利用本溪1981—2013年10月—次年4月降水资料,统计分析了近33年本溪冬半年不同降水相态的气候特征,得出本溪雨雪转换多发季节主要为3月和11月。利用2005—2013年10月—次年4月的探空资料和自动站数据,对近9年本溪冬半年不同相态降水过...利用本溪1981—2013年10月—次年4月降水资料,统计分析了近33年本溪冬半年不同降水相态的气候特征,得出本溪雨雪转换多发季节主要为3月和11月。利用2005—2013年10月—次年4月的探空资料和自动站数据,对近9年本溪冬半年不同相态降水过程的大气层结特征进行统计研究。结果表明：本溪冬半年出现雪时各层温度及地面温度均低于0℃;出现雨时0℃层高度在850~700 h Pa之间;雨雪转换时0℃层高度在925 h Pa附近,各层温度范围分别为：700 h Pa的温度范围[-11℃,-7℃]、850 h Pa的温度范围[-6.5℃,-1.5℃]、9250 h Pa的温度范围[-3℃,1℃]、1000 h Pa的温度范围[0℃,3℃],地面温度小于1000 h Pa温度。本工作的结果除适用于本溪地区的相关预报业务以外,还可以对辽宁东部山区及吉林部分地区的降水相态预报提供较好的参考。展开更多
Based on the routine observation data,the satellite cloud images and so on,the synoptics analysis and the diagnostic analysis of physical quantity field were used to analyze the heavy snowstorm process which happened ...Based on the routine observation data,the satellite cloud images and so on,the synoptics analysis and the diagnostic analysis of physical quantity field were used to analyze the heavy snowstorm process which happened in Northeast China during March 3-5 in 2007.The results showed that the main influence systems in the process were the eastward shift and up north of southern cyclone,the combination of south and north branches upper troughs in 500 hPa.The dynamic mechanisms of heavy snowstorm formation were the strong ascending movement which was caused by the configuration of high-layer divergence and low-layer convergence,the generation and maintenance of deep and thick positive vorticity in the middle and low layers.The sufficient water vapor in the East China Sea and the South China Sea which was brought by 700 hPa by south low-level jet stream reached Northeast China.The falling zones of strong precipitation were consistent with the big value zones of 850 hPa positive vorticity and 200 hPa positive divergence.Meanwhile,the intensity of temperature advection and the position of cold warm transition zone could reflect well the intensity and falling zone of precipitation.展开更多
文摘利用本溪1981—2013年10月—次年4月降水资料,统计分析了近33年本溪冬半年不同降水相态的气候特征,得出本溪雨雪转换多发季节主要为3月和11月。利用2005—2013年10月—次年4月的探空资料和自动站数据,对近9年本溪冬半年不同相态降水过程的大气层结特征进行统计研究。结果表明：本溪冬半年出现雪时各层温度及地面温度均低于0℃;出现雨时0℃层高度在850~700 h Pa之间;雨雪转换时0℃层高度在925 h Pa附近,各层温度范围分别为：700 h Pa的温度范围[-11℃,-7℃]、850 h Pa的温度范围[-6.5℃,-1.5℃]、9250 h Pa的温度范围[-3℃,1℃]、1000 h Pa的温度范围[0℃,3℃],地面温度小于1000 h Pa温度。本工作的结果除适用于本溪地区的相关预报业务以外,还可以对辽宁东部山区及吉林部分地区的降水相态预报提供较好的参考。
文摘Based on the routine observation data,the satellite cloud images and so on,the synoptics analysis and the diagnostic analysis of physical quantity field were used to analyze the heavy snowstorm process which happened in Northeast China during March 3-5 in 2007.The results showed that the main influence systems in the process were the eastward shift and up north of southern cyclone,the combination of south and north branches upper troughs in 500 hPa.The dynamic mechanisms of heavy snowstorm formation were the strong ascending movement which was caused by the configuration of high-layer divergence and low-layer convergence,the generation and maintenance of deep and thick positive vorticity in the middle and low layers.The sufficient water vapor in the East China Sea and the South China Sea which was brought by 700 hPa by south low-level jet stream reached Northeast China.The falling zones of strong precipitation were consistent with the big value zones of 850 hPa positive vorticity and 200 hPa positive divergence.Meanwhile,the intensity of temperature advection and the position of cold warm transition zone could reflect well the intensity and falling zone of precipitation.
