Abstract
On 10 October 1983 the two NOAA WP-3D aircraft completed a mission designed to provide airborne Doppler radar data for a convective cell embedded in a weak rainband on the trailing side of Hurricane Raymond. Comparisons of the wind field produced from the pseudo-dual-Doppler radar technique with in situ wind measurements suggest that the larger convective-scale features may be resolved if the sampling time is kept to a minimum. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 776-794 |
| Number of pages | 19 |
| Journal | Monthly Weather Review |
| Volume | 119 |
| Issue number | 3 |
| DOIs | |
| State | Published - 1991 |
| Externally published | Yes |
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