人民长江 ›› 2023, Vol. 54 ›› Issue (9): 91-98.doi: 10.16232/j.cnki.1001-4179.2023.09.012

• • 上一篇    

汉江流域盛夏期极端降水特征及大气环流分型研究

谢家旭 郭广芬 杜良敏 向华 宋娜   

  • 收稿日期:2022-10-25 出版日期:2023-09-28 发布日期:2023-10-16

Characteristics of extreme precipitation and classification of atmospheric circulation in mid-summer in Hanjiang River Basin

XIE Jiaxu GUO Guangfen DU Liangming XIANG Hua SONG Na   

  • Received:2022-10-25 Online:2023-09-28 Published:2023-10-16

摘要: 为提升汉江流域盛夏期极端降水预报准确性,基于1970~2020年7~8月汉江流域日降水量数据集,采用95%分位法定义汉江流域盛夏期极端降水事件,并对汉江流域盛夏期极端降水事件气候特征进行分析,研究汉江流域极端降水发生时的大气环流和海温背景,最后采用Lamb-Jenkinson分型法分析区域性极端降水事件与大气环流分型的关系。结果表明:(1)汉江流域盛夏期极端降水存在显著年际变化特征,且极端降水分布与盛夏期总降水气候平均态分布一致,呈现“边缘大,中部小”趋势,极值中心出现在流域西南部镇巴。(2)中高纬度“两脊一槽”以及副高位置偏北偏西的构架是汉江流域极端降水多发典型环流场,来自海上水汽补充配合贯穿整层的上升运动为极端降水的产生提供条件。此外,中东太平洋和西太平洋暖池两个海温关键区海温异常时,其外强迫的叠加作用致使汉江流域极端降水发生的典型大尺度环流稳定维持且强度增强。(3) L-J环流分型表明,汉江流域区域极端降水天气常见环流型有南风(S)型、东南风(SE)型、气旋(C)型、气旋配合西南风(CSW)型、气旋配合南风(CS)型,其中气旋(C)型出现概率超过55%,不同分型区别在于500 hPa高空槽、副高位置和850 hPa上西南涡和南风影响。对比2021年8月22日和29日汉江流域区域极端降水事件实况,发现分别符合500 hPa高度场上C型、850 hPa的CS型配置以及500 hPa高度场上的CS型、850 hPa上S型配置。研究成果可为汉江流域盛夏期极端降水预报和天气分型提供参考。

关键词: 大气科学;极端降水;气候特征;环流分型;合成分析;

Abstract: To improve the forecasting accuracy of extreme precipitation events in Hanjiang River Basin during the mid-summer, based on its daily precipitation data from 1970 to 2020,the extreme precipitation events in mid-summer in Hanjiang River Basin were defined by 95% fractional method, including climate characteristics, atmospheric circulation and sea surface temperature background.The atmospheric circulation of regional extreme precipitation events were divided into five main types by L-J method.The results show that:(1) The extreme precipitation in the mid-summer of the Hanjiang River basin has significant inter-annual variation characteristics, and the distribution of the extreme precipitation threshold is similar to the climate state over the region, which is “large at the edge, small in the middle”,and the extreme center is at Zhenba Town in the southwest of the basin.(2) The typical circulation field of extreme precipitation is Baikal trough, Ural Mountanins high, Okhotsk blocking high and the strong West Pacific subtropical high.The water vapor replenishment from the sea combined with upward movement throughout the entire layer provides the conditions for extreme precipitation.In addition, the superposition of the external forcing of the SST anomalies in the two key areas(the Eastern Central Pacific and the western Pacific warm pool)result in the stable maintenance and enhanced intensity of the atmospheric circulation.(3) The regional extreme precipitation are dominated by S type, SE type, C type, CSW type and CS type.By comparing the circulation of regional extreme precipitation events in the Hanjiang River Basin on August 22 and 29 in 2021,it was found that the circulation conforms to the C type on 500hPa and the CS type on 850hPa, the CS type on 500hPa and the S type on 850hPa, which can be offered as an subjective approach to classification and prediction of extreme precipitation events in mid-summer in Hanjiang River Basin in the future.

Key words: atmospheric science; extreme precipitation; climatic characteristics; circulation classification; synthetic analysis;