Thermo Spheric Circulation (Progress in Astronautics & Aeronautics Series) by W. Webb

Cover of: Thermo Spheric Circulation (Progress in Astronautics & Aeronautics Series) | W. Webb

Published by Amer Inst of Aeronautics & .

Written in English

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  • Astronautics,
  • Flow, turbulence, rheology,
  • Science/Mathematics

Book details

The Physical Object
Number of Pages372
ID Numbers
Open LibraryOL10237718M
ISBN 100262230534
ISBN 109780262230537

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Thermo Spheric Circulation (Progress in Astronautics & Aeronautics Series) by W. Webb, JuneAmer Inst of Aeronautics & edition, Hardcover in EnglishPages: American Institute of Aeronautics and Astronautics Sunrise Valley Drive, Suite Reston, VA   MODEL The thermospheric temperature structure and circulation is calculated using the NCAR thermo- spheric general circulation model (TGCM) as described in detail by Dickinson et al.

The model has a 5 latitude-by-longitude grid with 24 constant-pressure surface layers in the vertical, extending from approx.

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There are, however, reasonable grounds for reevaluating accepted ideas about the zonal variation of winds in the mid—latitude thermosphere. Pirst of all, there has been the appearance of semi—empirical models of thermo— spheric composition and temperature /5,6, etc./ which depict longitudinal depondences of the modelled parameters.

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corrected method of Boris and Book () is used. The paper is organized as follows: the scaling law of. spheric circulation phenomena can be either stationary or episodic. In hurricanes and tornadoes the rate of water vapor condensation is determined by the maximum velocity u E of air masses accelerated by force f E; condensation rate exceeds the evaporation rate dictated by solar power by many orders of magnitude.

The stationary pattern. convective mode of motion as the thermo-haline circulation. But results of the past few years suggest that such a convectively driven mass flux is impossible. There are several lines of argument. The first goes back to Sandström (4), who pointed out that when a fluid is heated and cooled at the.

Download Center Click on the language to view the e-book in your preferred you want to save the publication, click “PDF” in the ebook view. Available languages. The deep circulation, on the other hand, acts on much longer timescales.

This component is sometimes referred to as the “thermohaline” circulation, due to its dependence on changes in temperature (“thermo”) and salinity (“haline”), both of which regulate the density of seawater.

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Thermohaline circulation, also called Global Ocean Conveyor or Great Ocean Conveyor Belt, the component of general oceanic circulation controlled by horizontal differences in temperature and salinity. It continually replaces seawater at depth with water from the surface and slowly replaces surface water elsewhere with water rising from deeper depths.

(Marengo, ). Major problems have been identified with the prevailing thermo-dynamic approach to describing hurricanes (Smith et al., ; Makarieva et al., ). Furthermore, so far it has not been possible to derive a quantitatively realistic theory of Hadley circulation based on the effects of differential heating.

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McDermott Drive West Chester, Pennsylvania United States of America. Phone: + Toll Free: + Fax: + E-Mail: [email protected] circulation begins in the Earth's polar regions. When ocean water in these areas gets very cold, sea ice forms.

The surrounding seawater gets saltier, increases in density and sinks. Winds drive ocean currents in the upper meters of the ocean’s surface. However, ocean currents.

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