利用覆盖北京地区的地基GPS水汽监测网数据反演的地基GPS大气柱水汽含量(precipitable water vapor,PWV),分析了2009年7月3次暴雨天气过程中大气柱水汽含量的水平分布特征;利用高空、地面常规气象资料以及加密气象自动站观测资料计算地...利用覆盖北京地区的地基GPS水汽监测网数据反演的地基GPS大气柱水汽含量(precipitable water vapor,PWV),分析了2009年7月3次暴雨天气过程中大气柱水汽含量的水平分布特征;利用高空、地面常规气象资料以及加密气象自动站观测资料计算地面和高空比湿,结合温度、风等物理量分析3次暴雨天气过程中的大尺度水汽输送和中尺度局地辐合作用;对最大降水强度以及降水量的时间变化的分析表明:3次降水落区分布特征与降水前期大气柱水汽含量高值的水平分布较为一致;大气柱水汽含量曲线变化特征与各尺度天气系统造成的水汽输送和水汽辐合密切相关,大气柱水汽含量的大小与水汽来源密切相关;降水前4小时内大气柱水汽含量出现陡增,线性增速大于1.1mm/h,最大降水强度出现在大气柱水汽含量峰值出现后的1～2h。展开更多
A method for the determination of dichlofluanid residue by Capillary Collumns Gas Chromatography was established in this study.Samples were extracted with acetone and subjected to through liquid-liquid extraction with...A method for the determination of dichlofluanid residue by Capillary Collumns Gas Chromatography was established in this study.Samples were extracted with acetone and subjected to through liquid-liquid extraction with N-hexane,and then they were cleanup with column that filled with florisil,subsequently separated by Capillary Column Gas Chromatography,and the electron capture detector （ECD） was used for detection.The detection limit of this method was 0.005 mg/kg （S/N=3）,and this method was rapid,sensitive and accurate,and was applied in the determination of dichlofluanid residue in soybean.展开更多
The anthropogenic CO column content in the atmosphere is derived from measurements with infrared grating spectrometers in Beijing,China,and Moscow,Russia,during 1992–2012.Some specific variation characteristics and l...The anthropogenic CO column content in the atmosphere is derived from measurements with infrared grating spectrometers in Beijing,China,and Moscow,Russia,during 1992–2012.Some specific variation characteristics and long-term variation trends of the CO column content in the atmosphere in these regions are discussed.An evident variation trend of anthropogenic CO in the atmosphere for the Beijing region is not observed during 1992–2012,while for the Moscow region,it decreases yearly by about 1.4% for the same period.High CO concentrations appear quite frequently in Beijing,but much less frequently in Moscow,except during the natural fire events in summer 2010.From back trajectory analysis,the high CO concentration observed in Beijing can be attributed to the intensive CO emission sources in its surrounding areas.展开更多
文摘利用覆盖北京地区的地基GPS水汽监测网数据反演的地基GPS大气柱水汽含量(precipitable water vapor,PWV),分析了2009年7月3次暴雨天气过程中大气柱水汽含量的水平分布特征;利用高空、地面常规气象资料以及加密气象自动站观测资料计算地面和高空比湿,结合温度、风等物理量分析3次暴雨天气过程中的大尺度水汽输送和中尺度局地辐合作用;对最大降水强度以及降水量的时间变化的分析表明:3次降水落区分布特征与降水前期大气柱水汽含量高值的水平分布较为一致;大气柱水汽含量曲线变化特征与各尺度天气系统造成的水汽输送和水汽辐合密切相关,大气柱水汽含量的大小与水汽来源密切相关;降水前4小时内大气柱水汽含量出现陡增,线性增速大于1.1mm/h,最大降水强度出现在大气柱水汽含量峰值出现后的1～2h。
文摘A method for the determination of dichlofluanid residue by Capillary Collumns Gas Chromatography was established in this study.Samples were extracted with acetone and subjected to through liquid-liquid extraction with N-hexane,and then they were cleanup with column that filled with florisil,subsequently separated by Capillary Column Gas Chromatography,and the electron capture detector （ECD） was used for detection.The detection limit of this method was 0.005 mg/kg （S/N=3）,and this method was rapid,sensitive and accurate,and was applied in the determination of dichlofluanid residue in soybean.
基金supported in part by the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No.XDA05100300)the National Basic Research Program of China (Grant No.2013CB955801)+1 种基金the National Natural Science Foundation of China (Grant No.41175030)the Russian Foundation for Basic Research (Grant No.13-05-00956)
文摘The anthropogenic CO column content in the atmosphere is derived from measurements with infrared grating spectrometers in Beijing,China,and Moscow,Russia,during 1992–2012.Some specific variation characteristics and long-term variation trends of the CO column content in the atmosphere in these regions are discussed.An evident variation trend of anthropogenic CO in the atmosphere for the Beijing region is not observed during 1992–2012,while for the Moscow region,it decreases yearly by about 1.4% for the same period.High CO concentrations appear quite frequently in Beijing,but much less frequently in Moscow,except during the natural fire events in summer 2010.From back trajectory analysis,the high CO concentration observed in Beijing can be attributed to the intensive CO emission sources in its surrounding areas.
