study of some aspects of the radiation and heat budgets of the southern hemisphere oceans
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study of some aspects of the radiation and heat budgets of the southern hemisphere oceans by J. W. Zillman

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Published by Australian Government Publishing Service in Canberra .
Written in English

Subjects:

Places:

  • Indian Ocean.

Subjects:

  • Ocean-atmosphere interaction -- Indian Ocean.,
  • Heat budget (Geophysics),
  • Oceanography -- Indian Ocean.

Book details:

Edition Notes

Statement[by] J. W. Zillman.
SeriesBureau of Meteorology, Dept. of the Interior. Meteorological study, no. 26, Meteorological study ;, no. 26.
Classifications
LC ClassificationsQC851 .A84 no. 26, GC190 .A84 no. 26
The Physical Object
Pagination562 p.
Number of Pages562
ID Numbers
Open LibraryOL5082184M
LC Control Number74153222

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Surface Energy Budget. To understand how the Earth’s climate system balances the energy budget, we have to consider processes occurring at the three levels: the surface of the Earth, where most solar heating takes place; the edge of Earth’s atmosphere, where sunlight enters the system; and the atmosphere in : Rebecca Lindsey.   Motivated by these issues, a large international multi-agency effort called the Southern Ocean Clouds, Radiation, Aerosol Transport Experimental Study (SOCRATES) will be conducted to improve our understanding of clouds, aerosols, air-sea exchanges, and their interactions over the Southern Ocean. The oceans absorb much of the solar energy that reaches earth, and thanks to the high heat capacity of water, the oceans can slowly release heat over many months or years. The oceans store more heat in the uppermost 3 meters (10 feet) that the entire atmosphere, the key to understanding global climate change is inextricably linked to the ocean.   N.G. Loeb, B.A. Wielicki, in Encyclopedia of Atmospheric Sciences (Second Edition), Impact of Clouds on Earth's Radiation Budget at the TOA, at the Surface, and within the Atmosphere. Clouds have an important role in modulating the TOA, within-atmosphere, and surface radiation budgets at both visible and terrestrial infrared wavelengths.