单 位：
广西百色市气象局;广西区气象台;南京信息工程大学气象灾害教育部重点实验室/气候与环境变化国际合作联合实验室/气象灾害预报预警与评估协同创新中心/气候模拟与预测科技创新团队
摘 要：
为分析2012年1月13—15日广西暴雨过程的水汽来源、急流的输送作用和水汽饱和程度等特征,使用天气学分析和动力诊断的方法分析NCEP/NCAR 1°×1°再分析资料、红外云图等资料。结果表明:孟加拉湾和南海是本次暴雨过程的2个水汽源地,500~700 h Pa中低空西南急流的建立和加强使孟加拉湾成为主要水源地,加强了暴雨区的水汽供应。而这支急流的维持依赖于200 h Pa加强的副热带锋区西风急流入口区南侧的强辐散作用。不同源地的水汽输送高度不同,水汽通量中心出现在700 h Pa。600 h Pa以下为水汽通量辐合层,700~850 h Pa辐合强度远大于925~1000 h Pa;水汽通量中心在暴雨区的上风方,水汽辐合中心在水汽通量中心沿气流去向的一侧,700~850 h Pa叠加的辐合中心处即为暴雨区,辐合高度的升高、湿层剧烈向上扩展都可作为暴雨征兆。以上分析得出了冬季暴雨过程中水汽条件的形成机制,得出预报着眼点,对提高此类暴雨预报准确率有较大作用。
译 名：
Water Vapor Characteristics of a Winter Rainstorm in Guangxi
作 者：
Deng Ruyi;Wang Lijuan;Liu Guozhong;Key Laboratory of Meteorological Disaster,Ministry of Education(KLME),Joint International Research Laboratory of Climate and Environment Change(ILCEC),Collaborative Innovation Center on Forecast and Evaluation of Meterological Disasters(CIC-FEMD),Science and Technology Innovation Team on Climate Simulation and Forecast,Nanjing University of Information Science & Technology;Baise Meteorological Bureau;Guangxi Meteorological Observatory;
关键词：
winter rainstorm;;water vapor;;jet stream;;integrated vapor flux
摘 要：
The paper aims to analyze the characteristics of water vapor source, vapor transport by jet streamand water vapor saturation of a winter rainstorm occurred from January13 to15 of 2012 in Guangxi, the authorsused weather analysis and dynamic diagnostic methods to analyze the NCEP/NCAR 1°× 1° reanalysis data,infrared imagery and other information. The results showed that: Bay of Bengal and the South China Sea werethe two vapor sources of this rainstorm process, the establishment of low-level southwest jet stream at 500-700 h Pa made the Bay of Bengal be the main source, strengthened the water vapor supply to the rainstorm area.The jet stream mainly depended on strong divergence effect of south side of west jet stream entrance ofstrengthening sub- tropical frontal area at 200 h Pa. Different sources of water vapor transport had different heights, water vapor flux center appeared at 700 h Pa. The vapor flux convergence layer was below 600 h Pa,convergence at 700- 850 h Pa was much larger than that at 925- 1000 h Pa; the overlapping vapor fluxconvergence center at 700 h Pa and 850 h Pa was the rainstorm area, the increased height of convergence andthe wet layer'severe scaling up could be the signal of the rainstorm. The conclusion contained the formationmechanism of water vapor conditions of a winter rainstorm, obtained prediction focus, and had a great effect onimproving the accuracy of winter rainstorm's forecast.
