Raindrop Size Distribution Characteristics for Typhoons over the Coast in Eastern China

被引:0
|
作者
Wang, Dongdong [1 ]
Chen, Sheng [2 ,3 ]
Kong, Yang [1 ]
Gu, Xiaoli [1 ]
Li, Xiaoyu [4 ]
Nan, Xuejing [5 ]
Yue, Sujia [1 ]
Shen, Huayu [1 ]
机构
[1] Ningbo Meteorol Bur, Ningbo Meteorol Observ Academician Workstat, Ningbo 315012, Peoples R China
[2] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Remote Sensing Gansu Prov, Heihe Remote Sensing Expt Res Stn, Lanzhou 730000, Peoples R China
[3] Southern Lab Ocean Sci & Engn, Zhuhai 519000, Peoples R China
[4] Jiaying Univ, Sch Geog & Tourism, Meizhou 514015, Peoples R China
[5] China Meteorol Adm, Meteorol Observat Ctr, Beijing 100081, Peoples R China
关键词
raindrop size distribution (DSD); typhoons; eastern coast of China; 2D VIDEO DISDROMETER; RADAR PARAMETERS; MICROPHYSICS; SPECTRA; VARIABILITY; STRATIFORM; SEASON; EVENT; ERROR;
D O I
10.3390/atmos15080951
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study investigates the characteristics of the raindrop size distribution (DSD) for five typhoons that made landfall or passed by Zhejiang on the eastern coast of China, from 2019 to 2022. Additionally, it examines the raindrop shape-slope (mu-Lambda) relationship, as well as the local Z-R relationship for these typhoons. The DSD datasets were collected by the DSG1 disdrometer located in Ningbo, Zhejiang Province. Based on rainfall rate (R), the DSD can be categorized into convective and stratiform rainfall types. Some rainfall parameters can also be derived from the DSDs to further analyze the specific characteristics of rainfall. The histograms of the generalized intercept parameter (log10Nw) exhibit negative skewness in both convective and stratiform rainfall, whereas the histograms of the mass-weighted mean diameter (Dm) of raindrops display positive skewness. During typhoon periods on the eastern coast of China, the DSD characteristic was composed of a lower number concentration of small and midsize raindrops (3.42 for log10Nw, 1.43 mm for Dm in the whole dataset) as compared to Jiangsu in eastern China, Tokyo, in Japan, Miryang, in South Korea, and Thiruvananthapuram in south India, respectively. At the same time, the scatter plots of Dm and log10Nw indicate that the convective rain during typhoon periods exhibits characteristics that are intermediate between "maritime-like" and "continental-like" clusters. Additionally, the raindrop spectra of convective rainfall and midsize raindrops in stratiform rainfall are well-represented by a three-parameter gamma distribution. The mu-Lambda relation in this region is similar to Taiwan and Fujian, located along the southeastern coast of China. The Z-R relationship for eastern coastal China during typhoons based on filtered disdrometer data is Z = 175.04R1.53. These results could offer deeper insights into the microphysical characteristics of different rainfall types along the eastern coast of China and potentially improve the accuracy of precipitation estimates from weather radar observations.
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页数:17
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