The Environment of Precipitating Shallow Cumulus Convection

被引:109
作者
Nuijens, Louise [1 ]
Stevens, Bjorn [1 ,2 ]
Siebesma, A. Pier [3 ,4 ]
机构
[1] Univ Calif Los Angeles, Dept Atmospher & Ocean Sci, Los Angeles, CA 90095 USA
[2] Max Planck Inst Meteorol, Hamburg, Germany
[3] Royal Netherlands Meteorol Inst KNMI, De Bilt, Netherlands
[4] Delft Univ Technol, Dept Multiscale Phys, Delft, Netherlands
关键词
TRADE-WIND CLOUDS; TROPICAL OCEANS; DEEP CONVECTION; BOUNDARY-LAYER; RADAR ECHOES; WATER-VAPOR; RICO; RAIN; PACIFIC; CLIMATE;
D O I
10.1175/2008JAS2841.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Quantitative estimates of precipitation in a typical undisturbed trade wind region are derived from 2 months of radar reflectivity data and compared to the meteorological environment determined from soundings, surface flux, and airborne-lidar data. Shallow precipitation was ubiquitous, covering on average about 2% of the region and contributing to at least half of the total precipitation. Echo fractions on the scale of the radar domain range between 0% and 10% and vary greatly within a period from a few hours to a day. Variability in precipitation relates most strongly to variability in humidity and the zonal wind speed, although greater inversion heights and deeper clouds are also evident at times of more rain. The analysis herein suggests that subtle fluctuations in both the strength of the easterlies and in subsidence play a major role in regulating humidity and hence precipitation, even within a given meteorological regime (here, the undisturbed trades).
引用
收藏
页码:1962 / 1979
页数:18
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