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《Chinese Journal of Atmospheric Sciences》 1987-04
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RELATIONSHIP BETWEEN THE KEY REGION SST OF THE TROPICAL EASTERN PACIFIC AND AIR TEMPERATURE OF NORTHEAST CHINA

Zeng Zhaomei Zhang Mingli(Institite of Atmospheric Physics,Academia Sinica)  
The occurrence of serious cold summer in northeast China is well consistent with the appearance of the El Nino event in the Eastern Equatorial Pacific during the last thirty years (1951-1980). The teleconnection is analyzed and it is found that the SST anomalies in the low level have an effect on the large-scale atmospheric circulation anomalies, transfer the effect to the midlatitude area and cause temperature anomalies in northeast China during the El Nino event. At the same time, the "Walker cell" shifts eastward while an upper troposphere easterly wind and anticyclone cell strengthen over the tropical central and Western Pacific. But the South-Asia anticyclone (Tibetan High) is weak and farther to the south, the westerly belt along the Asia coast is also farther to the south. The cold air is more active than normal. Then the low temperature phenomenon in the most part of this area appears.
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