
2010, ISBN: 9048178096
[EAN: 9789048178094], Neubuch, [SC: 0.0], [PU: Springer Netherlands], AERONOMY; ATMOSPHERICCHEMISTRY; METEOROLOGY; OZONEDEPLETION; WEATHER; ANTARCTICOZONEHOLE; EXCHANGETHROUGHTROPOPAUSE; STRATOSPHERE-TROPOSPHERECOUPLING; STRATOSPHERICCOOLING; TROPOSPHERICWEATHERSYSTEM; FLUID-ANDAERODYNAMICS, Druck auf Anfrage Neuware -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. 436 pp. Englisch, Books
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2010, ISBN: 9048178096
[EAN: 9789048178094], Neubuch, [SC: 0.0], [PU: Springer Netherlands], AERONOMY; ATMOSPHERICCHEMISTRY; METEOROLOGY; OZONEDEPLETION; WEATHER; ANTARCTICOZONEHOLE; EXCHANGETHROUGHTROPOPAUSE; STRATOSPHERE-TROPOSPHERECOUPLING; STRATOSPHERICCOOLING; TROPOSPHERICWEATHERSYSTEM, Druck auf Anfrage Neuware - 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. 436 pp. Englisch, Books
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ISBN: 9789048178094
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. Books > Science & Nature > Science > Earth Sciences > Meteorology & Climatology List_Books
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2010, ISBN: 9048178096
[EAN: 9789048178094], Neubuch, [PU: Springer Netherlands], AERONOMY ATMOSPHERICCHEMISTRY METEOROLOGY OZONEDEPLETION WEATHER ANTARCTICOZONEHOLE EXCHANGETHROUGHTROPOPAUSE STRATOSPHERE-TROPOSPHERECOUPLING STRATOSPHERICCOOLING TROPOSPHERICWEATHERSYSTEM GEOWISSENSCHAFTEN SONSTIGES ATMOSPHERIC CHEMISTRY OZONE DEPLETION, Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. A comprehensive stratosphere troposphere coupling textbookHighly illustrated with diagrams and figuresIncludes latest developments and provides problem setsA va, Books
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2010, ISBN: 9789048178094
An Introduction, Buch, Softcover, Softcover reprint of hardcover 1st ed. 2008, [PU: Springer], Springer, 2010
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2010, ISBN: 9048178096
[EAN: 9789048178094], Neubuch, [SC: 0.0], [PU: Springer Netherlands], AERONOMY; ATMOSPHERICCHEMISTRY; METEOROLOGY; OZONEDEPLETION; WEATHER; ANTARCTICOZONEHOLE; EXCHANGETHROUGHTROPOPAUSE; … Meer...

2010, ISBN: 9048178096
[EAN: 9789048178094], Neubuch, [SC: 0.0], [PU: Springer Netherlands], AERONOMY; ATMOSPHERICCHEMISTRY; METEOROLOGY; OZONEDEPLETION; WEATHER; ANTARCTICOZONEHOLE; EXCHANGETHROUGHTROPOPAUSE; … Meer...

ISBN: 9789048178094
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 weath… Meer...

2010, ISBN: 9048178096
[EAN: 9789048178094], Neubuch, [PU: Springer Netherlands], AERONOMY ATMOSPHERICCHEMISTRY METEOROLOGY OZONEDEPLETION WEATHER ANTARCTICOZONEHOLE EXCHANGETHROUGHTROPOPAUSE STRATOSPHERE-TROPO… Meer...
2010, ISBN: 9789048178094
An Introduction, Buch, Softcover, Softcover reprint of hardcover 1st ed. 2008, [PU: Springer], Springer, 2010
auteur: | |
Titel: | |
ISBN: |
Gedetalleerde informatie over het boek. - Stratosphere Troposphere Interactions
EAN (ISBN-13): 9789048178094
ISBN (ISBN-10): 9048178096
Gebonden uitgave
pocket book
Verschijningsjaar: 2010
Uitgever: Springer
436 Bladzijden
Gewicht: 0,655 kg
Taal: eng/Englisch
Boek bevindt zich in het datenbestand sinds 2012-06-05T16:21:41+02:00 (Amsterdam)
Detailpagina laatst gewijzigd op 2022-03-13T22:56:12+01:00 (Amsterdam)
ISBN/EAN: 9789048178094
ISBN - alternatieve schrijfwijzen:
90-481-7809-6, 978-90-481-7809-4
Gegevens van de uitgever
Auteur: K. Mohanakumar
Titel: Stratosphere Troposphere Interactions - An Introduction
Uitgeverij: Springer; Springer Netherland
416 Bladzijden
Verschijningsjaar: 2010-10-19
Dordrecht; NL
Gedrukt / Gemaakt in
Gewicht: 0,664 kg
Taal: Engels
64,19 € (DE)
65,99 € (AT)
71,00 CHF (CH)
POD
XVII, 416 p.
BC; Previously published in hardcover; Hardcover, Softcover / Geowissenschaften/Sonstiges; Meteorologie und Klimatologie (Klimaforschung); Verstehen; Aeronomy; Atmospheric chemistry; Meteorology; Ozone depletion; Troposphere; Weather; antarctic ozone hole; exchange through tropopause; stratosphere-troposphere coupling; stratospheric cooling; tropospheric weather system; fluid- and aerodynamics; B; Atmospheric Sciences; Earth Sciences, general; Thermodynamics; Fluid- and Aerodynamics; Atmospheric Science; Earth Sciences; Thermodynamics; Continuum Mechanics; Earth and Environmental Science; Geowissenschaften; Thermodynamik und Wärme; Klassische Mechanik; BB
Structure and Composition of the Lower and Middle Atmosphere.- Radiative Processes in the Lower and Middle Atmosphere.- Dynamics of the Troposphere and Stratosphere.- Waves in the Troposphere and Stratosphere.- Chemical Processes in the Stratosphere and Troposphere.- Stratospheric Ozone Depletion and Antarctic Ozone Hole.- Transport Processes in the Stratosphere and Troposphere.- Stratosphere–Troposphere Exchange.- Stratospheric Influence on Tropospheric Weather and Climate.Andere boeken die eventueel grote overeenkomsten met dit boek kunnen hebben:
Laatste soortgelijke boek:
9781402082160 Stratosphere Troposphere Interactions: An Introduction (Mohanakumar, K)
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