The complex flows in the atmosphere and oceans are believed to be accurately modelled by the Navier-Stokes equations of fluid mechanics together with classical thermodynamics. However, due to the enormous complexity of these equations, meteorologists and oceanographers have constructed approximate m
Large-Scale Transport Processes in Oceans and Atmosphere
โ Scribed by Maurice L. Blackmon (auth.), J. Willebrand, D. L. T. Anderson (eds.)
- Publisher
- Springer Netherlands
- Year
- 1986
- Tongue
- English
- Leaves
- 383
- Series
- NATO ASI Series 190
- Edition
- 1
- Category
- Library
No coin nor oath required. For personal study only.
โฆ Synopsis
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 oceanography and meteorology have largely been carried out separately. But for climate research both disciplines must interact strongly, and another ob jecti ve of this school was to bring together both oceanographers and meteorologists. To promote an integrated approach, the lecture presentations were divided into two formats.
โฆ Table of Contents
Front Matter....Pages i-xii
Building, Testing and Using a General Circulation Model....Pages 1-70
Some Topics in the General Circulation of the Atmosphere....Pages 71-104
Lectures on Ocean Circulation Dynamics....Pages 105-161
Thermohaline Effects in the Ocean Circulation and Related Simple Models....Pages 163-200
Diagnostic Models of Ocean Circulation....Pages 201-223
Wind Driven Ocean Circulation Theory โ Steady Free Flow....Pages 225-245
Coupled Ocean-Atmosphere Models of El Nino and the Southern Oscillation....Pages 247-280
Maximum Entropy Production as a Constraint in Climate Models....Pages 281-323
Heat Transfer by Thermal Convection in a Rotating Fluid Subject to a Horizontal Temperature Gradient....Pages 325-336
Some Aspects of Turbulent Diffusion....Pages 337-357
Turbulent Diffusion in Large-Scale Flows....Pages 359-373
Back Matter....Pages 375-379
โฆ Subjects
Oceanography
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