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
Cite
CITATION STYLE
Barnes, G. M., Gamache, J. F., Lemone, M. A., & Stossmeister, G. J. (1991). A convective cell in a hurricane rainband. Monthly Weather Review, 119(3), 776–794. https://doi.org/10.1175/1520-0493(1991)119<0776:ACCIAH>2.0.CO;2
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