Abstract
A band model for atmospheric absorption is used to calculate the incoming longwave atmospheric radiative flux for some typical clear sky conditions. The sky radiation is also measured using a specially-designed calorimetric apparatus over a wide range of ground-level atmospheric conditions. Good agreement is obtained between the measurement and the calculation using appropriate atmospheric conditions. -from Authors
Original language | English (US) |
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Pages (from-to) | 566-578 |
Number of pages | 13 |
Journal | Journal of Applied Meteorology |
Volume | 21 |
Issue number | 4 |
DOIs | |
State | Published - 1982 |