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Radiation in a Cloudy Atmosphere

  • E. M. Feigelson

Part of the Atmospheric Sciences Library book series (ATSL, volume 6)

Table of contents

  1. Front Matter
    Pages I-IX
  2. Introduction

    1. E. M. Feigelson
      Pages 1-2
  3. Cloud Structures and Optical Characteristics of Clouds

    1. Front Matter
      Pages 3-3
    2. E. M. Feigelson
      Pages 4-15
    3. E. M. Feigelson
      Pages 16-31
    4. E. M. Feigelson
      Pages 43-66
    5. E. M. Feigelson
      Pages 67-79
  4. Photon Paths in Clouds

    1. Front Matter
      Pages 80-83
    2. E. M. Feigelson
      Pages 84-102
  5. Fluxes of Solar Radiation

    1. Front Matter
      Pages 117-117
    2. E. M. Feigelson
      Pages 118-135
    3. E. M. Feigelson
      Pages 136-151
    4. E. M. Feigelson
      Pages 177-196
  6. Thermal Radiation of a Cloudy Atmosphere

    1. Front Matter
      Pages 197-197
    2. E. M. Feigelson
      Pages 198-205
  7. Regional Features of the Radiation Regime of a Cloudy Atmosphere

    1. Front Matter
      Pages 232-232
    2. E. M. Feigelson
      Pages 233-244
  8. Back Matter
    Pages 261-293

About this book

Introduction

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 indicated radiation characteristics, the optical quantities directly determining them, the optically active compo­ nents of the atmosphere, and the meteorological fields will be discussed in this book.

Keywords

Absorption Aerosol Albedo Cloud cloud amount cloudiness temperature

Editors and affiliations

  • E. M. Feigelson
    • 1
  1. 1.Institute of Atmospheric PhysicsAcademy of SciencesU.S.S.R.

Bibliographic information

  • DOI https://doi.org/10.1007/978-94-009-6443-3
  • Copyright Information Springer Science+Business Media B.V. 1984
  • Publisher Name Springer, Dordrecht
  • eBook Packages Springer Book Archive
  • Print ISBN 978-94-009-6445-7
  • Online ISBN 978-94-009-6443-3
  • Series Print ISSN 1383-8601
  • Buy this book on publisher's site
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