Abstract
Millimeter wave radars are considered primarily as cloud radars due to their high sensitivity on weak targets such as shallow cloud. A unique application of millimeter wave radars is presented. This application capitalizes on the use of Mie scattering peculiarities as a means to identify raindrops of a given size in a dropsize distribution.
| Original language | English (US) |
|---|---|
| Title of host publication | Conference on Radar Meteorology |
| Publisher | American Meteorological Soc |
| Pages | 446-449 |
| Number of pages | 4 |
| State | Published - 1999 |
| Event | Proceedings of the 1999 29th International Conference on Radar Meteorology - Montreal, Que., Can Duration: Jul 12 1999 → Jul 16 1999 |
Other
| Other | Proceedings of the 1999 29th International Conference on Radar Meteorology |
|---|---|
| City | Montreal, Que., Can |
| Period | 7/12/99 → 7/16/99 |
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ASJC Scopus subject areas
- Atmospheric Science
- Electrical and Electronic Engineering
Cite this
Millimeter-wave radar observations of vertical air motion structure and evolution in precipitation. / Kollias, P.; Lhermitte, R.; Albrecht, Bruce A.
Conference on Radar Meteorology. American Meteorological Soc, 1999. p. 446-449.Research output: Chapter in Book/Report/Conference proceeding › Chapter
}
TY - CHAP
T1 - Millimeter-wave radar observations of vertical air motion structure and evolution in precipitation
AU - Kollias, P.
AU - Lhermitte, R.
AU - Albrecht, Bruce A
PY - 1999
Y1 - 1999
N2 - Millimeter wave radars are considered primarily as cloud radars due to their high sensitivity on weak targets such as shallow cloud. A unique application of millimeter wave radars is presented. This application capitalizes on the use of Mie scattering peculiarities as a means to identify raindrops of a given size in a dropsize distribution.
AB - Millimeter wave radars are considered primarily as cloud radars due to their high sensitivity on weak targets such as shallow cloud. A unique application of millimeter wave radars is presented. This application capitalizes on the use of Mie scattering peculiarities as a means to identify raindrops of a given size in a dropsize distribution.
UR - http://www.scopus.com/inward/record.url?scp=0032641210&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0032641210&partnerID=8YFLogxK
M3 - Chapter
SP - 446
EP - 449
BT - Conference on Radar Meteorology
PB - American Meteorological Soc
ER -