中东急流与东亚冬季风的相关关系
The Correlation between the Middle East Jet Stream and the East Asian Winter Monsoon
DOI: 10.12677/gser.2024.134081, PDF,   
作者: 周嘉鑫:成都信息工程大学大气科学学院/大气科学,四川 成都
关键词: 中东急流东亚冬季风气温降水Climate Change Middle East Jet Stream Temperature Precipitation
摘要: 为了研究中东急流对东亚冬季风系统的影响,本文基于1979~2021年ERA5月平均再分析资料,使用EOF分析,回归分析等方法研究了冬季中东急流的时空变化特征及其对东亚冬季大气环流和气温、降水的影响。结果表明:(1) 冬季中东急流变化的第一模态反映出急流核下游的急流变化特征,第二模态呈现出显著的南北反相变化特征,第三模态反映出急流核上游的急流变化特征;(2) 冬季中东急流的强度异常和东西位置异常都对东亚地区的冬季气候变化有着重要影响:当中东急流强度偏强,位置偏东时,中国南方地区出现异常偏南风,有利于冬季降水增多。中国东北、朝鲜半岛及日本地区的通过下沉增温导致冬季温度升高。(3) 中东急流异常对东亚大槽、东亚西风急流有显著影响,中东急流强度偏强,位置偏东时,东亚大槽、东亚急流减弱。对西伯利亚高压和阿留申低压的影响较不显著。
Abstract: To investigate the impact of the Middle East Jet Stream on the East Asian Winter Monsoon System, this study utilized the ERA5 monthly mean reanalysis data from 1979 to 2021, employing EOF analysis, regression analysis, and other methods to examine the spatiotemporal variations of the winter Middle East Jet Stream and its influence on the atmospheric circulation, temperature, and precipitation in East Asia during winter. The results indicate that: (1) The first mode of variation in the winter Middle East Jet Stream reflects the characteristics of jet changes downstream of the jet core, while the second mode exhibits significant north-south phase opposition, and the third mode reflects the characteristics of jet changes upstream of the jet core; (2) Abnormalities in the intensity and east-west position of the winter Middle East Jet Stream have significant impacts on the winter climate change in East Asia: When the jet is unusually strong and located further east, anomalous southerly winds occur in southern China, favoring increased winter precipitation. Meanwhile, the temperature in Northeast China, the Korean Peninsula, and Japan rises due to subsidence warming. (3) Abnormalities in the Middle East Jet Stream have a significant impact on the East Asian trough and the East Asian westerly jet. When the jet is unusually strong and located further east, the East Asian trough and jet weaken. However, the impact on the Siberian High and the Aleutian Low is less significant.
文章引用:周嘉鑫. 中东急流与东亚冬季风的相关关系[J]. 地理科学研究, 2024, 13(4): 851-861. https://doi.org/10.12677/gser.2024.134081

参考文献

[1] Wei, W., Zhang, R., Wen, M. and Yang, S. (2017) Relationship between the Asian Westerly Jet Stream and Summer Rainfall over Central Asia and North China: Roles of the Indian Monsoon and the South Asian High. Journal of Climate, 30, 537-552. [Google Scholar] [CrossRef
[2] Li, X., Wen, Z. and Huang, W. (2020) Modulation of South Asian Jet Wave Train on the Extreme Winter Precipitation over Southeast China: Comparison between 2015/16 and 2018/19. Journal of Climate, 33, 4065-4081. [Google Scholar] [CrossRef
[3] Krishnamurti, T.N. (1961) The Subtropical Jet Stream of Winter. Journal of Meteorology, 18, 172-191. [Google Scholar] [CrossRef
[4] Liu, Y., Hu, Z., Wu, R., Jha, B., Li, Q., Chen, L., et al. (2021) Subseasonal Prediction and Predictability of Summer Rainfall over Eastern China in BCC_AGCM2.2. Climate Dynamics, 56, 2057-2069. [Google Scholar] [CrossRef
[5] Lee, S. and Kim, H. (2003) The Dynamical Relationship between Subtropical and Eddy-Driven Jets. Journal of the Atmospheric Sciences, 60, 1490-1503. [Google Scholar] [CrossRef
[6] Yang, S., Lau, K., Yoo, S., Kinter, J.L., Miyakoda, K. and Ho, C. (2004) Upstream Subtropical Signals Preceding the Asian Summer Monsoon Circulation. Journal of Climate, 17, 4213-4229. [Google Scholar] [CrossRef
[7] 吴玲玲, 段俊毅. 冬季中东急流中心位置的年际变化及其与大气环流的联系[J]. 大气科学学报, 2022, 45(1): 65-75.
[8] 倪东鸿, 孙照渤, 李忠贤, 等. 冬季中东急流与中国气候异常的联系[J]. 气象科学, 2010, 30(3): 301-307.
[9] 倪东鸿, 孙照渤, 李忠贤, 等. 冬季中东急流时空变化特征及其与中国气候的关系[J]. 解放军理工大学学报(自然科学版), 2010, 11(3): 354-359.
[10] Yan, M., Liu, Z.Y., Ning, L. and Liu, J. (2020) Holocene EASM‐EAWM Relationship across Different Timescales in CCSM3. Geophysical Research Letters, 47, e2020GL088451. [Google Scholar] [CrossRef
[11] 王远皓, 陈文, 张井勇. 东亚中纬度干旱/半干旱区降水年际变化及其可能成因[J]. 气候与环境研究, 2012, 17(4): 444-456.
[12] Mohtadi, M., Oppo, D.W., Steinke, S., Stuut, J.W., De Pol-Holz, R., Hebbeln, D., et al. (2011) Glacial to Holocene Swings of the Australian-Indonesian Monsoon. Nature Geoscience, 4, 540-544. [Google Scholar] [CrossRef
[13] 马萌萌, 左洪超, 李立程, 等. 青藏高原夏季风和北半球夏季季节内振荡对中国西南地区雨季旱涝的影响及协同作用[J]. 干旱气象, 2022, 40(4): 577-588.
[14] 陈乾金, 高波, 张强. 青藏高原冬季雪盖异常与冬夏季风变异及其相互联系的物理诊断研究[J]. 大气科学, 2000, 24(4): 477-492.
[15] 姚杰, 温琴, 沈星辰, 等. 青藏高原对全球大气温度和水汽分布的影响[J]. 北京大学学报(自然科学版), 2018, 54(6): 1179-1185.
[16] 陈诚, 牛涛, 陆尔. 喀拉海和巴伦支海海冰对中高纬异常纬向环流暨中国东部重霾天气形成的作用[J]. 大气科学学报, 2019, 42(2): 267-279.
[17] 武炳义, 黄荣辉, 高登义. 冬季北极喀拉海、巴伦支海海冰面积变化对东亚冬季风的影响[J]. 大气科学, 1999, 23(3): 9.
[18] 段安民, 肖志祥, 王子谦. 青藏高原冬春积雪和地表热源影响亚洲夏季风的研究进展[J]. 大气科学, 2018, 42(4): 755-766.
[19] Kanamitsu, M., Ebisuzaki, W., Woollen, J., Yang, S., Hnilo, J.J., Fiorino, M., et al. (2002) NCEP-DOE AMIP-II Reanalysis (R-2). Bulletin of the American Meteorological Society, 83, 1631-1644. [Google Scholar] [CrossRef
[20] Adler, R.F., Huffman, G.J., Chang, A., Ferraro, R., Xie, P., Janowiak, J., et al. (2003) The Version-2 Global Precipitation Climatology Project (GPCP) Monthly Precipitation Analysis (1979-Present). Journal of Hydrometeorology, 4, 1147-1167. [Google Scholar] [CrossRef
[21] 任建成, 王峰, 卢晓宁. 基于EOF和小波分析的山东省年降水时空变化特征[J]. 水土保持研究, 2022, 29(2): 179-183.
[22] Wei, W., Ren, Q., Lu, M. and Yang, S. (2022) Zonal Extension of the Middle East Jet Stream and Its Influence on the Asian Monsoon. Journal of Climate, 35, 4741-4751. [Google Scholar] [CrossRef