Quasi-stationary extreme rain produced by mesoscale convective system on the Mei-Yu front-Reference-Cited by-同舟云学术

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Quasi-stationary extreme rain produced by mesoscale convective system on the Mei-Yu front

Published:2020-01-04 Issue:5 Volume:132 Page:721-742
ISSN:0177-7971
Container-title:Meteorology and Atmospheric Physics
language:en
Short-container-title:Meteorol Atmos Phys

Author:

Zhao Yuchun^ORCID,Liu Changhai,Wang Yehong,Moncrieff Mitchell W.

Funder

the National Natural Science Foundation of China

the Open Program of the State Key Laboratory of Severe Weather of the Chinese Academy of Meteorological Sciences

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science

Link

http://link.springer.com/content/pdf/10.1007/s00703-019-00717-1.pdf

Reference58 articles.

1. Akiyama T (1990) Large, synoptic and meso-scale variations of the Baiu front during July 1982. Part I: frontal structure and disturbances. J Meteorol Soc Japan 58:559–574. https://doi.org/10.2151/jmsj1965.68.6_705

2. Barthlott C, Kalthoff N (2011) A numerical sensitivity study on the impact of soil moisture on convection-related parameters and convective precipitation over complex terrain. J Atmos Sci 68(12):2971–2987. https://doi.org/10.1175/JAS-D-11-027.1

3. Benjamin TB (1968) Gravity currents and related phenomena. J Fluid Mech 31:209–248. https://doi.org/10.1017/S0022112068000133

4. Chaboureau JP, Guichard F, Redelsperger JL et al (2004) The role of stability and moisture in the diurnal cycle of convection over land. Q J R Meteorol Soc 130:3105–3117. https://doi.org/10.1256/qj.03.132

5. Chen TJG, Chang CP (1980) The structure and vorticity budget of an early summer monsoon trough (Mei-Yu) over southeastern China and Japan. Mon Weather Rev 108:942–953. https://doi.org/10.1175/1520-0493(1980)1082.0.CO;2

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