The 1997/98 ENSO cycle and its impact on summer climate anomalies in East Asia

The observed data of the sea surface temperature (SST) anomalies and the se a temperature (ST) in the sub-layer of the equatorial Pacific, the NCEP/NCA R reanalysis data and the data set of daily precipitation in China are used to analyze the characteristics of the 1997/98 ENSO cycle and its impact on summer climate anomalies in East Asia. The results show that the 1997/98 E NSO cycle, the strongest one in the 20th century, might be characterized by rapid development and decay and eastward propagation from the West Pacific warm pool Influenced by the ENSO cycle, in 1997, the serious drought and h ot summer occurred in North China, and in the summer of 1998, the severe fl oods occurred in the Yangtze River valley, especially in the Dongting Lake and Boyang Lake valleys, South Korea and Japan. The analysis also shows that: influenced by the 1997/98 ENSO cycle, the wat er vapor transportation by the Asian monsoon in the summer of 1997 was very different from that in the summer of 1998, In the summer of 1997, the wate r vapor transportation by the Asian summer monsoon was weak in North China and the northern part of the Korea Peninsula. Thus, it caused the drought a nd hot summer in North China. However, in the summer of 1998, the sea tempe rature in the sub-layer of the West Pacific warm pool dropped, the western Pacific subtropical high shifted southward. Thus, a large amount of water v apor was transported from the Bay of Bengal, the South China Sea and the tr opical western Pacific into the Yangtze River valley of China, South Korea and Japan, and the severe flood occurred there.