Citation: | Yang Cheng, Fu Zhijia, Peng Juan, et al. xxxx. Analysis of characteristics of an extreme precipitation event in Cangshan-Erhai Lake region [J]. Torrential Rain and Disasters,44(x):xx-xx. DOI: 10.12406/byzh.2024-156 |
In order to deeply understood the characteristics of extreme precipitation in Cangshan-Erhai Lake region, the precipitation observation data from 46 meteorological observation stations, relative humidity and water vapor pressure of the ground near, doppler weather radar, boundary layer wind profile radar in Dali station and ERA5 reanalysis data were used to analyzed the impact system and fine grained characteristics of an extreme precipitation event on September 18, 2020 in this region by statistical and classification methods. The results are as follows. This precipitation process was a significant regional rainfall event (RRE). Under the influence of the convergence shear line , the mesoscale convective system near the shear line directly triggered the heavy precipitation. There were sufficient convective triggering conditions in the boundary layer, and the favorable system configuration enabled multiple small-scale convective systems to be generated during this process, resulting in heavy rainfall above heavy rain in 30.5% of the stations in the region. The maximum accumulated precipitation in 19 h was 123.9 mm, and the maximum rainfall intensity was 33.6 mm·h−1. Dued to the differences in the origin, moving path and intensity of the convective system, the spatio-temporal distribution of the precipitation was uneven and the scale was small. The strong precipitation was mainly concentrated in the east of Cangshan Mountain, while the precipitation in other regions was relatively small. The convective system developed in the northern part of Erhai Lake has fast moving speed, strong echo of radar and relatively small influence range. The strong convection generated on the west side of Erhai Lake in the middle of Cangshan Mountain has a long duration and large influence range. The peak precipitation intensity appeared earlier in the northern part of Erhai Lake than in the southern part of Erhai Lake. The precipitation intensity in the south of Erhai Lake fell slowly after reaching the peak, while the peak precipitation intensity in other regions decreased rapidly after appearing.
陈权亮,刘皓,胡淼,等.2024.青藏高原东侧复杂地形区极端降水研究进展[J].暴雨灾害,43(3):255−265. doi: 10.12406/byzh.2023-216
Chen Q L, Liu H, Hu M, et al. 2024. A review of the studies on extreme precipitation in the complex terrain region on the eastern side of the Tibetan plateau [J]. Torrential Rain and Disasters,43(3):255−265 (in Chinese). doi:10.12406/byzh.2023−216
|
丁仁海,周后福.2010.九华山区下垫面对局地降水的影响分析[J].气象,36(3):47−53. doi: 10.7519/j.issn.1000-0526.2010.3.007
Ding R H, Zhou H F. 2010. Influences of underlying surface on local precipitation in Jiuhua mountains [J]. Meteorological Monthly,36(3):47−53 (in Chinese). doi:10.7519/j.issn.1000−0526.2010.3.007
|
董保举,付志嘉,李明,等.2012.风廓线雷达资料在暴雨天气过程特征分析中的应用[J].气象科技,40(1):74−78,86. doi: 10.19517/j.1671-6345.2012.01.015
Dong B J,Fu Z J,Li M,et al. 2012. Feature analysis of a rain storm with wind profile radar data [J]. Meteorological Science and Technology,40(1):74−78 (in Chinese). doi:10.19517/j.1671−6345.2012.01.015
|
董保举,徐安伦,苏锦兰.2023.大理苍山不同海拔高度湿季降水日变化特征分析[J].气象,49(11):1405−1413. doi: 10.7519/j.issn.1000-0526.2023.060402
Dong B J, Xu A L, Su J L. 2023. Diurnal variation of wet season precipitation at different altitudes of Cangshan mountain in Dali [J]. Meteorological Monthly,49(11):1405−1413 (in Chinese). doi:10.7519/j.issn.1000−0526.2023.060402
|
董保举,张成稳,付志嘉,等.2011.云南大理边界层风垂直变化观测研究[J].干旱气象,29(2):189−194. doi: 10.3969/j.issn.1006-7639.2011.02.010
Dong B J, Zhang C W, Fu Z J, et al. 2011. Study on the vertical change of wind in boundary layer in Dali of Yunnan province [J]. Journal of Arid Meteorology,29(2):189−194 (in Chinese). doi:10.3969/j.issn.1006−7639.2011.02.010
|
何华,孙绩华.2003.云南冷锋切变大暴雨过程的环流及水汽输送特征[J].气象,29(4):48−52. doi: 10.7519/j.issn.1000-0526.2003.4.011
He H,Sun J H. 2003. Circulation and moisture flux characteristics at middle and lower levels during heavy rains in Yunnan [J]. Meteorological Monthly,29(4):48−52 (in Chinese). doi:10.7519/j.issn.1000−0526.2003.4.011
|
卢珊,胡泽勇,付春伟,等.2022.黄土高原夏季极端降水及其成因分析[J].高原气象,41(1):241−254. doi: 10.7522/j.issn.1000-0534.2021.00027
Lu S, Hu Z Y, Fu C W, et al. 2022. Characteristics and possible causes for extreme precipitation in summer over the Loess plateau [J]. Plateau Meteorology,41(1):241−254 (in Chinese). doi:10.7522/j.issn.1000−0534.2021.00027
|
鲁亚斌,李华宏,闵颖,等.2018.一次云南强对流暴雨的中尺度特征分析[J].气象,44(5):645−654. doi: 10.7519/j.issn.1000-0526.2018.05.005
Lu Y B, Li H H, Min Y, et al. 2018. Analysis of mesoscale weather system characteristics of a severe convective rainstorm in Yunnan [J]. Meteorological Monthly,44(5):645−654 (in Chinese). doi:10.7519/j.issn.1000−0526.2018.05.005
|
沈晓琳,周宁芳,杨舒楠,等.2019.2015年冬季云南两次极端降水事件及环流异常特征分析[J].暴雨灾害,38(4):380−385. doi: 10.3969/i.issn.1004-9045.2019.04.011
Shen X L, Zhou N F, Yang S N, et al. 2019. Analysis of two extreme precipitation events and circulation anomalies in Yunnan province in winter of 2015 [J]. Torrential Rain and Disasters,38(4):380−385 (in Chinese). doi:10.3969/i.issn.1004−9045.2019.04.011
|
宋薇,邱晓滨,王兆宇,等.2024.一次冰雹过程的多源资料观测特征分析[J].暴雨灾害,43(3):322−331. doi: 10.12406/byzh.2023-032
Song W, Qiu X B, Wang Z Y, et al. 2024. Analysis of the characteristics of a hail event with multi-source data [J]. Torrential Rain and Disasters,43(3):322−331 (in Chinese). doi:10.12406/byzh.2023−032
|
苏锦兰,李建,杨桂荣,等.2015.横断山系云岭余脉点苍山东西侧小时降水特性对比分析[J].气象,41(1):17−24. doi: 10.7519/j.issn.1000-0526.2015.01.002
Su J L, Li J, Yang G R, et al. 2015. Comparative analysis on hourly precipitation features on the east and west sides of Yunling Diancang mountain in Hengduan mountains [J]. Meteorological Monthly,41(1):17−24 (in Chinese). doi:10.7519/j.issn.1000−0526.2015.01.002
|
万石云,赵宁坤,段玮.2015.云南省滑坡泥石流与强降水的相关性和多时间尺度特征研究[J].灾害学,30(1):45−50. doi: 10.3969/j.issn.1000-811X.2015.01.010
Wan S Y, Zhao N K, Duan W. 2015. Correlation and multi-timescale characteristics of strong precipitations and landslide debris flows in Yunnan province [J]. Journal of Catastrophology,30(1):45−50 (in Chinese). doi:10.3969/j.issn.1000−811X.2015.01.010
|
王凌梓,苗峻峰,韩芙蓉.2018.近10年中国地区地形对降水影响研究进展[J].气象科技,46(1):64−75. doi: 10.19517/j.1671-6345.20170081
Wang L Z, Miao J F, Han F R. 2018. Overview of impact of topography on precipitation in China over last 10 years [J]. Meteorological Science and Technology,46(1):64−75 (in Chinese). doi:10.19517/j.1671−6345.20170081
|
徐安伦,董保举,刘劲松,等.2010.洱海湖滨大气边界层结构及特征分析[J].高原气象,29(3):637−644
Xu A L, Dong B J, Liu J S, et al. 2010. Structure and characteristic of the atmospheric boundary layer in Erhai lakeside region of Dali [J]. Plateau Meteorology,29(3):637−644 (in Chinese)
|
徐安伦,李育,杨帆,等.2017.连年干旱背景下洱海流域降水的精细化特征[J].高原气象,36(6):1557−1566. doi: 10.7522/i.issn.1000-0534.2017.00014
Xu A L, Li Y, Yang F, et al. 2017. Fine-scale characteristics of rainfall in Erhai lake basin under continuous drought conditions [J]. Plateau Meteorology,36(6):1557−1566 (in Chinese). doi:10.7522/i.issn.1000−0534.2017.00014
|
许鲁君,刘辉志.2015.云贵高原洱海湖泊效应的数值模拟[J].气象学报,73(4):789−802. doi: 10.11676/qxxb2015.047
Xu L J, Liu H Z. 2015. Numerical simulation of the lake effect of Erhai in the Yunnan-Guizhou plateau area [J]. Acta Meteorologica Sinica,73(4):789−802 (in Chinese). doi: 10.11676/qxxb2015.047
|
许霖,姚蓉,陈红专,等.2020.2017年湖南一次极端降雨过程特征及成因分析[J].沙漠与绿洲气象,14(1):31−38. doi: 10.12057/j.issn.1002-0799.2020.01.004
Xu L, Yao R, Chen H Z, et al. 2020. Characteristics and causes analysis of extreme rainfall event in 2017 in Hunan province [J]. Desert and Oasis Meteorology,14(1):31−38 (in Chinese). doi:10.12057/j.issn.1002−0799.2020.01.004
|
阎丽凤,车军辉,周雪松,等.2013.泰山地形对一次局地强降水过程动力作用的数值模拟分析[J].气象,39(11):1393−1401. doi: 10.7519/j.issn.1000-0526.2013.11.002
Yan L F, Che J H, Zhou X S, et al. 2013. Numerical simulation analysis on dynamic effect of Taishan mountain terrain on local severe rainfall [J]. Meteorological Monthly,39(11):1393−1401 (in Chinese). doi:10.7519/j.issn.1000−0526.2013.11.002
|
杨智,刘劲松,孙绩华.2008.大理近地层山谷盆地湖陆风及湍流特征分析[J].气象与环境学报,24(5):32−37. doi: 10.3969/j.issn.1673-503X.2008.05.008
Yang Z, Liu J S, Sun J H. 2008. Lake-land breeze and turbulence characteristics in the surface layer of valley and basin in Dali, Yunnan province [J]. Journal of Meteorology and Environment,24(5):32−37(in Chinese). doi:10.3969/j.issn.1673−503X.2008.05.008
|
杨芳园,甄廷忠,邹灵宇,等.2021.昆明市主城区一次局地短时强降水特征研究[J].沙漠与绿洲气象,15(1):28−35. doi: 10.12057/j.issn.1002-0799.2021.01.004
Yang F Y, Zhen T Z, Zou L Y, et al. 2021. A study of the local short-time heavy rain in the main urban area of Kunming [J]. Desert and Oasis Meteorology,15(1):28−35 (in Chinese). doi:10.12057/j.issn.1002−0799.2021.01.004
|
周泓,杨若文,钟爱华,等.2015.云南省一次切变冷锋型暴雨过程的中尺度对流系统分析[J].气象,41(8):953−963. doi: 10.7519/j.issn.1000-0526.2015.08.004
Zhou H, Yang R W, Zhong A H, et al. 2015. Analysis on mesoscale convective system during a shear and cold front type rainstorm process in Yunnan province [J]. Meteorological Monthly,41(8):953−963 (in Chinese). doi:10.7519/j.issn.1000−0526.2015.08.004
|
周晓宇,周泓,段玮,等.2023.哀牢山复杂地形对一次夏季强降水影响的模拟[J].气候与环境研究,28(5):533−546. doi: 10.3878/j.issn.1006-9585.2023.23007
Zhou X Y, Zhou H, Duan W, et al. 2023. Simulation of the complex terrain influence on summer heavy precipitation in Ailao mountain [J]. Climatic and Environmental Research,28(5):533−546 (in Chinese). doi:10.3878/j.issn.1006−9585.2023.23007
|
Yu R C, Chen H M, Sun W. 2015. The definition and characteristics of regional rainfall events demonstrated by warm season precipitation over the Beijing plain [J]. Journal of Hydrometeorology,16(1):396−406. doi:10.1175/JHM−D−14−0086.1
|
Zhang M K, Li J, Li N N. 2021. Fine-scale characteristics of summer precipitation over Cang mountain [J]. Journal of Applied Meteorology and Climatology,60(9):1280−1300. doi:10.1175JAMC−D−20−0220.1
|