains rising from the ocean seafloor that do not reach the surface. There are likely many hundreds of thousands of seamounts, they are usually formed from volcanoes in the deep sea and are defined by oceanographers as independent features that rise to at least 0.5 km above the seafloor, although smaller features may have the same origin. This book follows a logical progression from geological and physical processes, ecology, biology and biogeography, to exploitation, management and conservation concerns. In 21 Chapters written by 57 of the world's leading seamount experts, the book reviews all aspects of their geology, ecology, biology, exploitation, conservation and management. In Section I of this book,... more...

  • Ocean Ridges and Trenchesby Peter Aleshire

    Infobase Publishing 2007; US$ 35.00

    Reveals how 10 undersea mountain ranges and valleys came to be, how and why it has changed over the span of geologic time, and its contributions to the environment. more...

  • Coastal Oceanography of Washington and Oregonby M.R. Landry; B.M. Hickey

    Elsevier 1989; US$ 287.00

    The Washington-Oregon coastal zone is a classical Eastern Boundary Current region. The area is extremely productive, the productivity dependent on near-shore infusions of nutrients into surface layers during wind-driven coastal upwelling. The Washington-Oregon coastline is much more regular than areas off California or off the East Coast, where large capes lend complexity to both the physical environment and the ecosystem response. The relatively straight coastline and broad, deep shelf greatly simplify the physical environment, so that processes responsible for much of the variance are more easily identified. The system response from mid-Oregon northward, although not strictly two-dimensional, is more so than many other coastal areas.... more...

  • Physical and Chemical Oceanography, and Physical Resourcesby F.T. Banner; M.B. Collins; K.S. Massie

    Elsevier 1980; US$ 287.00

    Physical and Chemical Oceanography, and Physical Resources more...

  • Carbon and Nutrient Fluxes in Continental Marginsby Kon-Kee Liu; Larry Atkinson; Renato Quinones; Liana Talaue-McManus

    Springer 2009; US$ 169.00

    Offers some of the best estimates of carbon and nutrient fluxes in seven types of continental margins. This book provides global syntheses on sediments and nutrients discharged to the ocean from land. It is suitable for researchers on continental margin environmental issues. more...

  • Abyssal Channels in the Atlantic Oceanby Eugene G. Morozov; Alexander N. Demidov; Roman Y. Tarakanov; Walter Zenk

    Springer 2010; US$ 129.00

    This book is dedicated to the study of structure and transport of deep and bottom waters through underwater channels of the Atlantic Ocean. The study is based on recent observations, analysis of historical data, and literature review. A strong flow of Antarctic Bottom Water from the Argentine Basin to the Brazil Basin through the Vema Channel (32iCdegree-27iCdegree S) is studied on the basis of CTD sections combined with LADCP profiling carried out annually and long-term moored measurements. The flow in the Vema Channel is mixed in the vertical direction but horizontally stratified. The mean speed of the flow is 30 cm/s and water transport is approximately 3.5 Sv. Owing to the bottom Ekman friction the dense core of the flow is usually displaced... more...

  • Where River Meets Seaby Lynne Turner; Dieter Tracey; Jan Tilden; William Dennison

    CSIRO Publishing 2006; US$ 34.95

    Details the health, geography, science, management and ecological functions of these unique coastal waterways. more...

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