Radiation balance and albedo in the tropical Atlantic during ATEX 1969

Details Radiation balance and albedo in the tropical Atlantic during ATEX 1969 Radiation balance and albedo in the tropical Atlantic during ATEX 1969

Aug 1975

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975mtrma.......56h&link_type=abstract

Meteor-Forschungsergebnisse, Reihe B - Meteorologie und Aeronomie, Aug. 1975, p. 56-64. Research supported by the Deutsche Forsc

Computer Science

Atlantic Ocean, Atmospheric Heat Budget, Atmospheric Radiation, Earth Albedo, Radiation Measurement, Tropical Regions, Atmospheric Moisture, Marine Environments, Ocean Surface, Synoptic Measurement, Tables (Data), Wind Effects, Wind Measurement

Scientific paper

Components of the radiation balance measured by the Meteor and Planet balloons in 1969 over the Atlantic Ocean are presented. The albedo of the sea surface is calculated on the basis of Meteor data as a function of solar elevation angle for a cloudy day and a clear day. Daily total radiative energy increased from north to south due to increasing temperatures and water vapor concentrations in the atmosphere. Data show that cloudiness before noon is more influential than cloudiness after noon. Albedo values were slightly different from those obtained by Kondratyev (1969); this discrepancy is attributed to a rougher sea surface in the present than in the previous study.

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