大连地区雷暴大风的气候和天气学特征  

Climatic and synoptic characteristics of thunderstorm gale in Dalian region

作　　者：杨景泰 隋玉秀 王健 周美娥 于德华 孙立娟 潘玉成 YANG Jing-tai;SUI Yu-xiu;WANG Jian;ZHOU Mei-e;YU De-hua;SUN Li-juan;PAN Yu-cheng(Dalian Meteorological Service Center,Dalian 116001,China;Air Force University,Changchun 130000,China)

机构地区：[1]大连市气象服务中心,辽宁大连116001 [2]空军航空大学,吉林长春130000

出　　处：《气象与环境学报》2017年第6期49-57,共9页Journal of Meteorology and Environment

基　　金：国家自然科学基金项目(41171137)资助

摘　　要：基于1999—2013年大连地区的雷暴大风、雷暴和冰雹等观测资料,对大连地区雷暴大风天气的气候和天气学特征进行了分析。结果表明:1999—2013年大连地区雷暴大风天气具有较强的地域特点,夜间雷暴大风天气的发生频率明显高于白天,海岛站雷暴大风出现次数明显多于陆地站;雷暴大风天气主要集中出现在夏季,10月雷暴大风发生也较多。统计表明,大连地区雷暴大风天气通常发生在空间尺度和时间尺度均相对较大的雷暴群中,单体雷暴出现雷暴大风的概率极低,且大都伴有降水,但雷暴大风与暴雨或冰雹相伴出现的概率较低。大连地区的雷暴大风天气是由多种有利的高低空系统配置及高低空急流和中高空干空气的共同作用产生的,其中高空急流和中高空干空气是制约雷暴大风产生的重要因素,高空急流有时制约雷暴大风的产生方位和分布形态,大连地区雷暴大风通常位于高空急流轴下方及其附近区域;中高空干空气具有3个作用:一是增强大气不稳定度;二是在干湿区的交界处形成较强的露点锋,有时具有雷暴的触发作用;三是与其他天气系统叠加时具有增强上升运动的作用。Based on the observation data of thunderstorm gale,thunderstorm,hail and other weather phenomena in the region of Dalian region from1999to2013,the climatic and synoptic characteristics of thunderstorm gale in Dalian were analyzed.The results reveal that occurrence regularity of thunderstorm gale in Dalian has a strong regional characteristic.The occurrence frequency at night is significantly higher than that at daytime.The number of thunderstorm gales happened on the island stations is significantly greater than that on the land stations.Thunderstorm gales mainly occur in summer.In addition,October is also the time when thunderstorm gales happened frequently.Statistics analyses show that the thunderstorm gales often occur in the thunderstorm groups which have a large spatial scale and time scale in Dalian region,and the probability that a single thunderstorm cell causes thunderstorm gales is very low.Mostly,the occurrence of thunderstorm gales accompanies with rainfall,while the occurrence of thunderstorm gale rainstorm or hail simultaneously is rare.The thunderstorm gales in Dalian region are usually formed by the combination of many favorable configurations of upper and lower altitude systems,jet stream at upper and lower level and dry air at middle and upper altitude.The most important factors that control the generation of thunderstorm gale are jet streams at the upper level and dry air at the middle and upper altitude.The jet stream at an upper level sometimes controls the location and the distributing pattern of the thunderstorm gale.Thunderstorm gales in Dalian region usually located at the areas near and down the axis of the upper level jet stream.There are three functions for dry air at the middle and upper altitude,i.e.enhancing the atmospheric instability,forming a very strong dew point front at the junction of dry and wet areas and sometimes triggering thunderstorms,and enhancing the ascending motion when it superposes with other weather systems.

关 键 词：干空气 急流 稳定度 露点锋 上升运动 

分 类 号：P425.47[天文地球—大气科学及气象学] P446