Albedos

Abstract

The albedo of the earth's surface varies dramatically from values of about 3 to 4 percent for calm bodies of water up to about 55 percent for gypsum sands. This rather broad range of reflected incoming solar radiation presents difficulties when attempting to define an average albedo for terrain over a large region from locally determined values. The patchwork, or checkerboard, appearance of the earth's surface as viewed from above is the result of various human activities, such as agriculture, the proliferation of urban sprawl, and road building. Each of these variable appearing surfaces will have individual albedos, rendering any attempt to determine an areal albedo almost an impossibility on the mesoscale. However, a vast data base exists for microscale applications for individual acreages, for example. A compilation of these data is presented.

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Document Details

Document Type
Technical Report
Publication Date
Jul 01, 1993
Accession Number
ADA268255

Entities

People

  • Frank V. Hansen

Organizations

  • United States Army Research Laboratory

Tags

Communities of Interest

  • Space
  • Weapons Technologies

DTIC Thesaurus Topics

  • Agriculture
  • Artillery
  • Atmospheric Sciences
  • Electromagnetic Radiation
  • Flight
  • Forests
  • Materials
  • Military Research
  • North America
  • Radiation
  • Snow Cover
  • Solar Radiation
  • Surface Properties
  • Terrain
  • Urban Areas
  • Urban Sprawl
  • Warfare

Readers

  • Educational Psychology
  • Solar Physics
  • Urban Planning and Geography.