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Titlebook: Coastal Upwelling Its Sediment Record; Part A: Responses of Erwin Suess,Jörn Thiede Book 1983 Springer Science+Business Media New York 1983

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书目名称Coastal Upwelling Its Sediment Record
副标题Part A: Responses of
编辑Erwin Suess,Jörn Thiede
视频video
丛书名称Nato Conference Series
图书封面Titlebook: Coastal Upwelling Its Sediment Record; Part A: Responses of Erwin Suess,Jörn Thiede Book 1983 Springer Science+Business Media New York 1983
描述NATO Advanced Research Institutes are designed to explore unre­ solved problems. By focusing complementary expertise from various disciplines onto one unifying theme, they approach old problems in new ways. In line with this goal of the NATO Science Committee, and with substantial support from the u.s. Office of Naval Research and the Seabed Assessment Program of the U. S. National Science Founda­ tion, such a Research Institute on the theme of Coastal Upwelling and Its Sediment Record was held september 1-4, 1981, in Vilamoura, Portugal. The theme implies a modification of uniformitarian thinking in earth science. Expectations were directed not so much towards find­ ing the key to the past as towards exploring the limits of interpret­ ing the past based on present upwelling oceanography. Coastal up­ welling and its imprint on sediments are particularly well-suited for such a scientific inquiry. The oceanic processes and conditions characteristic of upwelling are well understood and are a well­ packaged representation of ocean science that are familiar to geolo­ gists, just as the magnitude of bioproduction and sedimentation in upwelling regimes --among other biological and geologi
出版日期Book 1983
关键词Coast; Sediment; Sedimentation; geoscience; ocean; oceanography; production; research
版次1
doihttps://doi.org/10.1007/978-1-4615-6651-9
isbn_softcover978-1-4615-6653-3
isbn_ebook978-1-4615-6651-9
copyrightSpringer Science+Business Media New York 1983
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Searching for Welfare North and South, the Peruvian coastal upwelling ecosystem. Longterm fluctuations in anchoveta stock could, therefore, affect the quantity and composition of particulate matter input to the benthos and thereby to the sediment record.
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https://doi.org/10.1007/978-3-030-23061-6rient-rich subsurface waters. Its consequences have profound biological effects with strong economic implications for regional fisheries (Smith, 1968; Ryther, 1969; Parsons, 1979; Hartline, 1981; Walsh, 1981). Coastal upwelling produces characteristic perturbations of the boundary current regimes al
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Mono-jet Prospects at an Upgraded LHC,shelves. Preliminary observations from a study near Point Conception, California, as well as previous observations from Peru, near 15°S, provide us with some generalizations about coastal upwelling centers. The mean structures of these centers appear to be well-defined regions of low temperature, hi
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Detection Algorithms: FFT vs. KLTthermal signature. During the summer, upwelled waters occupy the surface layers over the whole western shelf and part of the upper slope of Portugal, and their areal extent pulsates onshore-offshore in response to cycles of northerly winds, reaching 30–50 km from the coast under calm conditions and
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ATA: A Cyclops for the 21st Centurybon stable isotopic composition of foraminiferal shells. For a better understanding of these isotopic signals, we systematically analyzed planktonic and benthic species from surface sediment samples and plankton tows from the eastern Atlantic continental margin (12–35°N). Due to seasonal variations
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