Wang Huijun. 2002: The Instability of the East Asian Summer Monsoom-ENSO Relations. Adv. Atmos. Sci, 19(1): 1-11., https://doi.org/10.1007/s00376-002-0029-5
Citation: Wang Huijun. 2002: The Instability of the East Asian Summer Monsoom-ENSO Relations. Adv. Atmos. Sci, 19(1): 1-11., https://doi.org/10.1007/s00376-002-0029-5

The Instability of the East Asian Summer Monsoom-ENSO Relations

  • The instability in the relation between the East Asian summer monsoon and the ENSO cycle in the long-term variation is found through this research. By instability, we mean that high inter-relation exists in some periods but low inter-relation may appear in some other periods. It is reveals that the interannual variation of the summer atmospheric circulation during the high correlation periods (HCP) is significantly different from that during the low correlation' periods (LCP).Larger interannual variability is found during HCP for trade wind over the tropical eastern Pacific of the Southern Hemisphere, the low-level air temperature over the tropical Pacific, the subtropical high pressure systems in the two hemispheres, and so on. The correlation between summer rainfall over China and ENSO is as well different between HCP and LCP.
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