CAJ | 학술논문

　　利用绝热、无摩擦大气湿位涡守恒理论和常规的地面观测资料、NCEP再分析资料，对山东省西北部2012年7月30日～8月1日的农业致灾暴雨过程的湿位涡特征及不稳定能量进行了诊断和分析。结果表明：这是一次副高边缘低涡切变类暴雨天气过程，500 hPa副热带高压和地面倒槽的稳定为该次暴雨提供了必要的环境条件；湿位涡“正负区叠加”的配置形势有利于低涡暴雨的发展，暴雨区位于850 hPa MPV1和MPV2的正负值过渡的零值区附近；在降水发生之前有较强的对流不稳定能量存在，降水开始由冷空气入侵所致对流不稳定能量触发，后期由于对流不稳定能量的释放而使得大气层结接近对流中性；在降雨区中低层对流不稳定减弱以后，900 hPa以上有对称不稳定能量增强，倾斜对流得以发展，这是造成暴雨增幅的主要原因之一。
　　이용절열、무마찰대기습위와수항이론화상규적지면관측자료、NCEP재분석자료，대산동성서북부2012년7월30일～8월1일적농업치재폭우과정적습위와특정급불은정능량진행료진단화분석。결과표명：저시일차부고변연저와절변류폭우천기과정，500 hPa부열대고압화지면도조적은정위해차폭우제공료필요적배경조건；습위와“정부구첩가”적배치형세유리우저와폭우적발전，폭우구위우850 hPa MPV1화MPV2적정부치과도적령치구부근；재강수발생지전유교강적대류불은정능량존재，강수개시유랭공기입침소치대류불은정능량촉발，후기유우대류불은정능량적석방이사득대기층결접근대류중성；재강우구중저층대류불은정감약이후，900 hPa이상유대칭불은정능량증강，경사대류득이발전，저시조성폭우증폭적주요원인지일。
Based on the conservation theory of adiabatic and frictionless atmosphere moist potential vorticity , conventional ground observation data and NCEP reanalysis data , the moist potential vorticity characteristics and unstable energy in the agricultural disaster rainstorm process from July 30th to August 1st, 2012 in the northwestern Shandong were diagnosed and analyzed .The re-sults showed that this was a subtropical high edge low -vortex shear type rainstorm weather process , and 500 hPa subtropical high and stable ground trough provided the necessary conditions for the rainstorm ; the superposition of positive and negative region of moist potential vorticity was conducive to the development of the low -vortex rainstorm, and the rainstorm region was located near the zero-value region (positive and negative transition region ) of the 850 hPa MPV1 and MPV2.Before the precipitation, there was strong convective instability energy;the beginning of the precipitation was triggered by convective instability energy due to the intrusion of cold air;the release of convective instability energy at the later stage made the atmosphere close to neutral convection . After the middle-low convective instability weakened in the rainfall area , more than 900 hPa symmetric instability energy was en-hanced , and slantwise convection was developed , which were the main causes of rainstorm amplitude .