Abstract
Theoretical calculations of the upwelling microwave radiances from clouds containing layers of rain, ice, and a melting region were performed at frequencies of 18, 37, and 92GHz. These frequencies coincide with high-resolution microwave radiometer measurements taken aboard the NASA ER-2 high-altitude aircraft during the summer 1986 COHMEX (Cooperative Huntsville Meteorological Experiment) in Alabama. For purposes of brightness temperature computations, the storms were modeled with rain, melting phase, and ice layers. The melting phase region was composed of water-coated ice spheres defined by a "melt index' in terms of the volume fraction of water. Single scatter albedo, scattering, and extinction coefficients were computed at the above frequencies as a function of the rain rate and melt index. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 561-585 |
| Number of pages | 25 |
| Journal | Journal of Applied Meteorology |
| Volume | 29 |
| Issue number | 7 |
| DOIs | |
| State | Published - 1990 |
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