SUN Xin,GONG Yuanfa,GUO Lifang,et al.A Study on the Summer Monsoon over the Tibetan Plateau based on High Resolution Reanalysis Data[J].Journal of Chengdu University of Information Technology,2025,40(05):633-642.[doi:10.16836/j.cnki.jcuit.2025.05.010]
基于高分辨率再分析资料的青藏高原夏季风研究
- Title:
- A Study on the Summer Monsoon over the Tibetan Plateau based on High Resolution Reanalysis Data
- 文章编号:
- 2096-1618(2025)05-0633-10
- Keywords:
- Tibetan Plateau; summer monsoon; precipitation; East Asian; South Asian
- 分类号:
- P467
- 文献标志码:
- A
- 摘要:
- 为进一步分析高原夏季风的变化特征,利用1979-2019年高分辨率再分析数据ERA地面和高空的高分辨率再分析资料以及CPC全球逐日降水数据,在分析青藏高原夏季地面风场气候特征的基础上,定义一个新的青藏高原地面夏季风指数(TPVI),并且采用相关分析、合成分析的方法,分析高原夏季风的变化特征,研究高原夏季风变化对高原及其邻近的南亚和东亚地区降水和季风环流系统的不同影响。结果表明,新指数TPVI与汤懋苍经典指数相关性较高,能很好地表征高原季风的变化特征; 高原季风异常强(弱)时,500 hPa上高原主体是异常气旋(反气旋)式环流,高原中东部异常辐合(辐散)、降水异常偏多(少)。印度半岛北部(南部)和高原西南部异常辐散(辐合)、降水偏少(偏多)。在东亚地区,四川盆地到长江流域位于异常环流的辐合(辐散)区、降水偏多(少),江南到华南沿岸位于异常环流辐散(辐合)区、降水偏少(多); 高原夏季风异常变化对南亚季风和东亚季风的影响是不同的,并伴有月际之间的差异。
- Abstract:
- In order to analyze the variation characteristics of the summer monsoon over the Tibetan Plateau,a new surface summer monsoon index(TPVI)was defined based on the analysis of the climate characteristics of the summer surface monsoon field over the Qinghai Tibet Plateau using high-resolution reanalysis data from the ERA ground and upper atmosphere from 1979 to 2019,as well as CPC global daily precipitation data.Correlation analysis and synthesis analysis were used to analyze the variation characteristics of the summer monsoon over the Tibetan Plateau,and the different impacts of the plateau summer monsoon changes on precipitation and monsoon circulation systems over the plateau and its neighboring South and East Asia regions were studied.The results show that the new index TPVI has a high correlation with the Tang Mao cang Classic Index,which can well characterize the characteristics of the changes in the plateau monsoon; When the plateau monsoon is abnormally strong(weak),the main body of the plateau at 500 hPa is an anomalous cyclonic(anticyclonic)circulation,with anomalous convergence(divergence)and excessive(insufficient)precipitation in the central and eastern parts of the plateau.The northern(southern)part of the Indian Peninsula and the southwestern part of the plateau exhibit abnormal divergence(convergence)and less(more)precipitation.In East Asia,the Sichuan Basin to the Yangtze River Basin are located in the convergence(divergence)area of abnormal circulation,with more(less)precipitation,while the Jiangnan to South China coasts are located in the convergence(divergence)area of abnormal circulation,with less(more)precipitation; The impact of abnormal changes in the plateau summer monsoon on the South Asian and East Asian monsoons is different,and there are differences between months.
参考文献/References:
[1] 叶笃正,罗四维,朱抱真.西藏高原及其附近的流场结构和对流层大气的热量平衡[J]. 气象学报,1957,28(2):108-121.
[2] 高由禧,徐淑英.关于东亚季风区域的气候的研究[J]. 气象学报,1959,30(3):258-262.
[3] 汤懋苍.高原季风与华西气候[C]. 甘肃省气象学会年会,1962.
[4] Tang M C,Reiter E R.Plateau monsoons of the Northern Hemisphere:a comparison between North America and Tibet[J]. Monthly Weather Review,1984,112(4):617-637.
[5] 马振锋,高文良,刘富明,等.青藏高原东侧初夏旱涝的季风环流分析[J]. 高原气象,2003,22(增刊):1-7.
[6] 白虎志,马振峰,董文杰.青藏高原地区季风特征及与我国气候异常的联系[J]. 应用气象学报,2005,16(4):484-491.
[7] 李菲,段安民.青藏高原夏季风强弱对其亚洲地区降水和环流的影响-2008年个例分析[J]. 大气科学,2011,35(4):694-706.
[8] 华维,范广洲,王炳赟.近几十年青藏高原夏季风变化趋势及其对中国东部降水的影响[J]. 大气科学,2012,36(4):784-794.
[9] 周懿.高原季风变化特征分析[D]. 成都:成都信息工程学院,2014.
[10] 龙妍妍,范广洲,李飞,等.高原夏季风对中国夏季极端降水的影响研究[J]. 高原气象,2018,37(1):1-12.
[11] Luo H B,Yanai M.The large-scale circulation and heat sources over the Tibetan Plateau and surrounding areas during the early summer of 1979.Part I:Precipitation and Kinematic Analyses[J]. Monthly Weather Review,1983,111:922-944.
[12] Wu G X,Zhang Y S.Tibetan plateau forcing and the timing of the monsoon onset over south Asia and the south China sea[J]. Monthly Weather Review,1998,126:913-927.
[13] Reiter E R,Gao D Y.Heating of the Tibetan Plateau and movements of the South Asian high during spring[J]. Monthly Weather Review,1982,110:1694-1711.
[14] Zhao,Ping,Chen,et al.Interannual variablity of atmospheric heat source/sink over the Qinghai-Xizang(Tibetan)Plateau and its relation to circulation[J]. Advances in Atmospheric Sciences,2001,18(1):106-116.
[15] Zhang L,Zhi X.Longitudinal Oscillations of the South Asian High and the Subtropical Western Pacific High during Boreal Summer[J]. Advances in Geoences,2015,16:364.
[16] Duan A M,Wu G X.Role of the Tibetan Plateau thermal forcing in the summer climate patterns oversubtropical Asia[J]. ClimateDynamics,2005,24:703-807.
[17] 王同美,吴国雄,万日金.青藏高原的热力和动力作用对亚洲季风区环流的影响[J]. 高原气象,2008,27(1):1-9.
[18] 周秀骥,赵平,陈军明,等.青藏高原热力作用对北半球气候影响的研究[J]. 中国科学(地球科学),2009,39(11):1473-1486.
[19] 王奕丹,胡泽勇,孙根厚,等.高原季风特征及其与东亚夏季风关系的研究[J]. 高原气象,2019,38(3):518-527.
[20] 汤懋苍,梁娟,邵明镜,等.高原季风年际变化的初步分析[J]. 高原气象,1984,3(3):75-82.
[21] 齐冬梅,李跃清,白莹莹,等.高原夏季风指数的定义及其特征分析[J]. 高原山地气象研究,2009,29(4):1-9.
[22] 田俊,马振峰,范广洲,等.新的高原季风指数与四川盆地夏季降水的关系[J]. 气象科学,2010,30(3):308-315.
[23] Xun X Y,Hu Z Y,Ma Y M.The Dynamic Plateau Monsoon Index and Its Association with General Circulation Anomalies[J]. Advances in Atmospheric Sciences,2012,29(6):1249-1263.
[24] 王颖,李栋梁.变暖背景下青藏高原夏季风变异及其对中国西南气候的影响[J]. 气象学报,2015,73(5):910-924.
[25] 周懿,范广洲,华维,等.高原季风的分布特征及其指数对比分析[J]. 高原气象,2015,34(6):1517-1530.
[26] 庞轶舒,马振峰,杨淑群,等.盛夏高原季风指数的探讨及其对四川盆地降水的影响[J]. 高原气象,2017,36(4):886-899.
[27] 周娟,文军,王欣,等.青藏高原季风演变及其与土壤湿度的相关分析[J]. 高原气象,2017,36(1):45-56.
[28] 汤懋苍,沈志宝,陈有虞,等.高原季风的平均气候特征[J]. 地理学报,1979,34(1):33-42.
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备注/Memo
收稿日期:2024-02-28
基金项目:国家自然科学基金资助项目(U20A2097)
通信作者:巩远发.E-mail:gyfa@cuit.edu.cn
