Ozone in the Troposphere and Stratosphere, Part 2
Author :
Publisher :
Page : 606 pages
File Size : 38,72 MB
Release : 1994
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ISBN :
Author :
Publisher :
Page : 606 pages
File Size : 38,72 MB
Release : 1994
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Author : R. D. HUDSON
Publisher :
Page : 528 pages
File Size : 15,42 MB
Release : 1994
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Author :
Publisher :
Page : 506 pages
File Size : 24,37 MB
Release : 1994
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Author : Robert D. Hudson
Publisher :
Page : 596 pages
File Size : 34,43 MB
Release : 1994
Category : Atmospheric ozone
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Author : Siegfried Böhme
Publisher : Springer Science & Business Media
Page : 851 pages
File Size : 46,83 MB
Release : 2013-04-18
Category : Science
ISBN : 3662123258
Author : Rolf Müller (physicien.)
Publisher : Royal Society of Chemistry
Page : 347 pages
File Size : 39,25 MB
Release : 2012
Category : Science
ISBN : 1849730024
In recent years, several new concepts have emerged in the field of stratospheric ozone depletion, creating a need for a concise in-depth publication covering the ozone-climate issue. This monograph fills that void in the literature and gives detailed treatment of recent advances in the field of stratospheric ozone depletion. It puts particular emphasis on the coupling between changes in the ozone layer and atmospheric change caused by a changing climate. The book, written by leading experts in the field, brings the reader the most recent research in this area and fills the gap between advanced textbooks and assessments.
Author : Robert D. Hudson
Publisher :
Page : 539 pages
File Size : 17,94 MB
Release : 1994
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Author :
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Page : 534 pages
File Size : 11,42 MB
Release : 2004
Category : Meteorological optics
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Author : K. Mohanakumar
Publisher : Springer Science & Business Media
Page : 424 pages
File Size : 16,83 MB
Release : 2008-07-03
Category : Science
ISBN : 1402082177
Stratospheric processes play a signi?cant role in regulating the weather and c- mate of the Earth system. Solar radiation, which is the primary source of energy for the tropospheric weather systems, is absorbed by ozone when it passes through the stratosphere, thereby modulating the solar-forcing energy reaching into the t- posphere. The concentrations of the radiatively sensitive greenhouse gases present in the lower atmosphere, such as water vapor, carbon dioxide, and ozone, control the radiation balance of the atmosphere by the two-way interaction between the stratosphere and troposphere. The stratosphere is the transition region which interacts with the weather s- tems in the lower atmosphere and the richly ionized upper atmosphere. Therefore, this part of the atmosphere provides a long list of challenging scienti?c problems of basic nature involving its thermal structure, energetics, composition, dynamics, chemistry, and modeling. The lower stratosphere is very much linked dynamically, radiatively,and chemically with the upper troposphere,even though the temperature characteristics of these regions are different. The stratosphere is a region of high stability, rich in ozone and poor in water - por and temperature increases with altitude. The lower stratospheric ozone absorbs the harmful ultraviolet (UV) radiation from the sun and protects life on the Earth. On the other hand, the troposphere has high concentrations of water vapor, is low in ozone, and temperature decreases with altitude. The convective activity is more in the troposphere than in the stratosphere.
Author : Air Pollution Technical Information Center
Publisher :
Page : 198 pages
File Size : 22,93 MB
Release : 1969
Category : Air
ISBN :