Actions for Radiation in a Cloudy Atmosphere [electronic resource]

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Radiation in a Cloudy Atmosphere [electronic resource] / edited by E. M. Feigelson

Published
Dordrecht : Springer Netherlands, 1984.
Physical Description
IX, 293 pages : online resource
Additional Creators
Feĭgelʹson, E. M. (Eva Mikhaĭlovna) and SpringerLink (Online service)
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Contents
I. Cloud Structures and Optical Characteristics of Clouds -- 1. Spatial Structure of Clouds -- 2. Physical Characteristics of Clouds -- 3. Space-Time Statistical Structure of a Cumulus Field -- 4. Optical Properties of Clouds -- 5. An Optical Model of the Atmosphere -- II. Photon Paths in Clouds -- 6. Calculations for Various Cloud Types -- 7. Experimental Determination of Effective Photon Path Lengths -- III. Fluxes of Solar Radiation -- 8. Visible and Ultraviolet Radiation -- 9. Integral Solar Radiation -- 10. Experimental Aircraft Studies of Solar Fluxes in the Presence of Stratiform Clouds -- 11. Solar Fluxes in the Presence of Cumulus Clouds -- IV. Thermal Radiation of a Cloudy Atmosphere -- 12. Methods of Calculating Radiation -- 13. Experimental Studies of the Thermal Radiation of a Cloudy Atmosphere -- 14. Effect of Optical Properties of Clouds on Thermal Radiation -- V. Regional Features of the Radiation Regime of a Cloudy Atmosphere -- 15. The Polar Regions -- 16. Radiation Regime of the Tropical Central Atlantic -- References.
Summary
Radiative heat transfer is a fundamental factor in the energetics of the terrestrial atmosphere: the system consisting of the atmosphere and the underlying layer is heated by the Sun, and this heating is compensated, on the average, by thermal radiation. Only over a period of 1-3 days from some specified initial moment can the dynamic processes in the atmosphere be considered to be adiabatic. Global dynamic processes of long duration are regulated by the actual influxes of heat, one of the main ones being the radiative influx. Radiation must be taken into account in long-term, weather forecasting and when considering the global circulation of the atmosphere, the theory of climate, etc. Thus it is necessary to know the albedo of the system, the amount of solar radiation transmitted by the atmosphere, the absorptivity of the atmosphere vis-a-vis solar radiation, and also the effective radiation flux, the divergence of which represents the radiative cooling or heating. All these quantities have to be integrated over the wavelength spectrum of the solar or thermal radiation, and they must be ascertained as functions of the determining factors. The relationships between the indicated radiation characteristics, the optical quantities directly determining them, the optically active components of the atmosphere, and the meteorological fields will be discussed in this book.
Subject(s)
ISBN
9789400964433
Digital File Characteristics
text file PDF
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AVAILABLE ONLINE TO AUTHORIZED PSU USERS.
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Springer eBooks
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