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Solar radiation and the duration of sunshine in Trinidad, West Indies

✍ Scribed by G. W. Smith


Publisher
John Wiley and Sons
Year
1959
Tongue
English
Weight
147 KB
Volume
85
Category
Article
ISSN
0035-9009

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✦ Synopsis


Abstract

Records of daily solar radiation energy extending over a period of one year have been compared with readings of sunlight duration obtained with a Campbell‐Stokes recorder. Energy records were made with a bimetallic antinograph. The regression equation obtained for the daily values in Trinidad, West Indies was R = R~A~ (0Β·20 + 0Β·59 n/N), with a correlation coefficient of 0Β·91 where R = radiation actually received

R~A~ = Angot's theoretical amounts of radiation which would reach the earth's surface in the absence of an atmosphere. These values are given by List (1951)

n = actual duration of sunlight

N = theoretical maximum duration of sunlight.


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