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Titlebook: Radiation in a Cloudy Atmosphere; E. M. Feigelson Book 1984 D. Reidel Publishing Company, Dordrecht, Holland 1984 Absorption.Aerosol.Albed

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书目名称Radiation in a Cloudy Atmosphere
编辑E. M. Feigelson
视频video
丛书名称Atmospheric and Oceanographic Sciences Library
图书封面Titlebook: Radiation in a Cloudy Atmosphere;  E. M. Feigelson Book 1984 D. Reidel Publishing Company, Dordrecht, Holland 1984 Absorption.Aerosol.Albed
描述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 radia­ tion. 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 relation­ ships between the indicate
出版日期Book 1984
关键词Absorption; Aerosol; Albedo; Cloud; cloud amount; cloudiness; temperature
版次1
doihttps://doi.org/10.1007/978-94-009-6443-3
isbn_softcover978-94-009-6445-7
isbn_ebook978-94-009-6443-3Series ISSN 1383-8601 Series E-ISSN 2215-162X
issn_series 1383-8601
copyrightD. Reidel Publishing Company, Dordrecht, Holland 1984
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https://doi.org/10.1007/978-94-009-6443-3Absorption; Aerosol; Albedo; Cloud; cloud amount; cloudiness; temperature
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Methods of Calculating Thermal Radiation2, 24], and in a number of collections and original articles. In this chapter we will present only some of the initial relations and we will describe some of the approximate calculation methods used in practice.
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Spatial Structure of CloudsWhen studying any mean characteristics of clouds over a time ., one should bear in mind that these characteristics relate only to the part of the period during which cloudiness was observed.
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Space-Time Statistical Structure of a Cumulus FieldWhen applying any of the methods for calculating the radiation regime and its variability for cumulus clouds, in addition to the optical characteristics of an individual cloud it is important to know something about the size distribution of the clouds and the structure of the cloud field.
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An Optical Model of the AtmosphereWhen calculating fluxes of ultraviolet and visible radiation, we can arrive at an optical model by specifying the quantities .and also the coefficient of ozone absorption α. and the aerosol absorption α..
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