Investigation on cloud vertical structures based on Ka-band cloud radar observations at Wuhan in Central China

被引:5
|
作者
Fang, Junjie [1 ,2 ]
Huang, Kaiming [1 ,2 ,3 ]
Du, Minkang [1 ,2 ]
Zhang, Zirui [1 ,2 ]
Cao, Rang [1 ,2 ]
Yi, Fan [1 ,2 ,3 ]
机构
[1] Wuhan Univ, Sch Elect Informat, Wuhan, Peoples R China
[2] Minist Educ, Key Lab Geospace Environm & Geodesy, Wuhan, Peoples R China
[3] State Observ Atmospher Remote Sensing, Wuhan, Peoples R China
基金
中国国家自然科学基金;
关键词
Ka-band cloud radar; Cloud base and top heights; Cloud and precipitation occurrence frequencies; Wuhan in Central China; TIBETAN PLATEAU; WIND PROFILER; CIRRUS CLOUDS; DOPPLER RADAR; CLIMATE; LIDAR; PRECIPITATION; SATELLITE; BOUNDARY; HEIGHTS;
D O I
10.1016/j.atmosres.2022.106492
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Based on vertically pointing observations of Ka-band frequency-modulated continuous millimeter wave cloud radar (MMCR) in 2020, we investigate cloud vertical structures at Wuhan in central China. Case comparison indicates that the cloud top locations in the MMCR observation are largely consistent with those in satellite data. The precipitation has the occurrence frequency of 9.5% over the year, with the maximum value of 16.3% in July and the submaximal value of 14.7% in January, showing the significant influences of monsoons on precipitation at Wuhan. As the humid, cloudy and rainy climate, the probability of precipitation and non-precipitation clouds increases gradually from 53.9% in January to a large value of 71.5% in July. The non-precipitation clouds have the probability of 44.5% in the year, with two prominent peaks at the reflectivities of-35 to-30 dBZ around 12 km in summer and -37--32 dBZ around 10 km in spring. The cloud top can reach the heights of 14.49, 16.62, 13.38 and 11.73 km from spring to winter, respectively. The monthly mean cloud layer thickness is the largest (2.18 km) in May and September, and the smallest (1.36 km) in November. The seasonally averaged base and top heights and thickness of clouds have small diurnal variations. The high cloud is predominant in the warm months from May to September, and in the other cool months, the middle cloud has the most fraction. The quantitative investigation of clouds is helpful in improving the cloud parameterization in climate models.
引用
收藏
页数:11
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