高原气象

高原气象 >

2017 , Vol. 36 >Issue 5: 1209 - 1220

DOI: https://doi.org/10.7522/j.issn.1000-0534.2016.00123

论文

南亚高压的多模态特征及其与新疆夏季降水的联系

  • 王前 ,
  • 赵勇 ,
  • 陈飞 ,
  • 杨青 ,
  • 黄安宁
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  • 中国民用航空华东地区空中交通管理局气象中心, 上海 200335;南京大学大气科学学院/中国气象局-南京大学气候预测研究联合实验室, 南京 210046;成都信息工程大学大气科学学院, 成都 610225;环境保护部南京环境科学研究所, 南京 210042;中国气象局乌鲁木齐沙漠气象研究所, 乌鲁木齐 830002;江苏省气候变化协同创新中心, 南京 210046

收稿日期: 2016-03-11

  网络出版日期: 2017-10-28

基金资助

国家自然科学基金项目（91437109, 41375101, 91537102）；江苏高校“青蓝工程”优秀青年骨干教师培养计划项目（0207001802）

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Characteristics of Different Patterns of South Asia High and Their Relationships with Summer Precipitation in Xinjiang

  • WANG Qian ,
  • ZHAO Yong ,
  • CHEN Fei ,
  • YANG Qing ,
  • HUANG Anning
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  • Meteorological Center of East China Air Traffic Management Bureau, Shanghai 200335, China;China Meteorological Administration-Nanjing University Joint Laboratory for Climate Prediction Studies, School of Atmospheric Sciences, Nanjing University, Nanjing 210046, China;School of Atmospheric Sciences, Chengdu University of Information Technology, Chengdu 610225, China;Nanjing Institute of Environmental Sciences, Ministry of Environmental Protection, Nanjing 210042, China;Institute of Desert Meteorology, China Meteorological Administration, Urumqi 830002, China;Jiangsu Collaborative Innovation Center for Climate Change, Nanjing 210046, China

Received date: 2016-03-11

  Online published: 2017-10-28

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摘要

基于欧洲中期天气预报中心（ECMWF）的Interim再分析资料（ERA-Interim）和新疆88个观测站点降水资料, 分析了1979-2013年夏季（7月和8月）南亚高压多模态特征及其与新疆夏季降水的关系。结果表明, 南亚高压除了青藏高压型和伊朗高压型外, 还存在双体型。伊朗高压型和双体型分布产生的降水占新疆夏季总降水的70%~90%, 青藏高压型分布产生的降水相对较少, 占10%~30%。南亚高压的多模态分布对新疆降水有不同影响, 伊朗高压型时, 北疆部分地区和东疆降水偏多, 塔里木盆地降水偏少；青藏高压型时, 除塔里木盆地西南部降水偏多外, 新疆其余地方降水均偏少。南亚高压双体型对塔里木盆地夏季降水影响最为突出, 当夏季南亚高压呈双体型分布时, 塔里木盆地降水偏多。合成分析发现, 南亚高压双体型中心位置变化对环流和水汽输送产生不同影响, 因而对应的塔里木盆地夏季降水也存在一定差异。当两个中心位置同时偏西时, 塔里木盆地中西部地区降水偏多, 水汽分两步进入塔里木盆地。当两个中心位置同时偏北时, 整个塔里木盆地降水增加, 水汽沿着青藏高原东侧绕流进入塔里木盆地。

关键词： 南亚高压; 双体型; 夏季降水; 新疆

本文引用格式

王前 , 赵勇 , 陈飞 , 杨青 , 黄安宁 . 南亚高压的多模态特征及其与新疆夏季降水的联系[J]. 高原气象, 2017 , 36(5) : 1209 -1220 . DOI: 10.7522/j.issn.1000-0534.2016.00123

Abstract

By using the ERA-Interim reanalysis data and precipitation data which was provided by 88 observation stations in Xinjiang, the relationships between the characteristics of different patterns of South Asia High and the summer precipitation (July and August) in Xinjiang during 1979-2013 were analyzed.The results showed that except Iran high pattern and Qinghai-Tibetan high pattern, the South Asia High could also be divided into Two centers pattern and Multiple centers pattern.The precipitation of Iran high pattern and Two centers pattern accounted for 70%~90% of summer total precipitation in Xinjiang, while the precipitation of Qinghai-Tibetan high pattern accounted for 10%~30% of summer total precipitation.Iran high pattern, Qinghai-Tibetan high pattern and Two centers pattern have different characteristics, and different patterns of South Asia High have different effects on the summer precipitation in Xinjiang.The precipitation of Iran high pattern increased in most parts of northern and eastern Xinjiang and decreased in the Tarim Basin in Xinjang compared to the averaged summer precipitation.Qinghai-Tibetan high pattern had the opposite precipitation distribution compared with the precipitation distribution of Iran high pattern.The precipitation of Qinghai-Tibetan high pattern decreased in most parts of Xinjiang except in southwestern parts of the Tarim Basin compared to the averaged summer precipitation.Two centers pattern had the largest impact on summer precipitation in the Tarim Basin.The precipitation of two centers pattern increased in the Tarim Basin compared to the averaged summer precipitation while the precipitation of Iran high pattern and Qinghai-Tibetan high pattern decreased in Tarim Basin.Based on the method of composite analysis, the results indicated that the changes of two centers positions of South Asia High had different impacts on circulation and moisture transport.Due to the different characteristics of circulation and moisture transport, the distributions of summer precipitation in the Tarim Basin were relatively different.The precipitation in central and western parts of the Tarim Basin increased compared to the averaged summer precipitation when two centers of South Asia High were both on the west of the averaged longitude, and the water vapor came into the Tarim Basin in Xinjiang from low latitudes by a two-step process.The precipitation in the whole Tarim Basin increased compared to the averaged summer precipitation when two centers of South Asia High were both on the north of the averaged latitude, and the water vapor came into the Tarim Basin along the east side of Qinghai-Tibetan Plateau.

Key words： South Asia High; Two centers pattern; Summer precipitation; Xinjiang

参考文献

[1]Bao X, Zhang F. 2013. Evaluation of NCEP-CFSR, NCEP-NCAR, ERA-Interim, and ERA-40 reanalysis datasets against independent sounding observations over the Tibetan Plateau[J]. J Climate, 26(1):206-214. DOI:10. 1175/JCLI-D-12-00056. 1.
[2]Berrisford P, Dee D, Poli P, et al. 2011. The ERA-initerim archive version 2. 0[R]. ERA report series, 1.
[3]Dee D P, Uppala S M, Simmons A J, et al. 2011. The ERA-Interim reanalysis:Configuration and performance of the data assimilation system[J]. Quart J Roy Meteor Soc, 137(656):553-597. DOI:10. 1002/qj. 828.
[4]Huang W, Feng S, Chen J H, et al. 2015. Physical mechanisms of summer precipitation variations in the Tarim Basin in northwestern China[J]. J Climate, 28:3579-3591. DOI:10. 1175/JCLI-D-14-00395. 1.
[5]Mason R B, Anderson C E. 1963. The development and decay of the 100-MB summertime anticyclone over Southern Asia[J]. Mon Wea Rev, 91(1):3-12.
[6]Qian Y F, Zhang Q, Yao Y H, et al. 2002. Seasonal variation and heat preference of the South Asia High[J]. Adv Atmos Sci, 19(5):821-836.
[7]Zhang Q, Wu G X, Qian Y F. 2002. The bimodality of the 100hPa South Asia High and its relationship to the climate anomaly over East Asia in summer[J]. J Meteor Soc Japan, 80(4):733-744.
[8]Zhao Y, Huang A N, Zhou Y, et al. 2014. Impact of the middle and upper tropospheric cooling over central Asia on the summer rainfall in the Tarim Basin[J]. J Climate, 27:4721-4732.
[9]Cai Ying, Song Minhong, Qian Zheng'an, et al. 2015. Reanalyses of precipitation circulation and vapor transportation of severe dry and wet events in summer in arid region of northwest China. Plateau Meteor, 34(3):597-610. DOI:10. 7522/j. issn. 1000-0534. 2015. 00049.<br/>蔡英, 宋敏红, 钱正安, 等. 2015.西北干旱区夏季强干、湿事件降水环流及水汽输送的再分析[J].高原气象, 34(3):597-610.
[10]Chen Xianji, Zhu Fukang, Lu Longhua, et al. 1980. Quasi three year oscillation period of South Asia High[J]. Meteor Sci Technol, 8(1):1-3.<br/>陈咸吉, 朱福康, 陆龙骅, 等. 1980.南亚高压准三年振荡周期[J].气象科技, 8(1):1-3.
[11]Duan Anmin, Liu Yimin, Wu Guoxiong. 2003. Thermal state of Tibetan Plateau in April to June and association with East Asian summer precipitation and atmospheric circulation anomalies[J]. Science in China (Ser. D), 33(10):997-1004.<br/>段安民, 刘屹岷, 吴国雄. 2003. 4-6月青藏高原热状况与盛夏东亚降水和大气环流的异常[J].中国科学(D辑), 33(10):997-1004.
[12]Huang Yanyan, Qian Yongfu. 2004. Relationship between South Asian High and characteristic of precipitation in mid-and lower-reaches of Yangtze river and north China[J]. Plateau Meteor, 23(1):68-74. DOI:10. 3321/j. issn:1000-0534. 2004. 01. 010.<br/>黄燕燕, 钱永甫. 2004.长江流域, 华北降水特征与南亚高压的关系分析[J].高原气象, 23(1):68-74.
[13]Huang Ying, Qian Yongfu. 2004. Relationships between South Asian High and summer rainfall in north China[J]. Plateau Meteor, 22(6):602-607. DOI:10. 3321/j. issn:1000-0534. 2003. 06. 011.<br/>黄樱, 钱永甫. 2004.南亚高压与华北夏季降水的关系[J].高原气象, 22(6):602-607.
[14]Lin Houbo, You Qinglong, Jiao Yang, et al. 2016. Water vapor transportation and its influences on precipitation in summer over Qinghai-Xizang Plateau and its surroundings[J]. Plateau Meteor, 35(2):309-317. DOI:10. 7522/j. issn. 1000-0534. 2014. 00146.<br/>林厚博, 游庆龙, 焦洋, 等. 2016.青藏高原及附近水汽输送对其夏季降水影响的分析[J].高原气象, 35(2):309-317.
[15]Liu Boqi, He Jinhai, Wang Lijuan. 2009. Characteristics of the South Asia High establishment processes above the Indo-China Peninsula from April to May and their possible mechanism[J]. Chinese J Atmos Sci, 33(6):1319-1332.<br/>刘伯奇, 何金海, 王黎娟. 2009. 4-5月南亚高压在中南半岛上空建立过程特征及其可能机制[J].大气科学, 33(6):1319-1332.
[16]Liu Huiyun. 2001a. Correlation analysis between anomalous precipitation in Xinjiang and monthly mean circulation features of South Asia High in summer[J]. Bimonthly of Xinjiang Meteorology, 24(3):9-11.<br/>刘惠云. 2001a.新疆夏季降水异常与100 hPa南亚高压月平均环流特征的相关分析[J].新疆气象, 24(3):9-11.
[17]Liu Huiyun, Ma Jun. 2001b. Correlation of the precipitation in Xinjiang in summer and the circulation features of South Asia High[J]. Bimonthly of Xinjiang Meteorology, 24(6):1-3.<br/>刘惠云, 麻军. 2001b.新疆夏季降水与南亚高压逐日环流特征的相关分析[J].新疆气象, 24(6):1-3.
[18]Liu Mei, Hu Luolin, Pu Meijuan, et al. 2007. Study on change of South Asia High and response of other weather system during summer[J]. Scientia Meteor Sinica, 27(3):294-301.<br/>刘梅, 胡洛林, 濮梅娟, 等. 2007.夏季南亚高压的演变及有关天气系统的响应研究[J].气象科学, 27(3):294-301.
[19]Liu Mei, Hu Luolin, Zhang Bei. 2008. Study on connection between South Asia High character of 100 hPa in plum flood season and Jiangsu plum rain[J]. J Trop Meteor, 24(3):285-293.<br/>刘梅, 胡洛林, 张备. 2008.梅汛期100hPa南亚高压特征与江苏梅雨关系研究[J].热带气象学报, 24(3):285-293.
[20]Qi Yulei, Feng Song, Huang Jianping, et al. 2015. Influence of Plateau Summer Monsoon on summer precipitation in the arid and semi-arid regions of the central and East Asia[J]. Plateau Meteor, 34(6):1566-1574. DOI:10. 7522/j. issn. 1000-0534. 2014. 00088.<br/>齐玉磊, 冯松, 黄建平, 等. 2015.高原夏季风对中东亚干旱半干旱区夏季降水的影响[J].高原气象, 34(6):1566-1574.
[21]Qian Yongfu, Jiang Jing, Zhang Yan, et al. 2004. The earliest onset area of the tropical Asia summer monsoon and its mechanisms[J]. Acta Meteor Sinica, 62(2):129-139.<br/>钱永甫, 江静, 张艳, 等. 2004.亚洲热带夏季风的首发地区和机理研究[J].气象学报, 62(2):129-139.
[22]Qian Yongfu, Zhang Qiong. 2002. The South Asian High and its effects on China's mid-summer climate abnormality[J]. Journal of Nanjing University (Natural Science), 38(3):295-307.<br/>钱永甫, 张琼. 2002.南亚高压与我国盛夏气候异常[J].南京大学学报:自然科学版, 38(3):295-307.
[23]Shi Yuguang, Sun Zhaobo. 2008. Climate characteristics of atmospheric precipitable water over Xinjiang and its variation[J]. J Desert Res, 28(3):519-525.<br/>史玉光, 孙照渤. 2008.新疆大气可降水量的气候特征及其变化[J].中国沙漠, 28(3):519-525.
[24]Tao Shiyan, Zhu Fukang. 1964. The 100-mb flow patterns in south Asia in summer and its relation to the advance and retreat of the West-Pacific subtropical anticyclone over the far east[J]. Acta Meteor Sinica, 34(4):385-396.<br/>陶诗言, 朱福康. 1964.夏季亚洲南部100毫巴流型的变化及其与西太平洋副热带高压进退的关系[J].气象学报, 34(4):385-396.
[25]Wang Lijuan, Guo Shuaihong. 2012. Interannual variability of the South Asian High establishment over the Indo-China Peninsula from April to May and its relation to Southern Asian summer monsoon[J]. Trans Atmos Sci, 35(1):10-23.<br/>王黎娟, 郭帅宏. 2012. 4-5月南亚高压在中南半岛上空建立的年际变化特征及其与亚洲南部夏季风的关系[J].大气科学学报, 35(1):10-23.
[26]Wu Guoxiong, Mao Jiangyu, Duan Anmin, et al. 2004. Recent Progress in the study on the impacts of Tibetan Plateau on Asian summer climate[J]. Acta Meteor Sinica, 62(5):528-540.<br/>吴国雄, 毛江玉, 段安民, 等. 2004.青藏高原影响亚洲夏季气候研究的最新进展[J].气象学报, 62(5):528-540.
[27]Yang Lianmei, Liu Wen. 2016. Cause analysis of persistent heavy snow processes in the Northern Xinjiang[J]. Plateau Meteor, 35(2):507-519. DOI:10. 7522/j. issn. 1000-0534. 2014. 00161.<br/>杨莲梅, 刘雯. 2016.新疆北部持续性暴雪过程成因分析[J].高原气象, 35(2):507-519.
[28]Yang Lianmei, Zhang Qingyun. 2007a. Surface latent heat flux characteristics over Tibetan Plateau and circulations of summer precipitation anomalies in south Xinjiang[J]. Plateau Meteor, 26(3):435-441. DOI:10. 3321/j. issn:1000-0534. 2007. 03. 001.<br/>杨莲梅, 张庆云. 2007a.南疆夏季降水异常的环流和青藏高原地表潜热通量特征分析[J].高原气象, 26(3):435-441.
[29]Yang Lianmei, Zhang Qingyun. 2007b. Circulation characteristics of interannual and interdecadal anomalies of summer rainfall in north Xinjiang[J]. Chinese J Geophys, 50(2):412-419.<br/>杨莲梅, 张庆云. 2007b.新疆北部汛期降水年际和年代际异常的环流特征[J].地球物理学报, 50(2):412-419.
[30]Zhang Jiabao, Deng Zifeng. 1987. The introduction of precipitation in Xinjiang[M]. Beijing:China Meteorological Press.<br/>张家宝, 邓子风.新疆降水概论[M]. 1987.北京:气象出版社.
[31]Zhang Qiong, Qian Yongfu, Zhang Xuehong. 2000. Interannual and interdecadal variations of the South Asia High[J]. Scientia Atmos Sinica, 24(1), 67-78.<br/>张琼, 钱永甫, 张学洪. 2000.南亚高压的年际和年代际变化[J].大气科学, 24(1):67-78.
[32]Zhang Qiong, Qian Zheng'an. 1997. The further study about south Asia High in summer Ⅰ. Statistic analyses of relationship between it and precipitation distribution over northwest china[J]. Plateau Meteor, 16(1):52-62.<br/>张琼, 钱正安. 1997.关于夏季南亚高压的进一步研究:Ⅰ.与我国西北地区降水关系的统计分析[J].高原气象, 16(1):52-62.
[33]Zhang Qiong, Wu Guoxiong. 2001. The large area flood and drought over Yangtze river valley and its relation to the south Asia High[J]. Acta Meteor Sinica, 59(5):569-577.<br/>张琼, 吴国雄. 2001.长江流域大范围旱涝与南亚高压的关系[J].气象学报, 59(5):569-577.
[34]Zhang Qiong. 1999. Laws of variation, mechanism and regional climatic effects of the South Asia High[D]. Nanjing:Nanjing University, 1-148.<br/>张琼. 1999. 南亚高压的演变规律, 机制及其对区域气候的影响[D]. 南京: 南京大学, 1-148.
[35]Zhao Yong, Li Ruqi, Yang Xia, et al. 2013. Impact of the anomaly of surface sensible heat in Qinghai-Xizang Plateau and its surrounding areas on summertime precipitation in northern Xinjiang[J]. Plateau Meteor, 32(5):1215-1223. DOI:10. 7522/j. issn. 1000-0534. 2012. 00117.<br/>赵勇, 李如琦, 杨霞, 等. 2013. 5月青藏高原地区感热异常对北疆夏季降水的影响[J].高原气象, 32(5):1215-1223.
[36]Zheng Sasa, Li Yueqing, Qi Dongmei, et al. 2014. The impact of Tibetan Plateau summer monsoon on the climate of the Yangtze River Basin and contact with South Asia[J]. Plateau Mountain Meteor Res, 34(2):30-38.<br/>郑飒飒, 李跃清, 齐冬梅, 等. 2014.青藏高原夏季风对长江中下游气候的影响及与南亚高压的联系[J].高原山地气象研究, 34(2):30-38.
[37]Zhou Limin, Chen Haishan, Peng Lixia, et al. 2016. Possible connection between interdecadal variations of snow depth in winter and spring over Qinghai-Xizang Plateau and South Asia High in summer[J]. Plateau Meteor, 35(1):13-23. DOI:10. 7552/j. issn. 1000-0534. 2014. 00152.<br/>周利敏, 陈海山, 彭丽霞, 等. 2016.青藏高原冬春雪深年代际变化与南亚高压可能联系[J].高原气象, 35(1):13-23.
[38]Zhu Fukang, Lu Longhua, Chen xianji. 1980. South Asia High[M]. Beijing:Science Press.<br/>朱福康, 陆龙骅, 陈咸吉. 1980.南亚高压[M].北京:科学出版社.
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