期刊
JOURNAL OF TROPICAL METEOROLOGY
卷 27, 期 3, 页码 291-302出版社
JOURNAL OF TROPICAL METEOROLOGICAL PRESS
DOI: 10.46267/j.1006-8775.2021.026
关键词
turbulent dissipation rate; rainfall microphysical parameters; wind profiler radar; spectrum width; collision coalescence; breakup; retrieval
资金
- National Key R&D Program of China [2018YFC1506102]
This study utilized boundary layer wind profiler radar measurements to explore the influence of turbulence on rainfall microphysical parameters. It was found that small raindrops grow in weak turbulence, while large raindrops break up in strong turbulence. The variation of rainfall microphysical parameters is more significant in the middle stage of rainfall events, and turbulence impacts on raindrop size and number concentration are more pronounced than on rain rate and liquid water content.
Rainfall is triggered and mainly dominated by atmospheric thertno-dynatnics and rich water vapor. Nonetheless, turbulence is also considered as an important factor influencing the evolution of rainfall microphysical parameters. To study such an influence, the present study utilized boundary layer wind profiler radar measurements. The separation point of the radar power spectral density data was carefully selected to classify rainfall and turbulence signals; the turbulent dissipation rate e and rainfall microphysical parameters can be retrieved to analyze the relationship between and microphysical parameters. According to the retrievals of two rainfall periods in Beijing 2016, it was observed that (I) 8 in the precipitation area ranged from 10(-3.5) to 10(-1) m(2) s(-3) and was positively correlated with the falling velocity spectrum width; (2) interactions between turbulence and raindrops showed that small raindrops got enlarge through collision and coalescence in weak turbulence, but large raindrops broke up into small drops under strong turbulence, and the separation value of 8. being weak or strong varied with rainfall attributes; (3) the variation of rainfall microphysical parameters (characteristic diameters, number concentration, rainfall intensity, and water content) in the middle stage were stronger than those in the early and the later stages of rainfall event; (4) unlike the obvious impacts on raindrop size and number concentration, turbulence impacts on rain rate and LWC were not significant because turbulence did not cause too much water vapor and heat exchange.
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