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- Springer Netherlands 2010; US$ 159.00
This book is dedicated to the study of the structure, as well as the transport, of deep and bottom waters through underwater channels in the Atlantic Ocean. The study is based on recent observations, analysis of historical data, and a literature review. more...
- Springer Berlin Heidelberg 2010; US$ 269.00
This exhaustive new edition offers the fundamentals of sidescan sonar imagery and bathymetry and explains the tricky science of interpreting them. It also covers all recent advances in the field regarding both technology and knowledge of marine structures. more...
- Elsevier Science 2013; US$ 93.95
On the Nature of Continental Shelves discusses continental margins using techniques of systems analysis applied on minicomputers. The book describes insights and theories of mechanisms of enhanced primary production at the continental shelves, emphasizing these as the source energy, food, and recreation, and a possible means to detect global change... more...
- Elsevier Science 1989; US$ 72.95
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... more...
- Elsevier Science 2011; US$ 320.00
Physical and Chemical Oceanography, and Physical Resources more...
- Springer Berlin Heidelberg 2010; US$ 279.00
Providing the best estimates of carbon and nutrient fluxes in seven types of continental margins, this book also contains a global synthesis for carbon and nutrient fluxes between continental margins, the atmosphere and ocean; and between land and ocean. more...
- Wiley 2008; US$ 95.95
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... more...