Based on an observational analysis, seven numerical experiments are designed to study the impacts of Pacific SSTA on summer precipitation over eastern China and relevant physical mechanism by NCAR CCM3. The numerical ...Based on an observational analysis, seven numerical experiments are designed to study the impacts of Pacific SSTA on summer precipitation over eastern China and relevant physical mechanism by NCAR CCM3. The numerical simulation results show that preceding winter SSTA in the Kuroshio region leads to summer precipitation anomaly over the Yangtze River valleys by modifying atmospheric general circulation over eastern Asia and middle-high latitude. West Pacific subtropical high is notably affected by preceding spring SSTA over the middle and east of Equator Pacific; SSTA of the central region of middle latitude in the corresponding period causes the summer rainfall anomaly over eastern China so as to trigger the atmospheric Eurasia-Pacific teleconnection pattern.展开更多
Sea surface temperature anomaly (SSTA) exerts great influence on the generation of global weather and climate. Much progress has been made with respect to SSTA in the Pacific Ocean region in contrast to the Indian Oce...Sea surface temperature anomaly (SSTA) exerts great influence on the generation of global weather and climate. Much progress has been made with respect to SSTA in the Pacific Ocean region in contrast to the Indian Ocean. The IAP9L model, which is developed at the Institute of Atmospheric Physics of the Chinese Academy of Science, is used to simulate the influence of the Indian Ocean SSTA on the general circulation and weather/climate anomalies in the monsoon region of Asia. It is found that the warm (cool) SSTA in the equatorial low latitudes of the Indian Ocean triggers winter (summer) teleconnection patterns in middle and higher latitudes of the Northern Hemisphere that are similar to PNA or EAP. They play a very important role in the anomaly of circulation or weather and climate in the middle and lower latitudes of the Asian summer monsoon region. With the warm (cool) SSTA forcing in the Indian Ocean, the Asian summer monsoon sets up at a late (early) date and withdraws at a early (late) date, lasting for a short (long) duration at a weak (strong) intensity. The Indian Ocean SSTA is shown to be an indicator for precipitation variation in China.展开更多
The relationship of Kuroshio sea surface temperature anomaly (SSTA) in theprevious winter and summer rainfall in China was analyzed based on observational studies andnumerical simulations. Observational results indica...The relationship of Kuroshio sea surface temperature anomaly (SSTA) in theprevious winter and summer rainfall in China was analyzed based on observational studies andnumerical simulations. Observational results indicate that there is a close relation betweenKuroshio SSTA and precipitation in China. When Kuroshio SSTA is positive, the western Pacificsubtropical high will be stronger and extend farther westward in, the following summer, with Asiansummer monsoon weaker and the frontal precipitation further southward. As a result, summerprecipitation increases (decreases) in the mid-lower reaches of the Yangtze River (in North andNortheast China), and vice versa. Conclusions drawn by NCAR-CCM3 testify the observational results.展开更多
基金Natural Science Foundation of China(40331010)Study Project of Jiangsu Key Laboratoryof Meteorological Disaster (KLME050304)
文摘Based on an observational analysis, seven numerical experiments are designed to study the impacts of Pacific SSTA on summer precipitation over eastern China and relevant physical mechanism by NCAR CCM3. The numerical simulation results show that preceding winter SSTA in the Kuroshio region leads to summer precipitation anomaly over the Yangtze River valleys by modifying atmospheric general circulation over eastern Asia and middle-high latitude. West Pacific subtropical high is notably affected by preceding spring SSTA over the middle and east of Equator Pacific; SSTA of the central region of middle latitude in the corresponding period causes the summer rainfall anomaly over eastern China so as to trigger the atmospheric Eurasia-Pacific teleconnection pattern.
基金Applied Foundation of Science and Technology Committee of Yunnan Province(97D033Q)and LASG
文摘Sea surface temperature anomaly (SSTA) exerts great influence on the generation of global weather and climate. Much progress has been made with respect to SSTA in the Pacific Ocean region in contrast to the Indian Ocean. The IAP9L model, which is developed at the Institute of Atmospheric Physics of the Chinese Academy of Science, is used to simulate the influence of the Indian Ocean SSTA on the general circulation and weather/climate anomalies in the monsoon region of Asia. It is found that the warm (cool) SSTA in the equatorial low latitudes of the Indian Ocean triggers winter (summer) teleconnection patterns in middle and higher latitudes of the Northern Hemisphere that are similar to PNA or EAP. They play a very important role in the anomaly of circulation or weather and climate in the middle and lower latitudes of the Asian summer monsoon region. With the warm (cool) SSTA forcing in the Indian Ocean, the Asian summer monsoon sets up at a late (early) date and withdraws at a early (late) date, lasting for a short (long) duration at a weak (strong) intensity. The Indian Ocean SSTA is shown to be an indicator for precipitation variation in China.
基金This study is supported by the National Natural Science Foundation of China under No. Grant 40175023 and by the GradateEducation and Innovation Project of Jiangsu Province: No. E30000008098-2.
文摘The relationship of Kuroshio sea surface temperature anomaly (SSTA) in theprevious winter and summer rainfall in China was analyzed based on observational studies andnumerical simulations. Observational results indicate that there is a close relation betweenKuroshio SSTA and precipitation in China. When Kuroshio SSTA is positive, the western Pacificsubtropical high will be stronger and extend farther westward in, the following summer, with Asiansummer monsoon weaker and the frontal precipitation further southward. As a result, summerprecipitation increases (decreases) in the mid-lower reaches of the Yangtze River (in North andNortheast China), and vice versa. Conclusions drawn by NCAR-CCM3 testify the observational results.
