[Objective] The research aimed to discuss the formation reason of low temperature and frozen disaster weather event in Guizhou in 2008.[Method] By using T213,ECMWF numerical forecast data and the conventional meteorol...[Objective] The research aimed to discuss the formation reason of low temperature and frozen disaster weather event in Guizhou in 2008.[Method] By using T213,ECMWF numerical forecast data and the conventional meteorological observation data which were provided by MICAPS,according to the variation situations of frozen rain,freezing,road freezing and ground surface 0 ℃ line range,the weather situation evolution characteristic of low temperature and frozen weather process (congelation for short) in Guizhou from January 13 to February 15,2008 was analyzed.The formation reason of low temperature and frozen disaster weather event in Guizhou was discussed,and the defense countermeasure was put forward.[Result] The low temperature and frozen weather process happened when the continuous precipitation was caused by that every scale weather system intersected in Guizhou under the abnormal atmospheric circulation background.East Asian inverted Ω flow type in the northern hemisphere made that the atmospheric circulation stabilized for a long time,and the north branch frontal zone was by south.The polar cold air continued to complement and went south to affect Jiangnan,South China.The south branch westerly fluctuation was active,and the frontal zone intensity of stationary front was big,which maintained for a long time.850 hPa shear line in the low level maintained to swing in the junction of Guangxi and Guizhou,Hunan.The southwest warm and wet airflow continued transporting to the south of China.The cold and warm air intersected in South China,which caused the long-time precipitation in Guizhou.The thermal inversion layer was deep and thick.The long-time precipitation based generally on the light rain.It was easy to form the supercooled water droplet.The verglas range expanded from Guizhou,the south of Hunan to the north of Guangxi.The frozen rain and frozen weather caused the long-time road and wire freezing.The disaster was serious.The ground surface temperature 0 ℃ line covered the cold mountain area in the whole province for a long time.The ground surface freezing was difficult to melt,and the low temperature and frozen weather affected Guizhou for a long time.[Conclusion] The research accumulated the experience for the disaster prevention and reduction of such weather.展开更多
文摘[Objective] The research aimed to discuss the formation reason of low temperature and frozen disaster weather event in Guizhou in 2008.[Method] By using T213,ECMWF numerical forecast data and the conventional meteorological observation data which were provided by MICAPS,according to the variation situations of frozen rain,freezing,road freezing and ground surface 0 ℃ line range,the weather situation evolution characteristic of low temperature and frozen weather process (congelation for short) in Guizhou from January 13 to February 15,2008 was analyzed.The formation reason of low temperature and frozen disaster weather event in Guizhou was discussed,and the defense countermeasure was put forward.[Result] The low temperature and frozen weather process happened when the continuous precipitation was caused by that every scale weather system intersected in Guizhou under the abnormal atmospheric circulation background.East Asian inverted Ω flow type in the northern hemisphere made that the atmospheric circulation stabilized for a long time,and the north branch frontal zone was by south.The polar cold air continued to complement and went south to affect Jiangnan,South China.The south branch westerly fluctuation was active,and the frontal zone intensity of stationary front was big,which maintained for a long time.850 hPa shear line in the low level maintained to swing in the junction of Guangxi and Guizhou,Hunan.The southwest warm and wet airflow continued transporting to the south of China.The cold and warm air intersected in South China,which caused the long-time precipitation in Guizhou.The thermal inversion layer was deep and thick.The long-time precipitation based generally on the light rain.It was easy to form the supercooled water droplet.The verglas range expanded from Guizhou,the south of Hunan to the north of Guangxi.The frozen rain and frozen weather caused the long-time road and wire freezing.The disaster was serious.The ground surface temperature 0 ℃ line covered the cold mountain area in the whole province for a long time.The ground surface freezing was difficult to melt,and the low temperature and frozen weather affected Guizhou for a long time.[Conclusion] The research accumulated the experience for the disaster prevention and reduction of such weather.
