Based on multiple kinds of observation data and NCEP/NCAR reanalysis data,the circulation background,cloud clusters and radar characteristics of a rainstorm far from the typhoon " Haitang" in Lianyungang,Jia...Based on multiple kinds of observation data and NCEP/NCAR reanalysis data,the circulation background,cloud clusters and radar characteristics of a rainstorm far from the typhoon " Haitang" in Lianyungang,Jiangsu on the morning of July 31,2017 were analyzed,and causes of convection were discussed from the aspects of dynamic,thermal and water vapor conditions. The results showed that the rainstorm process was caused by convection cells with low center of mass,and strong convection mainly occurred in a position where temperature gradient at cloud top was the largest. In North China at 850 hP a,eastern cold air on the south side of anticyclonic circulation moved southwards and joined southeast air flow on the periphery of typhoon,which was the main reason for the occurrence of convection. The circulation of upper-level divergence and lowerlevel convergence was beneficial to the maintaining of convection. The convergence of southeast wind speed on the periphery of typhoon made water vapor accumulate,thereby providing enough water vapor for the appearance of heavy rainfall. K index had good denotative meaning to convection activity,and the process of convection with weak Cape value needs to be paid special attention to in business. The prediction effect of rainfall distribution and areas by the models EC and ECRC was superior to other models.展开更多
Based on observation data from automatic stations in Lianyungang, visibility and weather situation of dense fog leading to a traffic accident in Lianyungang on April 15, 2012 were analyzed firstly, and then changes of...Based on observation data from automatic stations in Lianyungang, visibility and weather situation of dense fog leading to a traffic accident in Lianyungang on April 15, 2012 were analyzed firstly, and then changes of meteorological factors related to fog appearance and disappearance, such as wind speed, temperature and relative humidity, were discussed. The results showed that wind speed was below 2 m/s when fog occurred, and wind velocity reduced obviously before visibility deceased, appearing a trough. Fog appeared when temperature was neady the minimum, and there was no great change in wind speed, but visibility went up gradually after temperature rose. The longer the duration of the minimum temperature, the longer the duration of the minimum visibility. Moreover, visibility would become low after temperature rose.展开更多
基金Supported by Science and Technology Planning Project of Lianyungang Meteorological Bureau(LG201604,LG201602)Project of Lianyungang Science and Technology Bureau(SH1634,SH1422)Founds for Science and Technology Innovation Team of Marine Forecasting of Lianyungang Meteorological Bureau
文摘Based on multiple kinds of observation data and NCEP/NCAR reanalysis data,the circulation background,cloud clusters and radar characteristics of a rainstorm far from the typhoon " Haitang" in Lianyungang,Jiangsu on the morning of July 31,2017 were analyzed,and causes of convection were discussed from the aspects of dynamic,thermal and water vapor conditions. The results showed that the rainstorm process was caused by convection cells with low center of mass,and strong convection mainly occurred in a position where temperature gradient at cloud top was the largest. In North China at 850 hP a,eastern cold air on the south side of anticyclonic circulation moved southwards and joined southeast air flow on the periphery of typhoon,which was the main reason for the occurrence of convection. The circulation of upper-level divergence and lowerlevel convergence was beneficial to the maintaining of convection. The convergence of southeast wind speed on the periphery of typhoon made water vapor accumulate,thereby providing enough water vapor for the appearance of heavy rainfall. K index had good denotative meaning to convection activity,and the process of convection with weak Cape value needs to be paid special attention to in business. The prediction effect of rainfall distribution and areas by the models EC and ECRC was superior to other models.
基金Supported by the Meteorological Funds for Distinguished YoungScholars in Jiangsu Province,China(Q201104)Special Project for Forecasters in Jiangsu Meteorological Bureau(JSYBY201308)+2 种基金Project of Lianyungang Bureau of Science and Technology(SH1013)Project of Jiangsu Department of Science and Technology(BE2011720)Social Development Projects of Lianyungang Meteorological Bureau(LG200804,LG201205,LG201108,LG201106,LG201002)
文摘Based on observation data from automatic stations in Lianyungang, visibility and weather situation of dense fog leading to a traffic accident in Lianyungang on April 15, 2012 were analyzed firstly, and then changes of meteorological factors related to fog appearance and disappearance, such as wind speed, temperature and relative humidity, were discussed. The results showed that wind speed was below 2 m/s when fog occurred, and wind velocity reduced obviously before visibility deceased, appearing a trough. Fog appeared when temperature was neady the minimum, and there was no great change in wind speed, but visibility went up gradually after temperature rose. The longer the duration of the minimum temperature, the longer the duration of the minimum visibility. Moreover, visibility would become low after temperature rose.