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Titlebook: Large-Scale Transport Processes in Oceans and Atmosphere; J. Willebrand,D. L. T. Anderson Book 1986 Springer Science+Business Media Dordre

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书目名称Large-Scale Transport Processes in Oceans and Atmosphere
编辑J. Willebrand,D. L. T. Anderson
视频video
丛书名称Nato Science Series C:
图书封面Titlebook: Large-Scale Transport Processes in Oceans and Atmosphere;  J. Willebrand,D. L. T. Anderson Book 1986 Springer Science+Business Media Dordre
描述One of the major experiments in earth science at the present time is about to begin: the World Climate Research Program (WCRP). The objectives of WCRP are to determine the extent to which climate change can be predicted, and the extent to which human activities (such as increasing the level of CO ) can influence our climate. 2 To understand and possibly to predict climate change, one needs a good understanding of the dynamics of the ocean, the atmosphere, and the processes by which they are coupled. Two major programs are being developed within WCRP: TOGA (Tropical Oceans, Global Atmosphere) and WOCE (World Ocean CirculatIon Experiment). The success of these programs will depend on many things, not least of which is the existence of a pool of active young researchers. This NATO Advanced Study Institute brought together students and young scientists from 13 countries, most of them from Europe and North America. The objective was to provide them with a background in the perceived state of knowledge of atmosphere and ocean dynamics, and to mediate a flavour of the problems presently concerning scientists active in climate related dynamics. In the past, the two disciplines of oceanogra
出版日期Book 1986
关键词Global climate model; Meteorology; North America; atmosphere; carr; climate; energy; entropy; geoscience; oce
版次1
doihttps://doi.org/10.1007/978-94-009-4768-9
isbn_softcover978-94-010-8617-2
isbn_ebook978-94-009-4768-9Series ISSN 1389-2185
issn_series 1389-2185
copyrightSpringer Science+Business Media Dordrecht 1986
The information of publication is updating

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Diagnostic Models of Ocean Circulation,ctives of the diagnostic approach include the determination of circulation parameters (in particular the three-dimensional velocity field) and the testing of dynamical concepts (especially the role of mixing in the budgets of heat, salt and potential vorticity).
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1389-2185 es of WCRP are to determine the extent to which climate change can be predicted, and the extent to which human activities (such as increasing the level of CO ) can influence our climate. 2 To understand and possibly to predict climate change, one needs a good understanding of the dynamics of the oce
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Maximum Entropy Production as a Constraint in Climate Models,rch for simple “laws” which control the mean system. (Here a mean would usually be a time average over years or longer with, in addition, possible spatial averaging.) Progress towards a solution to the climate problem is likely to come about by a combination of these two methods.
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Thermohaline Effects in the Ocean Circulation and Related Simple Models,” developed the instruments needed to measure these and other oceanographic parameters of interest with the required accuracy. They also developed the theoretical tools by help of which the ocean currents could be calculated from the measured temperature and salinity fields, in particular the so-called “dynamic method”.
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Some Topics in the General Circulation of the Atmosphere,of equations are used to investigate the importance of orographic and thermal forcing and the role played by transients on the synoptic and longer time-scales..The usefulness of considering maps of potential vorticity on isentropic surfaces for the diagnosis of the behaviour of synoptic systems in t
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