作者: Chia Chou , Jien-Yi Tu , Jia-Yuh Yu
DOI: 10.1175/2761.1
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摘要: Abstract The interannual variability of the western North Pacific (WNP) summer monsoon is examined for non-ENSO, ENSO developing, and decaying years, respectively. developing (decaying) year defined as before (after) mature phase ENSO, non-ENSO that neither nor year. A strong (weak) WNP tends to occur during El Nino (La Nina) a weak (strong) In all associated with positive (negative) rainfall anomalies, cold (warm) sea surface temperature warm (cold) upper-tropospheric low (high) pressure low-level cyclonic (anticyclonic) circulation anomaly over subtropical WNP. 850-hPa wave train east...