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机构地区:[1]Nanjing Institute of Meteorology,Nanjing 210044 [2]China Meteorological Administration,Beijing 100081 [3]Meteorological Observatory of Anhui Province,Hefei 230061
出 处:《Acta meteorologica Sinica》2002年第3期388-400,404,共14页
摘 要:A hail process in Huaihe River Basin observed by CINRAD Doppler radar on 12May 2000 has been simulated by using nonhydrostatic mesoscale numerical model MM5.The simulated wind field is analyzed and compared with Doppler radar wind data,both of them show that there was a meso-β cyclone around the hail region.Results show that this meso-β cyclone existed below 3 km in the troposphere and its cyclonic circulation was very obvious below 1 km.The temperature and moisture fields from the simulation are also analyzed.Furthermore,the storm-relative environmental helicity and CAPE(convective available potential energy)are discussed.A hail process in Huaihe River Basin observed by CINRAD Doppler radar on 12May 2000 has been simulated by using nonhydrostatic mesoscale numerical model MM5.The simulated wind field is analyzed and compared with Doppler radar wind data,both of them show that there was a meso-β cyclone around the hail region.Results show that this meso-β cyclone existed below 3 km in the troposphere and its cyclonic circulation was very obvious below 1 km.The temperature and moisture fields from the simulation are also analyzed.Furthermore,the storm-relative environmental helicity and CAPE(convective available potential energy)are discussed.
关 键 词:hail process numerical simulations radar observation meso-β cyclone
分 类 号:TN959.4[电子电信—信号与信息处理]
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