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Journal Article

The environment of precipitating shallow cumulus convection

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Nuijens,  L.
Observations and Process Studies, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society;

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Stevens,  Bjorn       
Director’s Research Group AES, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society;

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JAS-66-2009-1962.pdf
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Citation

Nuijens, L., Stevens, B., & Siebesma, A. P. (2009). The environment of precipitating shallow cumulus convection. Journal of the Atmospheric Sciences, 66(7), 1962-1979. doi:10.1175/2008JAS2841.1.


Cite as: https://hdl.handle.net/11858/00-001M-0000-0011-F7D9-A
Abstract
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). [References: 45]