黑龙江气象
黑龍江氣象
흑룡강기상
HEILONGJIANG METEOROLOGY
2011年
3期
3-4,7
,共3页
许英杰%谢玉静%张林媛%任淑英
許英傑%謝玉靜%張林媛%任淑英
허영걸%사옥정%장림원%임숙영
冰雹%中尺度分析%雷达回波演变
冰雹%中呎度分析%雷達迴波縯變
빙박%중척도분석%뢰체회파연변
storm hail%middle scale analysis%radar echo changing
利用哈尔滨新一代天气雷达和常规观测资料,对黑龙江2011年6月9日受东北冷涡影响产生的区域性冰雹天气进行中尺度分析,结果表明:500 hPa黑龙江中西部有闭合冷中心,850hPa以下低空为暖脊,形成上冷下暖的不稳定大气层结。地面冷锋及850 hPa干线是不稳定能量释放的主要条件;冰雹落区是在低空急流出口区、高空槽前及850 hPa干线前方的中尺度对流潜势区内;雷达回波演变分析表明,初始阶段强回波高度迅速上升,降雹时有三体散射特征,消亡阶段强回波高度迅速下降,最后演变成积层混合性回波,并且各阶段强回波一直接地。
利用哈爾濱新一代天氣雷達和常規觀測資料,對黑龍江2011年6月9日受東北冷渦影響產生的區域性冰雹天氣進行中呎度分析,結果錶明:500 hPa黑龍江中西部有閉閤冷中心,850hPa以下低空為暖脊,形成上冷下暖的不穩定大氣層結。地麵冷鋒及850 hPa榦線是不穩定能量釋放的主要條件;冰雹落區是在低空急流齣口區、高空槽前及850 hPa榦線前方的中呎度對流潛勢區內;雷達迴波縯變分析錶明,初始階段彊迴波高度迅速上升,降雹時有三體散射特徵,消亡階段彊迴波高度迅速下降,最後縯變成積層混閤性迴波,併且各階段彊迴波一直接地。
이용합이빈신일대천기뢰체화상규관측자료,대흑룡강2011년6월9일수동북랭와영향산생적구역성빙박천기진행중척도분석,결과표명:500 hPa흑룡강중서부유폐합랭중심,850hPa이하저공위난척,형성상랭하난적불은정대기층결。지면랭봉급850 hPa간선시불은정능량석방적주요조건;빙박락구시재저공급류출구구、고공조전급850 hPa간선전방적중척도대류잠세구내;뢰체회파연변분석표명,초시계단강회파고도신속상승,강박시유삼체산사특정,소망계단강회파고도신속하강,최후연변성적층혼합성회파,병차각계단강회파일직접지。
in this article,we applied the data of Haerbin Doppler radar to analyze the middle scale regional storm hail happened on 9th Jun.Heilongjiang province,it was showed that the unstable atmosphere was formed with a circle could center in west Heilongjiang province on 500hPa weather map and a warm ridge on the lower level 850 hPa;could front and dry line on 850hPa were the main unstable energy realizing conditions.The storm hail fall region was near the follow mouth of lower jet and before the high level trough.The changes of radar echo showed that the strong echo developed quickly at beginning,and there was scatter characteristic when storm hail began to fall,and the strong echo reduced quickly too at the reducing stage,and changed to the mixed echo at last,and the echo connected to the ground at every stages.