Abstract
Possibilities of remote sensing of cirrus cloud ice mass content using spaceborne millimeter wavelength radar are analyzed. It is shown that measurements of radar reflectivity alone are generally insufficient to get unambiguous estimates of ice mass content. Ice mass content - radar reflectivity relationships, which are usually used for such estimates are sensitive to observational and meteorological conditions. Potential accuracy of these estimates can be significantly improved if independent information about characteristic cloud particle sizes is used.
| Original language | English |
|---|---|
| Pages (from-to) | 84-88 |
| Number of pages | 5 |
| Journal | Proceedings of SPIE - The International Society for Optical Engineering |
| Volume | 2309 |
| DOIs | |
| State | Published - Dec 23 1994 |
| Event | Passive Infrared Remote Sensing of Clouds and the Atmosphere II 1994 - Rome, Italy Duration: Sep 26 1994 → Sep 30 1994 |
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