热带气旋“桑美(2006)”冰云微物理属性垂直分布规律*

doi:10.11978/2013119

Abstract

Abstract: Using the retrieved data from CloudSat during August 3-11, 2006, the vertical distributions of ice particles in the clouds of different parts of tropical cyclone (TC) Saomai (2006) were analyzed, in their formation period, development-to- mature period and weakening period. The results are as follows. When the space-borne radar swept through different parts of TC Saomai (2006), ice particles in the clouds mainly distributed from the height of 5 to 16.5 km. The ice particle effective radius (r_e) reduced with increasing altitude and the large particles were mainly concentrated at the bottom of the ice clouds. The ice particle number concentration (C_in) increased with increasing altitude and large particles were mainly at the top of the ice clouds; the vertical distribution of the ice water content (C_iw) had a shape of unimodal or bimodal. The heights of the maximum r_e, C_in and C_iw were different from each other, and the ranges of the maximum what for r_e, C_in and C_iw were 107.9~177.7 μm, 123.8~827.9 L^-1 and 211~2858 mg•m^-3, respectively.

Key words: CloudSat, tropical cyclone, microphysical properties of cloud, vertical distribution

CLC Number:

P732.33

ZHANG Lei, SHI Lanhong, XU Jian, SUN Ran, ZHAO Bingke, CHEN Yonghang, WANG Xiaofeng, WANG Wencai, Li Meng, DING Mingyue. Vertical distribution of ice cloud microphysical properties of tropical cyclone Saomai (2006)^*[J].Journal of Tropical Oceanography, 2016, 35(3): 30-40.

References

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Vertical distribution of ice cloud microphysical properties of tropical cyclone Saomai (2006)^*

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Vertical distribution of ice cloud microphysical properties of tropical cyclone Saomai (2006)*

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Vertical distribution of ice cloud microphysical properties of tropical cyclone Saomai (2006)^*