A new East Asian subtropical summer monsoon circulation index is defined, where the barotropic and baroclinic components of circulation are included. Results show that this index can well indicate the interannual vari...A new East Asian subtropical summer monsoon circulation index is defined, where the barotropic and baroclinic components of circulation are included. Results show that this index can well indicate the interannual variability of summer precipitation and temperature anomalies in China. A strong monsoon is characterized by more rainfall in the Yellow River basin and northern China, less rainfall in the Yangtze River basin, and more rainfall in south and southeast China, in association with higher temperature in most areas of China. Furthermore, comparison is made between the index proposed in this paper and other monsoon indexes in representing climate anomalies in China.展开更多
From the point of view of atmospheric science and oceanography, the author explores the origin of abnormal climatic phenomena of El Nino and La Nina, the interaction between the two and their influence on climatic ano...From the point of view of atmospheric science and oceanography, the author explores the origin of abnormal climatic phenomena of El Nino and La Nina, the interaction between the two and their influence on climatic anomalies in China in general, and on precipitation in the Yangtze River Valley in particular.展开更多
The interdecadal change of the relationship between the tropical Indian Ocean dipole（IOD） mode and the summer climate anomaly in China is investigated by using monthly precipitation and temperature records at 210 st...The interdecadal change of the relationship between the tropical Indian Ocean dipole（IOD） mode and the summer climate anomaly in China is investigated by using monthly precipitation and temperature records at 210 stations in China and the NCEP/NCAR reanalysis data for 1957-2005.The results indicate that along with the interdecadal shift in the large-scale general circulation around the late 1970s,the relationship between the IOD mode and the summer climate anomaly in some regions of China has significantly changed.Before the late 1970s,a developing IOD event is associated with an enhanced East Asian summer monsoon,which tends to decrease summer precipitation and increase summer temperature in South China;while after the late 1970s,it is associated with a weakened East Asian summer monsoon,which tends to increase（decrease） precipitation and decrease（increase） temperature in the south（north） of the Yangtze River.During the next summer,following a positive IOD event,precipitation is increased in most of China before the late 1970s,while it is decreased（increased） south（north） of the Yangtze River after the late 1970s.There is no significant correlation between the IOD and surface air temperature anomaly in most of China in the next summer before the late 1970s;however,the IOD tends to increase the next summer temperature south of the Yellow River after the late 1970s.展开更多
基金Key Laboratory of Meteorological Disaster of Jiangsu Province (KLME060210)
文摘A new East Asian subtropical summer monsoon circulation index is defined, where the barotropic and baroclinic components of circulation are included. Results show that this index can well indicate the interannual variability of summer precipitation and temperature anomalies in China. A strong monsoon is characterized by more rainfall in the Yellow River basin and northern China, less rainfall in the Yangtze River basin, and more rainfall in south and southeast China, in association with higher temperature in most areas of China. Furthermore, comparison is made between the index proposed in this paper and other monsoon indexes in representing climate anomalies in China.
文摘From the point of view of atmospheric science and oceanography, the author explores the origin of abnormal climatic phenomena of El Nino and La Nina, the interaction between the two and their influence on climatic anomalies in China in general, and on precipitation in the Yangtze River Valley in particular.
基金Supported by the National Natural Science Foundation of China under Grant Nos. 40730953, 40523001, and 40905036,National Public Welfare Research Fund of China under Grant Nos. GYHY200706005 and GYHY200806004
文摘The interdecadal change of the relationship between the tropical Indian Ocean dipole（IOD） mode and the summer climate anomaly in China is investigated by using monthly precipitation and temperature records at 210 stations in China and the NCEP/NCAR reanalysis data for 1957-2005.The results indicate that along with the interdecadal shift in the large-scale general circulation around the late 1970s,the relationship between the IOD mode and the summer climate anomaly in some regions of China has significantly changed.Before the late 1970s,a developing IOD event is associated with an enhanced East Asian summer monsoon,which tends to decrease summer precipitation and increase summer temperature in South China;while after the late 1970s,it is associated with a weakened East Asian summer monsoon,which tends to increase（decrease） precipitation and decrease（increase） temperature in the south（north） of the Yangtze River.During the next summer,following a positive IOD event,precipitation is increased in most of China before the late 1970s,while it is decreased（increased） south（north） of the Yangtze River after the late 1970s.There is no significant correlation between the IOD and surface air temperature anomaly in most of China in the next summer before the late 1970s;however,the IOD tends to increase the next summer temperature south of the Yellow River after the late 1970s.
