FY-4A Measurement of Cloud-Seeding Effect and Validation of a Catalyst T&D Algorithm

被引:0
作者
Yan, Liangrui [1 ]
Zhou, Yuquan [2 ]
Wu, Yixuan [3 ]
Cai, Miao [2 ]
Peng, Chong [4 ]
Song, Can [4 ]
Liu, Shuoyin [5 ]
Liu, Yubao [3 ]
机构
[1] Chengdu Univ Informat Technol, Sch Elect Engn, Chengdu 610225, Peoples R China
[2] Artificial Weather Ctr, China Meteorol Adm, Beijing 100081, Peoples R China
[3] Nanjing Univ Informat Sci & Technol, Sch Atmospher Phys, Nanjing 210044, Peoples R China
[4] Weather Modificat Ctr Henan Prov, Zhengzhou 450000, Peoples R China
[5] Beijing ChenJing Technol Co Ltd, Beijing 100081, Peoples R China
关键词
aircraft cloud seeding; cloud track; airborne catalyst T&D; FY-4A cloud measurements; SATELLITE;
D O I
10.3390/atmos15050556
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The transport and dispersion (T&D) of catalyst particles seeded by weather modification aircraft is crucial for assessing their weather modification effects. This study investigates the capabilities of the Chinese geostationary weather satellite FY-4A for identifying the physical response of cloud seeding with AgI-based catalysts and continuously monitoring its evolution for a weather event that occurred on 15 December 2019 in Henan Province, China. Satellite measurements are also used to verify an operational catalyst T&D algorithm. The results show that FY-4A exhibits a remarkable capability of identifying the cloud-seeding tracks and continuously tracing their evolution for a period of over 3 h. About 60 min after the cloud seeding, the cloud crystallization track became clear in the FY-4A tri-channel composite cloud image and lasted for about 218 min. During this time period, the cloud track moved with the cloud system about 153 km downstream (northeast of the operation area). An operational catalyst T&D model was run to simulate the cloud track, and the outputs were extensively compared with the satellite observations. It was found that the forecast cloud track closely agreed with the satellite observations in terms of the track widths, morphology, and movement. Finally, the FY-4A measurements show that there were significant differences in the microphysical properties across the cloud track. The effective cloud radius inside the cloud track was up to 15 mu m larger than that of the surrounding clouds; the cloud optical thickness was about 30 mu m smaller; and the cloud-top heights inside the cloud track were up to 1 km lower. These features indicate that the cloud-seeding catalysts led to the development of ice-phase processes within the supercooled cloud, with the formation of large ice particles and some precipitation sedimentation.
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页数:15
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