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摘要
The summer precipitation anomalies over the tropical western North Pacific (WNP), which greatly affect East Asian climate, are closely related to Indian Ocean (IO) SST anomalies, and this WNP-IO relationship is widely assumed to be linear. This study indicates that the IO SST-WNP precipitation relationship is generally linear only when the IO SST anomalies are positive and not when the IO SST anomalies are negative, that is, a strongly cooler IO, in comparison with a moderately cooler IO, does not correspond to stronger precipitation enhancement over the WNP. Further analysis suggests that the phases of ENSO play a crucial role in modifying the impacts of IO SSTs on WNP anomalies. The reverse IO SST-WNP precipitation relationship, which exists without apparent ENSO development/decay, is intensified by El Nino decay through the enhancement of IO SST anomalies, but weakened by El Nino development and La Nina decay through the concurrence of SST anomalies in the tropical central and eastern Pacific. After removing El Nino developing and La Nina decaying cases, the IO SST and WNP precipitation anomalies show a clear linear relationship. Because of the effects of the phases of ENSO, the years of negative precipitation or anticyclonic anomalies over the WNP are highly concentrated over strongly warmer IO and El Nino decaying years, which is consistent with previous studies. However, the years of positive precipitation anomalies are scattered over cooler IO and moderately warmer IO years, implying a complexity of tropical SST forcing on positive WNP precipitation anomalies.
- 出版日期2015-2
- 单位中国科学院大学; 中国科学院大气物理研究所
