摘要
根据广州强对流天气发生前新一代天气雷达(CINRAD/SA)观测的晴空回波谱宽资料,经过数据质量控制和预处理,估算了不同高度的湍流耗散率,发现这次强对流天气过程发生前,低层的湍流耗散率明显增强,揭示了这次强对流天气过程的前兆特征。
A series of severe convective storms affected Guangdong Province and produced disastrous heavy rain in Guangzhou especially on August 11,2004. This paper introduces the elementary formation mechanisms for clear air-echo before severe convection and trys to extract the dissipation rate of turbulent energy 8 from the spectral data of CINRAD/SA in Guangzhou. The results show that the turbulence energy dissipation rate in the low atmosphere layer obviously increased before the severe convective storms occurred, which reveals the precursory character of this weather phenomena.
出处
《南京气象学院学报》
CSCD
北大核心
2007年第6期814-818,共5页
Journal of Nanjing Institute of Meteorology
基金
国家自然科学基金资助项目(40475017)
关键词
新一代天气雷达
晴空回波
谱宽
湍流耗散率
CINRAD
clear-air echo
spectrum width
dissipation rate of turbulent energy