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One of the most crucial but still very poorly understood topics of oceanographic science is the role of ocean processes in contributing to the dynamics of climate and global change. This book presents a series of high level lectures on the major categories of ocean/atmosphere processes. Three of these major issues are the focus of the lectures: (1) air--sea interaction processes; (2) water mass formation, dispersion and mixing; (3) general circulation, with specific emphasis on the thermohaline component. Global examples in the world ocean are provided and discussed in the lectures. In parallel, the Mediterranean Sea is a laboratory basin in providing analogues of the above global processes relevant to climate dynamics. They include the Mediterranean thermohaline circulation with its own `conveyor belt'; intermediate and deep water mass formation and transformations, dispersion and mixing. No other book in the field provides a review of fundamental lectures on these processes, coupled with global examples and their Mediterranean analogues.
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Previews available in: English
Edition | Availability |
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1
Ocean Processes in Climate Dynamics: Global and Mediterranean Examples
2012, Springer
in English
9401108706 9789401108706
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2
Ocean Processes in Climate Dynamics: Global and Mediterranean Examples
2012, Springer
in English
9401043760 9789401043762
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3
Ocean processes in climate dynamics: global and mediterranean examples
1994, Kluwer Academic
in English
0792326245 9780792326243
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4
Ocean Processes in Climate Dynamics: Global and Mediterranean Examples (NATO Science Series C: (closed))
December 31, 1899, Springer
Hardcover
in English
- 1 edition
0792326245 9780792326243
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zzzz
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Book Details
Edition Notes
Includes bibliographical references and index.
"Published in cooperation with NATO Scientific Affairs Division."
"Proceedings of the NATO Advanced Study Institute on Ocean Processes in Climate Dynamics: Global and Mediterranean Examples, Erice, Italy, January 20-February 2, 1993"--T.p. verso.
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- Created April 1, 2008
- 10 revisions
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