By using the routine weather data and the numerical value forecast products,applying the weather analysis and diagnostic analysis methods,the cold wave weather which happened in the south area of Dalian was analyzed o...By using the routine weather data and the numerical value forecast products,applying the weather analysis and diagnostic analysis methods,the cold wave weather which happened in the south area of Dalian was analyzed on December 29-30,2009.The results showed that based on the temperature rise in prior period,the strong cold air accumulated in Mongolia and passed Ulan Bator,Erenhot to invade Dalian area.In the cold wave process,the circulation situations in the middle and high latitudes were the 'one ridge and one trough' pattern in Asia.The dynamic mechanisms were the rotary low-pressure trough in high altitude and the strong frontal zone,and the flow field which induced the cold wave to break out was the 'low trough rotation pattern'.After the cold air broke out,Dalian area was controlled by the strong cold advection.The cold high-pressure on the ground entered into the key zone and reached the intensity of cold wave.However,the circulation of cold wave occurrence was southerly,and the shifts of cold air and influence system were quicker.Therefore,the cold wave appeared in Dalian's south areas which included Lvshun,Dalian and Jinzhou.On this basis,the key point of cold wave weather forecast in Dalian area was summarized.展开更多
Reflection of stratospheric planetary waves and its impact on tropospheric cold weather over Asia during January 2008 were investigated by applying two dimensional Eliassen-Palm （EP） flux and three-dimensional Plumb...Reflection of stratospheric planetary waves and its impact on tropospheric cold weather over Asia during January 2008 were investigated by applying two dimensional Eliassen-Palm （EP） flux and three-dimensional Plumb wave activity fluxes.The planetary wave propagation can clearly be seen in the longitude-height and latitude-height sections of the Plumb wave activity flux and EP flux,respectively,when the stratospheric basic state is partially reflective.Primarily,a wave packet emanating from Baffin Island/coast of Labrador propagated eastward,equatorward and was reflected over Central Eurasia and parts of China,which in turn triggered the advection of cold wind from the northern part of the boreal forest regions and Siberia to the subtropics.The wide region of Central Eurasia and China experienced extreme cold weather during the second ten days of January 2008,whereas the extraordinary persistence of the event might have occurred due to an anomalous blocking high in the Urals-Siberia region.展开更多
利用常规气象观测资料、NECP/NCAR 1°×1°再分析资料和探空资料,应用天气学和动力气象学分析诊断方法,对2016年1月21—24日山西寒潮、大风和降雪过程的影响系统配置、冷空气移动路径和高低空环流形势演变进行了诊断分析,...利用常规气象观测资料、NECP/NCAR 1°×1°再分析资料和探空资料,应用天气学和动力气象学分析诊断方法,对2016年1月21—24日山西寒潮、大风和降雪过程的影响系统配置、冷空气移动路径和高低空环流形势演变进行了诊断分析,并对大风和降雪主要成因进行了分析。结果表明:此次寒潮过程属于"横槽型",500 h Pa上贝加尔湖东部的冷涡引导冷空气,沿西北偏西路径进入山西,以及地面冷高压南下是寒潮爆发的原因。850 h Pa存在强盛的冷平流,是产生寒潮天气的主要原因。但由于冷空气移动路径偏西,冷高压主体偏北,造成本次降温幅度只有个别站点突破历史极值。水汽条件较差,所以降水过程较弱;地面正负3 h变压差达10 h Pa,利于产生变压风,造成大风天气。展开更多
利用地面、探空实时业务观测以及NCEP 1°×1°分析数据等资料,对2016年1月下旬寒潮过程地面气压场、过程最低气温、广东降雪空间分布、大气温湿结构以及天气系统等方面进行了分析,结果发现:该次寒潮过程广东地面气压突破...利用地面、探空实时业务观测以及NCEP 1°×1°分析数据等资料,对2016年1月下旬寒潮过程地面气压场、过程最低气温、广东降雪空间分布、大气温湿结构以及天气系统等方面进行了分析,结果发现:该次寒潮过程广东地面气压突破了有气象记录(1951年)以来的历史极值,但大部分市县最低气温未破历史记录;降雪南界较历史南界(1951—2015年)明显南压,即西部压到信宜、阳春一带,中东部则南压到了沿海;t850<0℃或t925<0℃的单层温度指标难以判断广东雨雪相态;当高空整层温度都在0℃以下,且近地面0℃层高度低时降水相态多为雪,0℃层高度过高时则降水相态为雨,其余为雨夹雪(霰);当高空有暖层存在时,出现纯雪的可能性较小,若地面0℃层高度低,且高空暖层厚度<位于其下方的冷冻层,则有雨夹雪(霰)的可能;降雪时大气湿度呈下干上湿状态,90%以上的高湿度区主要在800~500 h Pa之间;降雪时的辐合抬升主要发生在700~500 h Pa,中层的槽和西到西南急流是重要的动力因子。展开更多
文摘By using the routine weather data and the numerical value forecast products,applying the weather analysis and diagnostic analysis methods,the cold wave weather which happened in the south area of Dalian was analyzed on December 29-30,2009.The results showed that based on the temperature rise in prior period,the strong cold air accumulated in Mongolia and passed Ulan Bator,Erenhot to invade Dalian area.In the cold wave process,the circulation situations in the middle and high latitudes were the 'one ridge and one trough' pattern in Asia.The dynamic mechanisms were the rotary low-pressure trough in high altitude and the strong frontal zone,and the flow field which induced the cold wave to break out was the 'low trough rotation pattern'.After the cold air broke out,Dalian area was controlled by the strong cold advection.The cold high-pressure on the ground entered into the key zone and reached the intensity of cold wave.However,the circulation of cold wave occurrence was southerly,and the shifts of cold air and influence system were quicker.Therefore,the cold wave appeared in Dalian's south areas which included Lvshun,Dalian and Jinzhou.On this basis,the key point of cold wave weather forecast in Dalian area was summarized.
基金supported jointly by the National Basic Research Program of China (Grant No. 2010CB 428603)the National Natural Science Foundation of China (Grants Nos. 41250110073, 41350110331 and 41025017)+1 种基金the Chinese Academy of Sciences fellowship for young international scientists (Grant No. 2011Y2ZZB05)a China postdoctoral science foundation grant (Grant No. 2013M541010)
文摘Reflection of stratospheric planetary waves and its impact on tropospheric cold weather over Asia during January 2008 were investigated by applying two dimensional Eliassen-Palm （EP） flux and three-dimensional Plumb wave activity fluxes.The planetary wave propagation can clearly be seen in the longitude-height and latitude-height sections of the Plumb wave activity flux and EP flux,respectively,when the stratospheric basic state is partially reflective.Primarily,a wave packet emanating from Baffin Island/coast of Labrador propagated eastward,equatorward and was reflected over Central Eurasia and parts of China,which in turn triggered the advection of cold wind from the northern part of the boreal forest regions and Siberia to the subtropics.The wide region of Central Eurasia and China experienced extreme cold weather during the second ten days of January 2008,whereas the extraordinary persistence of the event might have occurred due to an anomalous blocking high in the Urals-Siberia region.
文摘利用常规气象观测资料、NECP/NCAR 1°×1°再分析资料和探空资料,应用天气学和动力气象学分析诊断方法,对2016年1月21—24日山西寒潮、大风和降雪过程的影响系统配置、冷空气移动路径和高低空环流形势演变进行了诊断分析,并对大风和降雪主要成因进行了分析。结果表明:此次寒潮过程属于"横槽型",500 h Pa上贝加尔湖东部的冷涡引导冷空气,沿西北偏西路径进入山西,以及地面冷高压南下是寒潮爆发的原因。850 h Pa存在强盛的冷平流,是产生寒潮天气的主要原因。但由于冷空气移动路径偏西,冷高压主体偏北,造成本次降温幅度只有个别站点突破历史极值。水汽条件较差,所以降水过程较弱;地面正负3 h变压差达10 h Pa,利于产生变压风,造成大风天气。
文摘利用地面、探空实时业务观测以及NCEP 1°×1°分析数据等资料,对2016年1月下旬寒潮过程地面气压场、过程最低气温、广东降雪空间分布、大气温湿结构以及天气系统等方面进行了分析,结果发现:该次寒潮过程广东地面气压突破了有气象记录(1951年)以来的历史极值,但大部分市县最低气温未破历史记录;降雪南界较历史南界(1951—2015年)明显南压,即西部压到信宜、阳春一带,中东部则南压到了沿海;t850<0℃或t925<0℃的单层温度指标难以判断广东雨雪相态;当高空整层温度都在0℃以下,且近地面0℃层高度低时降水相态多为雪,0℃层高度过高时则降水相态为雨,其余为雨夹雪(霰);当高空有暖层存在时,出现纯雪的可能性较小,若地面0℃层高度低,且高空暖层厚度<位于其下方的冷冻层,则有雨夹雪(霰)的可能;降雪时大气湿度呈下干上湿状态,90%以上的高湿度区主要在800~500 h Pa之间;降雪时的辐合抬升主要发生在700~500 h Pa,中层的槽和西到西南急流是重要的动力因子。
