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This study examined the relationship between mature phase of the cold event in 1999 and the East Asian summer atmosphere circulation in 2000.The cold event reaches its mature phase in the autumn and winter of 1999,which is the strongest La Nina episode in recent 11 years.There is a clear anomalous pattern of the atmosphere circulation around East Asia in the summer of 2000, i.e.the negative anomaly centers around the Cherski Mountains and 20°N,170°E at 500 hPa,the main body of the subtropical high keeps in further northern position than usual and the negative anomaly of precipitation located in southern central China.This pattern is thought as the response to the preceding strong cold event in autumn of 1999.It is also identified that the response of the East Asian atmosphere circulation in summer of 2000 to the strong La Nina event in 1999 belongs to the top rank in recent 43 years.On the other hand,the inactive blocking anticyclone around East Asia in summer of 2000 is associated with the positive SST anomaly and the 850 hPa temperature anomaly around the Bering Sea simultaneously.Nevertheless,although the impact on the summer atmosphere circulation around East Asia from La Nina events could not rank with that from E1 Nino,the impact could not be neglected especially in a strong La Nina case.
This study examined the relationship between mature phase of the cold event in 1999 and the East Asian summer atmosphere circulation in 2000. The cold event reaches its mature phase in the autumn and winter of 1999, which is the strongest La Nina episode in recent 11 years .here is a clear anomalous pattern of the atmosphere once around East Asia in the summer of 2000, iethe negative anomaly centers around the Cherski Mountains and 20 ° N, 170 ° E at 500 hPa, the main body of the subtropical high keeps in further northern position than usual and the negative anomaly of precipitation located in southern central China.This pattern is thought as the response to the ago strong strong event in autumn of 1999.It is also identified that the response of the East Asian atmosphere circulation in summer of 2000 to the strong La Nina event in 1999 belongs to the top rank in recent 43 years.On the other hand, the inactive blocking anticyclone around East Asia in summer of 2000 is associated w ith the positive SST anomaly and the 850 hPa temperature anomaly around the Bering Sea simultaneously. However, although the impact on the summer of East Asia from La Nina events could not rank with that from E1 Nino, the impact could not be neglected especially in a strong La Nina case.