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    Please use this identifier to cite or link to this item: https://ir.lib.ncu.edu.tw/handle/987654321/100447


    Title: The kinematic and microphysical characteristics and associated precipitation efficiency of subtropical convection during SoWMEX/TiMREX
    Authors: 廖宇慶;Chang, Wei-Yu;Lee, Wen-Chau;Liou, Yu-Chieng
    Contributors: 地球科學學院大氣科學學系
    Keywords: Climate change;Clouds;Computational efficiency;Computing time;Convection;Convective precipitation;Freezing;Meteorology;Monsoons;Precipitation;Rain;Rainfall;Studies;Tropical environments;Water;Water content;Wind;Wind shear
    Date: 2015-01-01
    Issue Date: 2026-04-21 14:03:00 (UTC+8)
    Publisher: American Meteorological Society;Washington: American Meteorological Society
    Abstract: 摘要: AbstractDual-Doppler, polarimetric radar observations and precipitation efficiency (PE) calculations are used to analyze subtropical heavy rainfall events that occurred in southern Taiwan from 14 to 17 June 2008 during the Southwest Monsoon Experiment/Terrain-Influenced Monsoon Rainfall Experiment (SoWMEX/TiMREX) field campaign. Two different periods of distinct precipitation systems with diverse kinematic and microphysical characteristics were investigated: 1) prefrontal squall line (PFSL) and 2) southwesterly monsoon mesoscale convective system (SWMCS). The PFSL was accompanied by a low-level front-to-rear inflow and pronounced vertical wind shear. In contrast, the SWMCS had a low-level southwesterly rear-to-front flow with a uniform vertical wind field. The PFSL (SWMCS) contained high (low) lightning frequency associated with strong (moderate) updrafts and intense graupel–rain/graupel–small hail mixing (more snow and less graupel water content) above the freezing level. It is postulated that the reduced vertical wind shear and enhanced accretional growth of rain by high liquid water content at low levels in the SWMCS helped produce rainfall more efficiently (53.1%). On the contrary, the deeper convection of the PFSL had lower PE (45.0%) associated with the evaporative loss of rain and the upstream transport of liquid water to form larger stratiform regions. By studying these two events, the dependence of PE on the environmental and microphysical factors of subtropical heavy precipitation systems are investigated by observational data for the first time. Overall, the PE of the convective precipitation region (47.9%) from 14 to 17 June is similar to past studies of convective precipitation in tropical regions.
    出版者: Washington: American Meteorological Society
    出版日期: 2015-01-01
    出處: Monthly Weather Review, 2015-01, Vol.143 (1), p.317-340
    資源來源: EBSCOhost OmniFile Full Text Select
    版權: Copyright American Meteorological Society Jan 2015
    識別號: ISSN: 0027-0644
    識別號: EISSN: 1520-0493
    識別號: DOI: 10.1175/mwr-d-14-00081.1
    識別號: CODEN: MWREAB
    Appears in Collections:[Department of Atmospheric Sciences] journal & Dissertation

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