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Analysis of heavy precipitation caused by the vortices in the lee of the Tibetan Plateau from TRMM (the tropical rainfall measuring mission) observations

机译:从TRMM(热带雨量测量任务)观测分析青藏高原背风涡旋引起的强降水

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By using not only TRMM (the tropical rainfall measuring mission) precipitation radar (TRMM/PR) and microwave imager data, but also NCEP/NCAR reanalysis data, the paper compares and analyzes the two rainstorms caused by the southwest vortex (SWV) in Southwest China and eastward Tibetan Plateau vortex (TPV) formed over the Tibetan Plateau, respectively. It shows that the heavy rainfall systems of both two vortex rainstorms consist of a main rain band and several scattered precipitation clouds, with non-uniform distributed precipitation intensity. The horizontal scale of this main rain band and the intensive precipitation clouds of TPV on 21st July, 2008 are larger than those of SWV on 17th July, 2007. The common feature of the two mesoscale rainstorm systems detected by TRMM/PR is that most of precipitation are stratiform precipitation which has large scale but weak intensity caused by the two kinds of precipitation. However, the convective precipitation contributes more to the total precipitation, with larger rain rate than that of the stratiform precipitation. The rainfall intensity spectrum of the convective precipitation is wider than that of the stratiform precipitation, which ranges from 1 to 50 mm/h. It also indicates that the height of the rain top increases along with the surface precipitation intensity in the two rainstorms. The highest height of the rain top reaches 16km. The SWV rainstorm is more intensive than TPV rainstorm, and the microwave brightness temperature varies inversely as the height of the rain top. The release of the precipitation latent heat, the increase of the raindrops and the change of the ice particles mainly occur below 8km. Moreover, mid- and low-level precipitation are the main source of the column precipitation. The convective precipitation and the stratiform precipitation caused by SWV release much more latent heat than those caused by TPV.
机译:通过不仅使用TRMM(热带降水测量任务)降水雷达(TRMM / PR)和微波成像仪数据,还使用NCEP / NCAR再分析数据,对西南西南涡(SWV)引起的两次暴雨进行了比较和分析。中国和青藏高原东部分别形成了青藏高原涡。结果表明,两次涡旋暴雨的强降水系统均由主雨带和几条分散的降水云组成,降水强度分布不均匀。 2008年7月21日,该主雨带的水平尺度和TPV的强降水云大于2007年7月17日的SWV。TRMM/ PR检测到的两个中尺度暴雨系统的共同特征是,大部分降水是层状降水,由两种降水引起,规模较大,强度较弱。但是,对流降水对总降水的贡献更大,降雨率比层状降水大。对流降水的降雨强度谱比层状降水的降雨强度谱宽,范围为1至50 mm / h。这也表明在两次暴雨中,雨顶的高度随地表降水强度的增加而增加。雨顶的最高高度达到16公里。 SWV暴雨比TPV暴雨更为强烈,并且微波亮度温度与雨顶的高度成反比。降水潜热的释放,雨滴的增加和冰粒的变化主要发生在8km以下。此外,中低层降水是柱状降水的主要来源。与TPV相比,SWV引起的对流降水和层状降水释放的潜热要大得多。

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