基于风廓线雷达技术的沙尘天气监测研究
1. 中国气象局乌鲁木齐沙漠气象研究所,乌鲁木齐 830002;
2. 塔克拉玛干沙漠大气环境观测试验站,新疆塔中 841000
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摘要
利用塔克拉玛干沙漠大气环境观测试验站2010年4月11日沙尘天气风廓线雷达资料,分析了此次过程启动爆发的水平风场、垂直速度和雷达等效回波强度特征。研究表明:风廓线雷达是进行沙尘探测和监测的一种有效的高空大气遥感系统,它不仅可以捕捉到沙尘天气的开始和结束时间,而且能监测到沙尘在空中被输送的高度、厚度范围以及沙尘运动的垂直强度特征;塔克拉玛干沙漠扬沙和沙尘暴雷达等效回波强度约为-3~10 dBZ,浮尘等效回波强度约为-15~-3 dBZ;水平风垂直切变以及低空东风的维持是此次沙尘天气发生的动力成因。扬沙、沙尘暴发生时,大气垂直速度表现为上升运动,在较大水平风速及干燥下垫面的配合下,导致地面沙粒被输送到高空,形成了沙尘天气。
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