1998年和2010年夏季长江流域降水低频变化及水汽输送特征对比分析
Comparative Analysis of the Characteristics of the Low-Frequency Precipitation and Low-Frequency Water Vapor Transport over Yangtze River during Summer in 1998 and 2010
DOI: 10.12677/CCRL.2018.74026, PDF,   
作者: 罗 菁*, 孙金花, 钟泽洲:湖南省汨罗市气象局,湖南 汨罗;李丽平:南京信息工程大学大气科学学院,江苏 南京
关键词: 厄尔尼诺长江流域低频降水低频水汽输送El Nino Yangtze River Low-Frequency Precipitation Low-Frequency Water Vapor Transport
摘要: 利用长江流域夏季降水资料和NCEP/NCAR再分析资料、NOAA海温等资料,对比分析了1998年和2010年夏季降水异常特征,探讨了不同分布型厄尔尼诺事件背景下长江流域典型涝年夏季低频降水特征及其低频水汽输送差异。结果表明,1998年长江流域全流域性多降水,而2010年降水偏多区域主要集中在长江中下游地区。1998年夏季长江流域降水存在8~15 d和30~50 d的显著低频周期,来自阿拉伯海、孟加拉湾的西南低频水汽输送及沿着副高西南、西北边缘来自西太平洋、南海的东南低频水汽输送对该年长江流域夏季8~15 d低频降水的发生和维持有着显著的作用;而2010年长江流域夏季降水存在10~20 d和30~60 d的显著低频周期,来自西太平洋的偏东低频水汽输送和沿副高西南侧北上的东南低频水汽输送对该年夏季长江流域10~20 d低频降水的发生和维持有着显著的作用。
Abstract: In this study, summer rainfall anomalies in China in the two years are compared by using the summer rainfall dataset in the Yangtze River, NCEP/NCAR reanalysis data, NOAA sea surface temperature data and so on, revealing the characteristics and the differences in low-frequency water vapor transport of the summer low-frequency precipitation of typical flood years in the Yangtze River under the background of the different type of El Nino events. The results show that the whole basin multi-precipitation occurred in the Yangtze River in 1998 while the region of more rainfall is mainly concentrated in the middle and lower reaches of the Yangtze River in 2010. There is a significant low-frequency period of 8 - 15 d and 30 - 50 d during the phase of the summer rainfall in the Yang-tze River in 1998. The southwest low-frequency water vapor transport from the Arabian Sea, the Bay of Bengal and the one from the western Pacific, South China Sea along the southwest, northwest edge of the western Pacific subtropical high play an important role in the development and maintenance of the 8 - 15 d low-frequency precipitation period in summer in the Yangtze River in 1998. In contrast, there is a significant low-frequency period of 10 - 20 d and 30 - 60 d during the phase of the summer rainfall in the Yangtze River in 2010. The east low-frequency water vapor transport from the western Pacific and the northward southeast one along the southwest edge of the western Pacific subtropical high play an important role in the development and maintenance of the 10 - 20 d low-frequency precipitation period in summer in the Yangtze River in 2010.
文章引用:罗菁, 李丽平, 孙金花, 钟泽洲. 1998年和2010年夏季长江流域降水低频变化及水汽输送特征对比分析[J]. 气候变化研究快报, 2018, 7(4): 232-244. https://doi.org/10.12677/CCRL.2018.74026

参考文献

[1] 符淙斌, 腾星林. 我国夏季的气候异常与厄尔尼诺/南方涛动现象的关系[J]. 大气科学, 1988, 12(特刊): 133-141.
[2] 陈文. El Nino和LaNina事件对东亚冬、夏季风循环的影响[J]. 大气科学, 2002, 26(5): 595-610.
[3] Huang, R.H. and Wu, Y.F. (1989) The Influence of ENSO on the Summer Climate Change in China and Its Mechanism. Advances in Atmospheric Sciences, 6, 21-32. [Google Scholar] [CrossRef
[4] 金祖辉, 陶诗言. ENSO循环与中国东部地区夏季和冬季降水关系的研究[J]. 大气科学, 1999, 23(6): 663-672.
[5] 袁媛, 杨辉, 李崇银. 不同分布型厄尔尼诺事件及对中国次年夏季降水的可能影响[J]. 气象学报, 2012, 70(3): 467-478.
[6] Feng, J. and Li, J.P. (2011) Influence of El Nino Modoki on Spring Rainfall over South China. Journal of Geophysical Research: Atmospheres, 116, D13102. [Google Scholar] [CrossRef
[7] Feng, J., Chen, W., Tam, C.Y., et al. (2011) Different Impacts of El Nino and El Nino Modoki on China Rainfall in the Decaying Phases. International Journal of Climatology, 31, 2091-2101. [Google Scholar] [CrossRef
[8] 黄荣辉, 徐予红, 王鹏飞, 等. 1998年夏长江流域特大洪涝特征及其成因探讨[J]. 气候与环境研究, 1998, 3(4): 300-313.
[9] 贾小龙, 陈丽娟, 龚振淞, 等. 2010年海洋和大气环流异常及对中国气候的影响[J]. 气象, 2011, 37(4): 446-453.
[10] 丁一汇, 胡国权. 1998年中国大洪水时期的水汽收支研究[J]. 气象学报, 2003, 61(2): 129-145.
[11] 谢安, 毛江玉, 宋焱云, 叶谦. 长江中下游地区水汽输送的气候特征[J]. 应用气象学报, 2002, 13(1): 67-77.
[12] 姚文清, 徐祥德, 张雪金. 1998年长江流域梅雨期暴雨过程的水汽输送特征[J]. 大气科学学报, 2003, 26(4): 496-503.
[13] 陶玫, 蒋薇, 项瑛, 等. 1998和2010年长江流域汛期洪涝成因对比分析[J]. 气象科学, 2012, 32(3): 282-287.
[14] 王钦, 李双林, 付建建, 李国平. 1998和2010年夏季降水异常成因的对比分析: 兼论两类不同厄尔尼诺事件的影响[J]. 气象学报, 2012, 70(6): 1207-1222.
[15] 刘芸芸, 丁一汇. 西北太平洋夏季风对中国长江流域夏季降水的影响[J]. 大气科学, 2009, 33(6): 1225-1237.
[16] Krishnamurti, T.N. and Subrahmanyan, D. (1982) The 30-50 Day Mode at 850 mb during MONEX. Journal of the Atmospheric Sciences, 39, 2080-2095. [Google Scholar] [CrossRef
[17] 陆尔, 丁一汇. 1991年江淮特大暴雨与东亚大气低频振荡[J]. 气象学报, 1996, 54(6): 730-736.
[18] Yang, J., Wang, B., Wang, B., et al. (2010) Biweekly and 21-30-Day Varia-tions of the Subtropical Summer Monsoon Rainfall over the Lower Reach of the Yangtze River Basin. Journal of Climate, 23, 1146-1159. [Google Scholar] [CrossRef
[19] 左金清, 任宏利, 李维京, 等. 我国南方夏季低频雨型的季节内水汽输送特征[J]. 地球物理学报, 2009, 52(9): 2210-2221.
[20] 吴洪宝, 吴蕾. 气候变率诊断和预测方法[M]. 北京: 气象出版社, 2005: 208-225.
[21] Lau, K.-M., Yang, G.J. and Shen, S.H. (1988) Seasonal and Intraseasonal Climatology of Monsoon Rainfall over East Asia. Monthly Weather Review, 116, 18-37. [Google Scholar] [CrossRef
[22] Chan, J.C.L., Ai, W. and Xu, J. (2002) Mechanisms Responsible for the Maintenance of the 1998 South China Sea Summer Monsoon. Jour-nal of the Meteorological Society of Japan, 80, 1103-1113. [Google Scholar] [CrossRef
[23] 毛红玉, 吴国雄. 1991年江淮梅雨与副热带高压的低频特征[J]. 气象学报, 2005, 63(5): 762-770.
[24] 李丽平, 许冠宇, 柳艳菊. 2010年华南前汛期低频水汽输送对低频降水的影响[J]. 热带气象学报, 2014, 30(3): 423-431.
[25] 闫之辉, 田华. 1998年6月下旬长江中下游强降水过程成因分析[J]. 应用气象学报, 2002, 13(6): 680-687.
[26] 张耀华, 周兵, 张耀存. 2010年南方持续暴雨期大气环流异常及其低频特征研究[J]. 气象, 2012, 38(11): 1367-1377.