The incoming short wave radiation can be estimated based on several formulae. If the solar radiation at the exterior of the atmosphere is known, the incoming short wave radiation can be estimated based on an empirical formula of Black et al 1954:
where is the mean monthly cloudiness as decimal fraction and
is the extraterrestrial-radiation for the whole month in cal/cm²/day.
Another method of estimating is by means of the equation:
where are empirical constants,
are observed duration of sunshine hours per day and
are maximum possible duration of sunshine hours.
Location | a | b | Source |
---|---|---|---|
World | 0.23 | 0.48 | Black et al. 1954 |
World | 0.23*cos ![]() | 0.52 | Glover and McCulloch 1958 |
S.E. England | 0.18 | 0.55 | Penman 1948 |
Virgina U.S.A | 0.22 | 0.54 | in Penman 1948 |
Canberra Australia | 0.25 | 0.54 | in Penman 1948 |
Brisbane Australia | 0.23 to 0.35 | 0.38 to 0.54 | Cartledge 1973 |
West Africa | -0.12 to 0.26 | 0.99 to 0.50 | Davies 1966 |