ZHANG Jing,FAN Guang-zhou,LAI Xin,et al.Relationship between Variation of the Tibetan Plateau Summer Monsoon and South Asian High[J].Journal of Chengdu University of Information Technology,2016,(05):494-499.
高原夏季风强弱和南亚高压的关系研究
- Title:
- Relationship between Variation of the Tibetan Plateau Summer Monsoon and South Asian High
- 文章编号:
- 2096-1618(2016)05-0494-06
- Keywords:
- meteorology; climate change and numerical simulation; south asian high; tibetan plateau summer monsoon; diabatic heating
- 分类号:
- P425.4+2
- 文献标志码:
- A
- 摘要:
- 为进一步认识高原夏季风和南亚高压的关系,利用1948～2013年NCEP/NCAR日平均再分析资料,采用相关分析 和合成分析,探讨高原夏季风异常对南亚高压活动的影响。研究表明,高原夏季风强时,南亚高压中心位置偏东偏南 ,呈“青藏高压模态”,高原夏季风弱时,南亚高压中心偏西偏北,呈“伊朗高压模态”。在非绝热加热场上,高原夏 季风强时,青藏高原南侧感热偏强,青藏高原以西到伊朗高原东部感热偏弱。高原夏季风弱时,青藏高原南侧及西南 侧为感热偏弱,高原西北部感热偏强。值得注意的是,地表感热的正负异常分布与南亚高压中
- Abstract:
- In order to further acquire the relationship between the Tibetan Plateau Summer Monsoon (TPSM)and South Asian High(SAH). Using the 66-year(1948-2013)NECP/NCAR daily reanalysis data, the impact of TPSM anomaly on SAH activities are investigated by the correlation analysis and the composite analysis. The results show that a stronger(weaker)TPSM is associated with the center of the SAH shifting eastward(westward)and southward(northward), and SAH presenting its Tibetan high (Iranian high)pattern. Meanwhile, when TPSM is stronger, sensible heat over southern TP has positive anomalies and it over western TP and eastern IP has negative anomalies. When TPSM is weaker, sensible heat over southern TP and southwestern TP has negative anomalies and it over northwestern TP has positive anomalies. It's important to note that the distribution of sensible heat anomalies are consistent with SAH's center location, which reveal that the distribution of SAH's center in summer may be closely associated with sensible heating.
参考文献/References:
[1] Tao,S Y,L X Chen.A review of recent research on the East Asian summer monsoon in China
[M].Monsoon Meteorology,C P Chang and T.N.Krishnamurti,Eds.,Oxford University,Press,1987,60 -92.
[2] T N Krishnamurti,H N Bhalme.Oscillations of a Monsoon System[J].Observational
Aspects.Journal of the Atmospheric Sciences,1976,33:1937-1954.
[3] 汤懋苍. 高原季风研究的若干进展[J]. 高原气象,1993,(1):95-101.
[4] 汤懋苍,沈志宝,陈有虞. 高原季风的平均气候特征[J]. 地理学报,1979,(1):33-42.
[5] Tang Mao cang, Reiter E R. Plateau monsoons of the Northern Hemisphere [J].Monthly Weather
Review, 1984, 112(4): 617 - 637.
[6] Kuo H L, Qian Y F. Influence of Tibetan Plateau on cumulative and diurnal changes of
weather and climate in summer[J].Monthly Weather Review,1981,109(11):2337-2356.
[7] 马振锋. 高原季风强弱对南亚高压活动的影响[J]. 高原气象,2003,(2):143-146.
[8] 李菲,段安民. 青藏高原夏季风强弱变化及其对亚洲地区降水和环流的影响——2008年个例分析[J]. 大
气科学,2011,(4):694-706.
[9] 马振锋,高文良.热带海温变化与高原季风发展[J].应用气象学报,2002,13(4):440-447.
[10] 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,(4):784-794.
[11] Mason R B, Anderson C E. The development and decay of the 100-MB. Summertime anticyclone
over Southern Asia[J]. Monthly Weather Review, 1963, 91(1): 3-12.
[12] Yongfu Q, Qiong Z, Yonghong Y, et al. Seasonal variation and heat preference of the South
Asia High[J]. Advances in Atmospheric Sciences, 2002, 19(5): 821-836.
[13] 陶诗言, 朱福康. 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,1964,(4):3-14.
[14] 罗四维, 钱正安, 王谦谦. 夏季 100 毫巴青藏高压与我国东部旱涝关系的天气气候研究[J]. 高原气
象, 1982, 1(2): 1-10.
[15] 朱福康,陆龙弊,陈咸吉,等.南亚高压[M]. 北京:科学出版社, 1980.
[16] 王斌, 李跃清. 近 10 多年南亚高压活动特征及其影响的研究进展[J]. 高原山地气象研究, 2011,
31(2): 75-80.
[17] 魏维,张人禾,温敏. 南亚高压的南北偏移与我国夏季降水的关系[J]. 应用气象学报,2012,(6):650-
659.
[18] Wei Wei, Zhang R H, Wen M, et al. Impact of Indian summer monsoon on the South Asian High
and its influence on summer rainfall over China [J]. Clim Dyn,2014,(43):1257-1269.
[19] 张琼,钱永甫,张学洪. 南亚高压的年际和年代际变化[J]. 大气科学,2000,(1):67-78.
[20] 周懿. 高原季风变化特征分析[D].成都:成都信息工程大学,2014.
[21] Yanai M, Esbensen S, Chu J H. Determination of bulk properties of tropical cloud clusters
form large-scale heat and moisture budgets[J]. J. Atmos. Sci., 1973,30: 611-627.
相似文献/References:
[1]廖洪涛,肖天贵,魏 微,等.东亚梅雨季低频波波包传播特征[J].成都信息工程大学学报,2019,(02):143.[doi:10.16836/j.cnki.jcuit.2019.02.008]
LIAO Hongtao,XIAO Tiangui,WEI Wei,et al.Low Frequency Wave Packet Propagation
Characteristics in East Asian Meiyu Season[J].Journal of Chengdu University of Information Technology,2019,(05):143.[doi:10.16836/j.cnki.jcuit.2019.02.008]
[2]王雨歌,郑佳锋,朱克云,等.一次西南涡过程的云-降水毫米波云雷达回波特征分析[J].成都信息工程大学学报,2019,(02):172.[doi:10.16836/j.cnki.jcuit.2019.02.011]
WANG Yuge,ZHENG Jiafeng,ZHU Keyun,et al.Analysis of Cloud-Precipitation Echo Characteristics of a Southwest Vortex[J].Journal of Chengdu University of Information Technology,2019,(05):172.[doi:10.16836/j.cnki.jcuit.2019.02.011]
[3]青 泉,罗 辉,陈刚毅.基于L波段秒级探空数据V-3θ图形的四川盆地暴雨预报模型研究[J].成都信息工程大学学报,2019,(02):186.[doi:10.16836/j.cnki.jcuit.2019.02.013]
QING Quan,LUO Hui,CHEN Gangyi.Forecasting Model of Torrential Rain in Sichuan Basin based on V-3θ
Structural Graphs of L-Band Second Level Sounding Data[J].Journal of Chengdu University of Information Technology,2019,(05):186.[doi:10.16836/j.cnki.jcuit.2019.02.013]
[4]吴秋月,华 维,申 辉,等.基于湿位涡与螺旋度的一次西南低涡强降水分析[J].成都信息工程大学学报,2019,(01):63.[doi:10.16836/j.cnki.jcuit.2019.01.013]
WU Qiuyue,HUA Wei,SHEN Hui,et al.Diagnostic Analysis of a Southwest Vortex Rainstormbased on Moist Potential Vorticity and Helicity[J].Journal of Chengdu University of Information Technology,2019,(05):63.[doi:10.16836/j.cnki.jcuit.2019.01.013]
[5]李潇濛,赵琳娜,肖天贵,等.2000-2015年青藏高原切变线统计特征分析[J].成都信息工程大学学报,2018,(01):91.[doi:10.16836/j.cnki.jcuit.2018.01.016]
LI Xiao-meng,ZHAO Lin-na,XIAO Tian-gui,et al.Statistical Characteristics Analysis of the Shear Linein the Qinghai-Tibet Plateau from 2000 to 2015[J].Journal of Chengdu University of Information Technology,2018,(05):91.[doi:10.16836/j.cnki.jcuit.2018.01.016]
[6]喻乙耽,马振峰,范广洲.华西秋雨气候特征分析[J].成都信息工程大学学报,2018,(02):164.[doi:10.16836/j.cnki.jcuit.2018.02.011]
YU Yi-dan,MA Zhen-feng,FAN Guang-zhou.The Analysis of Climatic Feature of Autumn Rainfall in West China[J].Journal of Chengdu University of Information Technology,2018,(05):164.[doi:10.16836/j.cnki.jcuit.2018.02.011]
[7]孙康慧,巩远发.20世纪70年代末云南省雨季降水的突变及原因分析[J].成都信息工程大学学报,2018,(02):177.[doi:10.16836/j.cnki.jcuit.2018.02.012]
SUN Kang-hui,GONG Yuan-fa.Abrupt Change of Precipitation in Rainy Season in YunnanProvince in Late 1970s and its Cause Analysis[J].Journal of Chengdu University of Information Technology,2018,(05):177.[doi:10.16836/j.cnki.jcuit.2018.02.012]
[8]吴树炎,顾建峰,刘海文,等.高原冬季雪深与重庆夏季降水的年际关系研究[J].成都信息工程大学学报,2018,(02):184.[doi:10.16836/j.cnki.jcuit.2018.02.013]
WU Shu-yan,GU Jian-feng,LIU Hai-wen,et al.Interannual Relationship between Winter Snow Depth over TibetanPlateau and Summer Precipitation over Chongqing[J].Journal of Chengdu University of Information Technology,2018,(05):184.[doi:10.16836/j.cnki.jcuit.2018.02.013]
[9]魏 凡,李 超.利用气象雷达信息划设雷暴飞行限制区的方法研究[J].成都信息工程大学学报,2018,(02):205.[doi:10.16836/j.cnki.jcuit.2018.02.016]
WEI Fan,LI Chao.Study on the Method of Setting Up Limited Flying area ofThunderstorm by Using Weather Radar Information[J].Journal of Chengdu University of Information Technology,2018,(05):205.[doi:10.16836/j.cnki.jcuit.2018.02.016]
[10]朱 莉,张腾飞,李华宏,等.云南一次短时强降水过程的中尺度特征及成因分析[J].成都信息工程大学学报,2018,(03):335.[doi:10.16836/j.cnki.jcuit.2018.03.017]
ZHU Li,ZHANG Teng-fei,LI Hua-hong,et al.Analysis on Meso-scale Features and Forming Reasons of a Short TimeIntensive Precipitation Case in Yunnan Province[J].Journal of Chengdu University of Information Technology,2018,(05):335.[doi:10.16836/j.cnki.jcuit.2018.03.017]
备注/Memo
收稿日期:2016-01-06 基金项目:国家自然科学基金资助项目(91537214、41275079、4140 5069、41305077、41505078); 公益性行业(气 象)科研专项资助项目(GYHY201506001); 四川省教育厅科研资助项目(16ZA0203)