Initiation and Evolution of Elevated Convection in a Nocturnal Squall Line Along the Meiyu Front

Author:

He Zhiwei1ORCID,Zhang Qinghong1ORCID,Zhao Kun2ORCID,Hu Huiqin3

Affiliation:

1. Department of Atmospheric and Oceanic Sciences, School of Physics; Peking University; Beijing China

2. Key Laboratory for Mesoscale Severe Weather/MOE and School of Atmospheric Science; Nanjing University; Nanjing China

3. College of Oceanic and Atmospheric Sciences; Ocean University of China; Qingdao China

Funder

Ministry of Science and Technology of the People's Republic of China

Chinese National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Reference45 articles.

1. Observations of dual slantwise circulations above a cool undercurrent in a mesoscale convective system;Browning;Quarterly Journal of the Royal Meteorological Society,2010

2. Assimilating surface observations in a four-dimensional variational Doppler radar data assimilation system to improve the analysis and forecast of a squall line case;Chen;Advances in Atmospheric Sciences,2016

3. Relationship between abnormal activities of southwest vortex and heavy rain the upper reach of Yangtze River during summer of 1998;Chen;Plateau Meteorology,2003

4. Thunderstorms above frontal surfaces in environments without positive CAPE. Part I: A climatology;Colman;Monthly Weather Review,1990a

5. Thunderstorms above frontal surfaces in environments without positive CAPE. Part II: Organization and instability mechanisms;Colman;Monthly Weather Review,1990b

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