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) |
|---|---|
| Pages (from-to) | 566-578 |
| Number of pages | 13 |
| Journal | Journal of Applied Meteorology |
| Volume | 21 |
| Issue number | 4 |
| DOIs | |
| State | Published - 1982 |
| Externally published | Yes |