Using the daily and monthly data of surface air pressure, meridional wind, radiation and water vapor from NCEP/NCAR reanalysis for the period of 1979―2006, we have examined the seasonal variations of the interhemisph...Using the daily and monthly data of surface air pressure, meridional wind, radiation and water vapor from NCEP/NCAR reanalysis for the period of 1979―2006, we have examined the seasonal variations of the interhemispheric oscillations (IHO) in mass field of the global atmosphere. Our results have demonstrated that IHO as observed in surface air pressure field shows the distinct seasonal cycle. This seasonal cycle has an interhemispheric seesaw structure with comparable annual ranges of surface air pressure in the Southern and Northern Hemispheres. Mass of water vapor changes out-of-phase between the Southern and Northern Hemispheres, showing clearly a seasonal cycle with its annual range almost equivalent to annual range of the IHO seasonal cycle. Amazingly, the cross-equatorial flow is found to be induced by annual changes in water vapor mass as a response of the atmosphere to seasonal cycle of forcing from hemispheric net surface short- and long-wave radiations. The IHO seasonality exhibits its larger variations in magnitude in mid-latitudes other than in other regions of the globe. Additionally, our results also show that the global air mass is redistributed seasonally not only between the Northern and Southern Hemispheres but also between land and sea. This land-sea air mass redis- tribution induces a zonal pattern of surface air pressure in the Northern Hemisphere but the meridional pattern in the Southern Hemisphere.展开更多
南北两半球大气中高纬度之间的相互作用与季风等跨半球的天气气候系统存在着密切联系,由于涉及全球范围的大尺度环流与能量变化,其联系途径与机理受到学者们的广泛关注。本文结合ERA5再分析资料以及CMIP6中MPI-ESM1-2-HR模式历史输出资...南北两半球大气中高纬度之间的相互作用与季风等跨半球的天气气候系统存在着密切联系,由于涉及全球范围的大尺度环流与能量变化,其联系途径与机理受到学者们的广泛关注。本文结合ERA5再分析资料以及CMIP6中MPI-ESM1-2-HR模式历史输出资料,验证了冬季南北半球际大气质量涛动(Inter-Hemispheric atmospheric mass Oscillation, IHO)与东亚冬季风异常的联系及其对中国冬季气温的影响。研究表明,再分析资料以及模式结果均表明冬季IHO与东亚冬季风存在显著的正相关关系。IHO通过全球大气质量再分配与东亚冬季风建立起紧密的联系。当IHO为正位相时,大气质量在欧亚大陆北部异常堆积,而在中低纬地区异常亏损,这使得东亚地区海陆气压差明显增大,冬季风增强,同时对中国华中地区冬季地表气温具有显著影响;反之亦然。进一步分析发现,热带低平流层气温可以通过剩余环流调节臭氧含量经向分布进而影响南极对流层气温,从而对IHO年际变化起主要的驱动作用。展开更多
本研究确定了某激光粉尘仪测试上海市环境大气颗粒物(PM10和PM2.5)的质量浓度转换系数K值。利用激光粉尘仪和TEOM RP 1400a型监测仪,同时对选定的环境监测站同一监测点的环境大气颗粒物(PM10和PM2.5)进行了测定,得出了该激光粉尘仪测试...本研究确定了某激光粉尘仪测试上海市环境大气颗粒物(PM10和PM2.5)的质量浓度转换系数K值。利用激光粉尘仪和TEOM RP 1400a型监测仪,同时对选定的环境监测站同一监测点的环境大气颗粒物(PM10和PM2.5)进行了测定,得出了该激光粉尘仪测试上海市环境大气颗粒物(PM10和PM2.5)的质量浓度转换系数K值呈基本正态分布,分别为0.00594和0.00158。展开更多
基金the National Natural Science Foundation of China (Grant No. 40675025)the Project of National Key Basic Research Development (Grant No. 2004CB418302)the Key Lab of Meteorological Disasters (KLME) of Nanjing University of Information Science and Technology (NUIST) (Grant No. KLME060101)
文摘Using the daily and monthly data of surface air pressure, meridional wind, radiation and water vapor from NCEP/NCAR reanalysis for the period of 1979―2006, we have examined the seasonal variations of the interhemispheric oscillations (IHO) in mass field of the global atmosphere. Our results have demonstrated that IHO as observed in surface air pressure field shows the distinct seasonal cycle. This seasonal cycle has an interhemispheric seesaw structure with comparable annual ranges of surface air pressure in the Southern and Northern Hemispheres. Mass of water vapor changes out-of-phase between the Southern and Northern Hemispheres, showing clearly a seasonal cycle with its annual range almost equivalent to annual range of the IHO seasonal cycle. Amazingly, the cross-equatorial flow is found to be induced by annual changes in water vapor mass as a response of the atmosphere to seasonal cycle of forcing from hemispheric net surface short- and long-wave radiations. The IHO seasonality exhibits its larger variations in magnitude in mid-latitudes other than in other regions of the globe. Additionally, our results also show that the global air mass is redistributed seasonally not only between the Northern and Southern Hemispheres but also between land and sea. This land-sea air mass redis- tribution induces a zonal pattern of surface air pressure in the Northern Hemisphere but the meridional pattern in the Southern Hemisphere.
文摘南北两半球大气中高纬度之间的相互作用与季风等跨半球的天气气候系统存在着密切联系,由于涉及全球范围的大尺度环流与能量变化,其联系途径与机理受到学者们的广泛关注。本文结合ERA5再分析资料以及CMIP6中MPI-ESM1-2-HR模式历史输出资料,验证了冬季南北半球际大气质量涛动(Inter-Hemispheric atmospheric mass Oscillation, IHO)与东亚冬季风异常的联系及其对中国冬季气温的影响。研究表明,再分析资料以及模式结果均表明冬季IHO与东亚冬季风存在显著的正相关关系。IHO通过全球大气质量再分配与东亚冬季风建立起紧密的联系。当IHO为正位相时,大气质量在欧亚大陆北部异常堆积,而在中低纬地区异常亏损,这使得东亚地区海陆气压差明显增大,冬季风增强,同时对中国华中地区冬季地表气温具有显著影响;反之亦然。进一步分析发现,热带低平流层气温可以通过剩余环流调节臭氧含量经向分布进而影响南极对流层气温,从而对IHO年际变化起主要的驱动作用。
文摘本研究确定了某激光粉尘仪测试上海市环境大气颗粒物(PM10和PM2.5)的质量浓度转换系数K值。利用激光粉尘仪和TEOM RP 1400a型监测仪,同时对选定的环境监测站同一监测点的环境大气颗粒物(PM10和PM2.5)进行了测定,得出了该激光粉尘仪测试上海市环境大气颗粒物(PM10和PM2.5)的质量浓度转换系数K值呈基本正态分布,分别为0.00594和0.00158。