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宋燕, 季劲钧, 孙丹. 20世纪60年代中期亚非夏季风减弱的全球气候背景异常分析[J]. 大气科学, 2009, 33(2): 313-324. DOI: 10.3878/j.issn.1006-9895.2009.02.10
引用本文: 宋燕, 季劲钧, 孙丹. 20世纪60年代中期亚非夏季风减弱的全球气候背景异常分析[J]. 大气科学, 2009, 33(2): 313-324. DOI: 10.3878/j.issn.1006-9895.2009.02.10
SONG Yan, JI Jinjun, SUN Dan. Global Climatic Anomalous Background Analyses of the Asian-African Summer Monsoon Weakening in the Mid-1960s[J]. Chinese Journal of Atmospheric Sciences, 2009, 33(2): 313-324. DOI: 10.3878/j.issn.1006-9895.2009.02.10
Citation: SONG Yan, JI Jinjun, SUN Dan. Global Climatic Anomalous Background Analyses of the Asian-African Summer Monsoon Weakening in the Mid-1960s[J]. Chinese Journal of Atmospheric Sciences, 2009, 33(2): 313-324. DOI: 10.3878/j.issn.1006-9895.2009.02.10

20世纪60年代中期亚非夏季风减弱的全球气候背景异常分析

Global Climatic Anomalous Background Analyses of the Asian-African Summer Monsoon Weakening in the Mid-1960s

  • 摘要: 利用美国NASA格点月降水总量资料、美国CO2信息分析中心地表面温度异常月平均网格点资料、美国NCEP/NCAR再分析全球网格点资料和兰州高原大气物理研究所的台站地温观测资料分析了1960年代中期亚非夏季风环流圈年代际时间尺度的减弱及其与之有关的全球气候场异常现象。结果发现, 1960年代中期全球对流层大气温度和海洋温度场发生异常变化, 对流层大气有明显降温, 海洋主要以印度洋升温、 北太平洋和北大西洋降温为主要特征, 同时, 我国大陆土壤温度和青藏高原温度在1960年代中期有明显的下降, 导致亚洲大陆与印度洋之间的热力对比明显减弱, 东风急流减弱, 最终导致亚非夏季风明显减弱。

     

    Abstract: Based on the American NASA monthly precipitation grid data, the monthly mean surface temperature anomalies grid data from the CO2 Information Analyses Centre, USA, the NCEP/NCAR reanalysis global grid data and the stations observational soil temperature data from the Cold and Arid Regions Environmental and Engineering Research Institute of the Chinese Academy of Sciences, the authors study the Asian-African summer monsoon meridional circulation weakening in the mid-1960s on interdecadal time scale and the related global climatic anomalies phenomena. The results show that the tropospheric temperature reduced obviously and the global oceanic temperature abnormal changes in the mid-1960s are mainly characterized by SST increasing in the Indian Ocean and SST decreasing in the northern Pacific Ocean and the northern Atlantic Ocean. Simultaneously, the soil temperatures at 1.6-m and 3.2-m depths in Chinese continent and the surface temperature in the Tibetan Plateau decreased respectively and remarkably in the mid-1960s, which reduces the thermal contrast between Asian continent and the Indian Ocean. Accordingly, the easterly jet weakened, finally the Asian-African summer monsoon weakened too and the monsoon meridional circulation weakened obviously.

     

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