On the world ocean circulation. Volume I, some global features/North Atlantic circulation
Citable URI
https://hdl.handle.net/1912/355DOI
10.1575/1912/355Abstract
This is the first volume of a "final report" that summarizes, often in a speculative vein, what I have learned over
the past 35 years or so about large-scale, low-frequency ocean currents, primarily with support from the Office of
Naval Research (ONR). I was also fortunate to have been partially supported by the National Science Foundation
and, during the preparation of this report, by the Clark Foundation.
This report is meant to be an informal, occasionally anecdotal, state-of-the-art summary account of the World
Ocean Circulation (WOC). Seemingly simple questions about how ocean currents behave, such as where various
brands of sea water are coming from and going to, have been exciting and difficult research topics for many years.
This report is not remotely about "all" of the WOC, it is simply a set of comments about what I have looked into. I
believe that the results in this report, although presented in a personal way, are consistent with community wisdom.
The report is intended to be readable by non-specialists who have a basic scientific/technical background, especially
in other oceanographic areas or meteorology or physics or the geophysical disciplines, not just by specialists in
physical oceanography. Anyone wishing to get spun up on the observational basis for the WOC could use this report
and associated reference lists as a starting point.
Volume I concentrates on the North Atlantic Ocean although there is preliminary discussion of global features.
Highlights of this global summary are a new type of composite schematic picture of the World Ocean Circulation in
its "upper layers" (Figure I-I) and new summaries (Figures 1-12, 21,91) of the global "thermohaline" circulation.
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Suggested Citation
Technical Report: Schmitz, William J., "On the world ocean circulation. Volume I, some global features/North Atlantic circulation", 1996-06, DOI:10.1575/1912/355, https://hdl.handle.net/1912/355Related items
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