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
Air mass is inter-hemispherically redistributed, leading to an interesting phenomenon known as the Inter-Hemispheric Oscillation （IHO）. In the present article, the seasonality of the interannual IHO has been examine...Air mass is inter-hemispherically redistributed, leading to an interesting phenomenon known as the Inter-Hemispheric Oscillation （IHO）. In the present article, the seasonality of the interannual IHO has been examined by employing monthly mean reanalyses from NCEP/NCAR, EAR40, and JRA25 for the period of 1958–2006. It is found that the IHO indices as calculated from different reanalyses are generally consistent with each other. A distinct seesaw structure in all four seasons between the northern and southern hemispheres is observed as the IHO signature in both the surface air pressure anomalies （SAPAs） and the leading EOF component of the anomalous zonal mean quantities. When the SAPAs are positive （negative） in the northern hemisphere, they are negative （positive） in the southern hemisphere. Large values of SAPAs are usually observed in mid- and high-latitude areas in all but the solstice seasons. In boreal summer and winter, relatively stronger perturbations of IHO-related SAPA are found in the Asian monsoon region, which shows a large difference from the status in boreal spring and fall. This suggests that seasonal mean monsoon activity is globally linked via air mass redistribution globally on interannual timescales, showing a very interesting linkage between monsoons and the IHO in the global domain. In all seasons, large values of SAPA always exist over the Antarctic and the surrounding regions, implying a close relation with Antarctic oscillations.展开更多
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 jointlyby the National Key Technology R&D Program (GrantNo. 2007BAC29B02)the National Natural Science Foundation of China (NSFC, Grant No. 40675025)the Key Laboratory of Meteorological Disasters, Nanjing University of Information Science & Technology (NUIST,KLME060101)
文摘Air mass is inter-hemispherically redistributed, leading to an interesting phenomenon known as the Inter-Hemispheric Oscillation （IHO）. In the present article, the seasonality of the interannual IHO has been examined by employing monthly mean reanalyses from NCEP/NCAR, EAR40, and JRA25 for the period of 1958–2006. It is found that the IHO indices as calculated from different reanalyses are generally consistent with each other. A distinct seesaw structure in all four seasons between the northern and southern hemispheres is observed as the IHO signature in both the surface air pressure anomalies （SAPAs） and the leading EOF component of the anomalous zonal mean quantities. When the SAPAs are positive （negative） in the northern hemisphere, they are negative （positive） in the southern hemisphere. Large values of SAPAs are usually observed in mid- and high-latitude areas in all but the solstice seasons. In boreal summer and winter, relatively stronger perturbations of IHO-related SAPA are found in the Asian monsoon region, which shows a large difference from the status in boreal spring and fall. This suggests that seasonal mean monsoon activity is globally linked via air mass redistribution globally on interannual timescales, showing a very interesting linkage between monsoons and the IHO in the global domain. In all seasons, large values of SAPA always exist over the Antarctic and the surrounding regions, implying a close relation with Antarctic oscillations.
