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
利用NCEP/NCAR的1950—1998年海表温度场和1958—1997年海表风场再分析资料,采用相关、合成等分析方法,研究了黑潮区域SSTA(sea surface temperature anomaly)与太平洋风场的关系。结果表明:从SSTA滞后风场3月起,与其关系密切的经向风...利用NCEP/NCAR的1950—1998年海表温度场和1958—1997年海表风场再分析资料,采用相关、合成等分析方法,研究了黑潮区域SSTA(sea surface temperature anomaly)与太平洋风场的关系。结果表明:从SSTA滞后风场3月起,与其关系密切的经向风关键区位于赤道西太平洋(140~160°E,5°S^5°N),纬向风关键区位于赤道中太平洋(160°E^150°W,5°S^5°N),两者对SSTA的影响均可持续6月左右;纬向风关键区的强度和范围均大于经向风。进一步研究表明,黑潮SS-TA与ENSO事件有着密切的联系:E l N ino(La N ina)事件当年11月—次年12月期间黑潮海温多为正(负)异常。展开更多
The present study investigates the persistence of summer sea surface temperature anomalies（SSTAs） in the midlatitude North Pacific and its interdecadal variability. Summer SSTAs can persist for a long time（approxim...The present study investigates the persistence of summer sea surface temperature anomalies（SSTAs） in the midlatitude North Pacific and its interdecadal variability. Summer SSTAs can persist for a long time（approximately 8–14 months）around the Kuroshio Extension（KE） region. This long persistence may be strongly related to atmospheric forcing because the mixed layer is too shallow in the summer to be influenced by the anomalies at depths in the ocean. Changes in atmospheric circulation, latent heat flux, and longwave radiation flux all contribute to the long persistence of summer SSTAs. Among these factors, the longwave radiation flux has a dominant influence. The effects of sensible heat flux and shortwave radiation flux anomalies are not significant. The persistence of summer SSTAs displays pronounced interdecadal variability around the KE region, and the variability is very weak during 1950–82 but becomes stronger during 1983–2016. The changes in atmospheric circulation, latent heat flux, and longwave radiation flux are also responsible for this interdecadal variability because their forcings on the summer SSTAs are sustained for much longer after 1982.展开更多
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.
文摘利用NCEP/NCAR的1950—1998年海表温度场和1958—1997年海表风场再分析资料,采用相关、合成等分析方法,研究了黑潮区域SSTA(sea surface temperature anomaly)与太平洋风场的关系。结果表明:从SSTA滞后风场3月起,与其关系密切的经向风关键区位于赤道西太平洋(140~160°E,5°S^5°N),纬向风关键区位于赤道中太平洋(160°E^150°W,5°S^5°N),两者对SSTA的影响均可持续6月左右;纬向风关键区的强度和范围均大于经向风。进一步研究表明,黑潮SS-TA与ENSO事件有着密切的联系:E l N ino(La N ina)事件当年11月—次年12月期间黑潮海温多为正(负)异常。
基金supported by the National Natural Science Foundation of China (NSFC) (Grant Nos. 41375094 and 41406028)the Basic Scientific Research Fund for National Public Institutes of China (Grant No. GY0215P04)+2 种基金the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No. XDA11010102)the NSFC–Shandong Joint Fund for Marine Science Research Centers (Grant No. U1406401)the Foundation for Innovative Research Groups of the NSFC (Grant No. 41421005)
文摘The present study investigates the persistence of summer sea surface temperature anomalies（SSTAs） in the midlatitude North Pacific and its interdecadal variability. Summer SSTAs can persist for a long time（approximately 8–14 months）around the Kuroshio Extension（KE） region. This long persistence may be strongly related to atmospheric forcing because the mixed layer is too shallow in the summer to be influenced by the anomalies at depths in the ocean. Changes in atmospheric circulation, latent heat flux, and longwave radiation flux all contribute to the long persistence of summer SSTAs. Among these factors, the longwave radiation flux has a dominant influence. The effects of sensible heat flux and shortwave radiation flux anomalies are not significant. The persistence of summer SSTAs displays pronounced interdecadal variability around the KE region, and the variability is very weak during 1950–82 but becomes stronger during 1983–2016. The changes in atmospheric circulation, latent heat flux, and longwave radiation flux are also responsible for this interdecadal variability because their forcings on the summer SSTAs are sustained for much longer after 1982.
