RADIATION FROM PLANET EARTH

Abstract

Information is given on the part played by the sun, earth's surface, and atmosphere in the heat balance of our planet. Following a general survey of solar and terrestrial radiation, including the emissivity and reflectivity of various terrestrial features (clouds, land masses, oceans), an estimate is made of the planetary radiation received by a satellite radiometer in five spectral channels covering the ultraviolet, visible, and infrared spectral regions. The wavelengths and purpose for selecting each of the channels is given. The signal-to-noise ratios associated with the received radiation in each channel using bolometers such as those in TIROS II and III, are included.

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Document Details

Document Type
Technical Report
Publication Date
Sep 01, 1961
Accession Number
AD0266790

Entities

People

  • I. L. Goldberg

Organizations

  • United States Army Communications-Electronics Command

Tags

Communities of Interest

  • Advanced Electronics
  • Energy and Power Technologies
  • Space

DTIC Thesaurus Topics

  • Artificial Satellites
  • Atmospheric Attenuation
  • Cloud Cover
  • Emissivity
  • Energy
  • Heat Balance
  • Heat Energy
  • Latent Heat
  • Particles
  • Radiation
  • Reflection
  • Reflectivity
  • Scattering
  • Sea Level
  • Solar Radiation
  • Terrestrial Radiation
  • Visible Spectra

Fields of Study

  • Physics

Readers

  • Atmospheric Science/Meteorology
  • Coastal and Marine Engineering/Sediment Transport/Hydraulic Engineering
  • Spectroscopy.

Technology Areas

  • Space