Abstract:
This
is the initial volume in a comparatively wide-ranging review of
present knowledge of the circulation processes in the Gulf of Mexico.
Volume I is focused on the large-scale low-frequency deep-water current
structures in the Gulf, and on identifying in a preliminary way
interactions of these circulation patterns (typically referred to as the
general circulation) with the flow regimes on continental shelves
(typically referred to as coastal circulations). Volume II is primarily
concerned with coastal circulations, including their remote forcing and
considering shelf-estuarine interactions. This review will attempt to
expose and synthesize the physical oceanographic idea and publication
base for the Gulf, as an aid in becoming familiar with what has been
done, and not, what is known, and not known. The audience envisioned
would include scientists and engineers and students who are specialists
in other fields, perhaps especially marine scientists in other
disciplines, as well as members of the general public with a technical
inclination, and could be used as a supplemental text. The results
discussed and synthesized and critiqued could also be of interest to
professional physical oceanographers.
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the whole abstract >
This
book in PDF format:
Cover
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Table
of Contents (pdf 43.0 KB)
Abstract
(pdf 48.0 KB)
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Sea Surface
Temperature Map for the Gulf of Mexico on 5 March 1998.
Temperatures (°C) are color-coded as indicated
by the bar scale to the right. Names for various elements of the Loop
Current and its Eddy Field, the major components of the general
circulation of the Gulf of Mexico, are superimposed on a classical
"necking-down" configuration, involving a large warm-core Loop
Current Ring that will eventually detach and drift into the western Gulf
(OLDER EDDY on the map). The smaller scale features that are also
illustrated (frontal eddies and cyclones) play a role in the separation
process. Some clouds (fuzzy patches with bits of white) have not been
filtered out of this image (a 3-day average nominal). |