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机构地区:[1]空军航空气象研究所,北京100085 [2]中国科学院大气物理研究所,北京100029
出 处:《大气科学》2004年第6期876-891,共16页Chinese Journal of Atmospheric Sciences
基 金:国家重点基础研究发展项目G1 9980 40 90 7;国家自然科学基金资助项目 4973 5 1 80共同资助
摘 要:利用再分析资料及加密观测资料 ,对 1 999年 6月下旬有利大尺度环境条件下长江中下游地区梅雨锋上频发的 5个中尺度低压 (扰动 )进行了诊断研究。由合成分析得到了长江中下游地区中尺度低压 (扰动 )的基本特征 (共性 ) ;依其特征将之归纳为两种类型 ;之后选择两个典型个例分析了它们各自发生发展过程中特征的异同 (个性 )。分析结果揭示了梅雨锋中尺度低压 (扰动 )的动力和热力结构特征、暴雨过程中对流活动的详细过程及典型雨团的路径和生命史。此外 ,高山站每小时的风记录等信息反映出低空西南急流和其上大风速中心同中尺度低压 (扰动 )及暴雨发生演变过程有密切关系。高空急流对中尺度低压 (扰动 )的发展及暴雨有明显的作用 ,有无高空西风急流与低空急流的耦合似乎是未来发展与不发展中尺度低压 (扰动 )之间重要的动力学区别之一。By utilizing reanalysis and intensive observation data, characteristics of mesoscale lows (disturbances) are studied, which occurred on Meiyu front over the middle and lower reaches of the Yangtze River during the last ten-day of June in 1999. It is confirmed that there existed at least five mesoscale lows (disturbances), which were the direct makers of heavy rainfall, occurring during that period. They could be divided into two groups according to their characteristics. The common characteristics of mesoscale lows (disturbances) over the middle and lower reaches of the Yangtze River are obtained by means of compositive analysis. Then two typical cases are selected and analyzed. The dynamical and thermodynamical structures of mesoscale lows (disturbances) are investigated. The detailed evolution of convection, track and lifecycle of typical convection are also revealed. In addition, wind data of Huangshan station and other information show that southwest low-level jet and wind streak on it are related closely with the process of mesoscale lows (disturbances) and associated heavy rainfall. The coupling between the westerly upper-level jet and the southwest low-level jet seems to be one of main dynamical factors that cause the evident development of mesoscale low (disturbance).
关 键 词:中尺度 梅雨锋暴雨 暴雨过程 高空急流 个例分析 雨团 对流活动 诊断研究 长江中下游地区 环境条件
分 类 号:P458[天文地球—大气科学及气象学] P456.7
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