周涛, 李娜, 许敏, 王清川, 张湘涵. 基于多源资料的一次暖区暴雨水汽特征分析[J]. 沙漠与绿洲气象, 2022, 16(5): 62-69.
引用本文: 周涛, 李娜, 许敏, 王清川, 张湘涵. 基于多源资料的一次暖区暴雨水汽特征分析[J]. 沙漠与绿洲气象, 2022, 16(5): 62-69.
ZHOU Tao, LI Na, XU Min, WANG Qingchuan, ZHANG Xianghan. Water Vapor Characteristics of a Rainstorm in Warm Region Based on Multisource Data[J]. Desert and Oasis Meteorology, 2022, 16(5): 62-69.
Citation: ZHOU Tao, LI Na, XU Min, WANG Qingchuan, ZHANG Xianghan. Water Vapor Characteristics of a Rainstorm in Warm Region Based on Multisource Data[J]. Desert and Oasis Meteorology, 2022, 16(5): 62-69.

基于多源资料的一次暖区暴雨水汽特征分析

Water Vapor Characteristics of a Rainstorm in Warm Region Based on Multisource Data

  • 摘要: 利用常规气象观测资料、NCEP逐6 h再分析资料(1°×1°)、微波辐射计资料以及HYSPLIT模式等,对2021年7月5日冀中平原一次暖区暴雨过程的水汽输送特征进行对比分析。结果表明:应用HYSPLIT模式模拟分析后发现,本次过程中925和850 hPa降水开始前比湿在12 g/kg以上,是暴雨区的主要水汽贡献者,其主要水汽通道为西南路径,水汽贡献率分别占57.57%和63.64%。源自黄海或途径黄海、渤海等地的气块在东南转西南气流的引导下为暴雨区低层带来丰富的水汽,同时源自亚欧大陆中高层的气块,随着西风带长波槽脊的运动,为暴雨区上空500 hPa带来干空气,构成上干下湿的不稳定层结。降水开始前,925和850 hPa在相应引导气流的作用下,水汽不断向冀中平原输送,使得优良的水汽条件主要集中于低层大气,与HYSPLIT模式模拟结果一致。通过微波辐射计对降雨过程的水汽特征进行分析,结果表明在降雨开始前,700 hPa以下高度的水汽含量有明显增加,水汽密度最大达到14 g/m3。分析3种不同资料得到相似结论,但HYSPLIT模式和微波辐射计两种高时空分辨率资料的应用,可以及时且多方位分析水汽特征,为暖区暴雨落区、强度等精细化准确预报预警提供一定参考。

     

    Abstract: Based on the conventional meteorological observation data,NCEP reanalysis data(1°×1°),microwave radiometer data and the HYSPLIT model,the characteristics of water vapor transport during a heavy rain in the warm zone of Jizhong Plain on July 5,2021 was comparatively analyzed.The results showed that before the onset of precipitation in this process,the specific humidity of 925 hPa and 850 hPa were above 12 g/kg by applying the analysis of the HYSPLIT model simulation,which were the main water vapor contributors in the rainstorm area,and the main water vapor channels were the southwest route,the contribution rate of water vapor accounted for 57.57% and 63.64% respectively.Under the guidance of the southeast turning southwest airflow,the air masses which were originated from the Yellow Sea or passed through the Yellow Sea,Bohai Sea,etc.,brought abundant water vapor to the lower layers of the rainstorm area.At the same time,the air masses originating from the middle and high levels of the Eurasian continent,brought dry air to 500 hPa over the rainstorm area,which constituted an unstable stratification of upper dry and lower wet along with the movement of the longwave troughs and ridges in the westerly zone.Before the start of precipitation,under the action of the corresponding guiding airflow at 925 hPa and850 hPa,water vapor were continuously transported to the central Jizhong Plain,so that the excellent water vapor conditions were mainly concentrated in the lower atmosphere,which was consistent with the simulation results of the HYSPLIT model.The water vapor characteristics which were analyzed by microwave radiometer,showed that the water vapor content at altitudes below 700 hPa increased significantly before the rainfall started,and the maximum water vapor density reached 14 g/m~3.Three different data were analyzed to get similar conclusions,but the application of the two high-temporal-spatial-resolution data of the HYSPLIT mode and microwave radiometer can analyze the water vapor characteristics in a more timely and detailed manner,and provide accurate forecast and early warning of the rainstorm falling area and intensity in warm regions.

     

/

返回文章
返回