暴雨灾害
暴雨災害
폭우재해
TORRENTIAL RAIN AND DISASTERS
2012年
3期
210-217
,共8页
隋兴斌%李昀英%周毅%严仕尧
隋興斌%李昀英%週毅%嚴仕堯
수흥빈%리윤영%주의%엄사요
扰动位涡倾向方程%尺度分离%中尺度低压%凝结加热
擾動位渦傾嚮方程%呎度分離%中呎度低壓%凝結加熱
우동위와경향방정%척도분리%중척도저압%응결가열
PVDTE%scale separation%mesoscale low%condensation heat
为研究暴雨过程中尺度低压系统的演变,推导出非守恒条件下的位涡方程并简化得出中尺度扰动位涡倾向方程,以广西一次特大暴雨过程为例,验证方程在分析中尺度系统发展演变中的有效性和可操作性,并分析了暴雨过程中两类中低压的不同演变因子。结果表明:(1)中尺度扰动位涡大值中心的演变对中尺度低压系统的发展演变具有较好的指示意义;(2)推导出的包含非绝热加热作用项的中尺度扰动位涡倾向方程,可用来揭示凝结加热潜热对中尺度低压系统发展演变的作用;(3)利用中尺度扰动位涡倾向方程定量分析凝结加热的贡献,是区分引发降水的中尺度系统和降水过程中凝结加热强迫出的中尺度系统的方法,对研究凝结加热和不同类型中尺度系统之间的相互作用具有重要意义。
為研究暴雨過程中呎度低壓繫統的縯變,推導齣非守恆條件下的位渦方程併簡化得齣中呎度擾動位渦傾嚮方程,以廣西一次特大暴雨過程為例,驗證方程在分析中呎度繫統髮展縯變中的有效性和可操作性,併分析瞭暴雨過程中兩類中低壓的不同縯變因子。結果錶明:(1)中呎度擾動位渦大值中心的縯變對中呎度低壓繫統的髮展縯變具有較好的指示意義;(2)推導齣的包含非絕熱加熱作用項的中呎度擾動位渦傾嚮方程,可用來揭示凝結加熱潛熱對中呎度低壓繫統髮展縯變的作用;(3)利用中呎度擾動位渦傾嚮方程定量分析凝結加熱的貢獻,是區分引髮降水的中呎度繫統和降水過程中凝結加熱彊迫齣的中呎度繫統的方法,對研究凝結加熱和不同類型中呎度繫統之間的相互作用具有重要意義。
위연구폭우과정중척도저압계통적연변,추도출비수항조건하적위와방정병간화득출중척도우동위와경향방정,이엄서일차특대폭우과정위례,험증방정재분석중척도계통발전연변중적유효성화가조작성,병분석료폭우과정중량류중저압적불동연변인자。결과표명:(1)중척도우동위와대치중심적연변대중척도저압계통적발전연변구유교호적지시의의;(2)추도출적포함비절열가열작용항적중척도우동위와경향방정,가용래게시응결가열잠열대중척도저압계통발전연변적작용;(3)이용중척도우동위와경향방정정량분석응결가열적공헌,시구분인발강수적중척도계통화강수과정중응결가열강박출적중척도계통적방법,대연구응결가열화불동류형중척도계통지간적상호작용구유중요의의。
Potential Vorticity Equation (PVE) is derived and simplified to get mesoscale Potential Vorticity Disturbance Tendency Equation (PVDTE) in order to investigate the evolution of mesoscale lows associated with torrential rain. The availability and operability of PVDTE to analyze the evolution of mesoscale lows is verified and the different evolution factors are analyzed with the torrential rain case in Guangxi province. The result shows the following. (1) The evolution of the high-value center of mesoscale disturbance potential vorticity can directly indicate the development and evolution of mesoscale lows. (2) The derived PVDTE containing the diabafic heating action term could be used to reveal the effect of latent heat of condensation heating on the evolution of mesoscale lows. (3) The quantitative analysis of the contribution of condensation heating by PVDTE is an effective method to differentiate the mesoscale lows causing precipitation from the mesoscale lows pro- duced forcibly by condensation heating during the precipitation. The equation has a great significance to research the interaction between con- densation heating and different types of mesoseale lows.