It is found that waters within 5°S-5°N,60°-75°E are the key areas of sea surface temperature anomaly(SSTA) that affect the winter temperature of these regions from Apri.

The composites for circulation anomaly and sea surface temperature anomaly(SSTA) show that both the low .

More attention was paid on studying the relationship between sea surface temperature anomaly (SSTA) over the north Pacific and summer precipitation anomaly in North China and an AGCM was utilized to con.

The important effects of SST(SST heating and SST anomaly) on low-frequency oscillation systems in tropics are studied by baroclinic equation groups for the characteristics of strong evaporation,convergence ascending and SST anomaly in the tropics.

In order to study the effects of SST anomaly in tropical western Pacific during winter and spring on the early summer monsoon in East Asia, a set of numerical experiments is conducted using OSU AGCM.

Using a primitive equation model with a spheric band domain,a numerical study iscarried out of the effect on rainfall of 1991 Pacific SST anomaly in the leading region with theaffecting mechanisms investigated.

ANOMALIES OF THE NORTHEAST CHINA FLOODS SEASON PRECIPITATION AND SVD ANALYSIS WITH SSTA IN WORLD OCEANS;

Mechanism for SSTA Impact on Summer Rainfall in North China;

Relationship of the SSTA Temporal Variation in the Middle and East Equatorial Pacific in Spring and Summer to East Asia Summer Monsoon;

Waters bounded by 9-1°S, 121-129°E are the key zones of SST anomalies that affect the precipitation in these regions over May - July in preceding years.

In 1985, negative sea surface temperature anomalies(SSTA) distributed in the eastern equatorial Pacific broadly, and positive SSTA which were about 0.

By using the atmosphere-land coupled model IAP9L_CoLM of the Institute of Atmospheric Physics,Chinese Academy of Sciences,the imapct of sea surface temperature anomalies(SSTAs) in different ocean basins on the extreme climate events affecting Southern China during January 2008 has been investigated through four sets of ensemble numerical simulations.