2012
DOI: 10.1080/16742834.2012.11447016
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Study on the Dynamic Characteristics of an Eastward-offshore Mesoscale Vortex along the Meiyu-Baiu Front

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Cited by 5 publications
(2 citation statements)
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“…In the lower troposphere, many studies have examined the mesoscale structure of the Meiyu front [18]. These studies have generally presented the Meiyu front as a quasi-stationary boundary defined by a wind shear line at 850 hPa that is associated with a robust gradient in 700 hPa equivalent potential temperatures.…”
Section: Introductionmentioning
confidence: 99%
“…In the lower troposphere, many studies have examined the mesoscale structure of the Meiyu front [18]. These studies have generally presented the Meiyu front as a quasi-stationary boundary defined by a wind shear line at 850 hPa that is associated with a robust gradient in 700 hPa equivalent potential temperatures.…”
Section: Introductionmentioning
confidence: 99%
“…The relatively stable quasi-stationary front makes the Meiyu precipitation to exhibit continuous characteristics, often accompanied by heavy rainfall and floods. Meiyu is an important part of the East Asian monsoon system (e.g., Huang et al, 2011;Yu et al, 2015;Zheng et al, 2013) and the rainfall during the Meiyu period accounts for about 45% of the total summer rainfall (e.g., Ding & Chan, 2005). The amount of the Meiyu precipitation directly affects the flood and drought conditions in the Jianghuai Basin and influences the economic and social production of the region (e.g., Ding et al, 2020).A large portion of Meiyu rain belt is located over the ocean, limiting its direct observation.…”
mentioning
confidence: 99%