生物灾害科学
生物災害科學
생물재해과학
Biological Disaster Science
2015年
3期
264-269
,共6页
邓吉录%任余龙%韦伯龙%马玉坤
鄧吉錄%任餘龍%韋伯龍%馬玉坤
산길록%임여룡%위백룡%마옥곤
甘肃中部%暴雪%物理特征
甘肅中部%暴雪%物理特徵
감숙중부%폭설%물리특정
central Gansu%blizzard%physical characteristics
利用地面与高空实况观测资料,从高低空地面环流形势和部分物理量反映等方面对甘肃省中部2013年2月17—18日暴雪天气进行综合分析。结果表明:此次暴雪发生在新疆北部冷空气东移南下、高原上有强盛西南暖湿气流配合的有利环流形势下,主要降雪区与500 hPa辐合线相一致;水汽输送主要集中在500 hPa附近,700 hPa偏南气流的水汽输送只是有益的补充;对流层中层500 hPa有较深厚的上升运动,且上升运动极值出现和维持的时间与主要降雪时段一致;暴雪发生前在甘肃中部有较长时间的能量积聚,而冷空气的突然加速南压触发了本次暴雪。
利用地麵與高空實況觀測資料,從高低空地麵環流形勢和部分物理量反映等方麵對甘肅省中部2013年2月17—18日暴雪天氣進行綜閤分析。結果錶明:此次暴雪髮生在新疆北部冷空氣東移南下、高原上有彊盛西南暖濕氣流配閤的有利環流形勢下,主要降雪區與500 hPa輻閤線相一緻;水汽輸送主要集中在500 hPa附近,700 hPa偏南氣流的水汽輸送隻是有益的補充;對流層中層500 hPa有較深厚的上升運動,且上升運動極值齣現和維持的時間與主要降雪時段一緻;暴雪髮生前在甘肅中部有較長時間的能量積聚,而冷空氣的突然加速南壓觸髮瞭本次暴雪。
이용지면여고공실황관측자료,종고저공지면배류형세화부분물리량반영등방면대감숙성중부2013년2월17—18일폭설천기진행종합분석。결과표명:차차폭설발생재신강북부랭공기동이남하、고원상유강성서남난습기류배합적유리배류형세하,주요강설구여500 hPa복합선상일치;수기수송주요집중재500 hPa부근,700 hPa편남기류적수기수송지시유익적보충;대류층중층500 hPa유교심후적상승운동,차상승운동겁치출현화유지적시간여주요강설시단일치;폭설발생전재감숙중부유교장시간적능량적취,이랭공기적돌연가속남압촉발료본차폭설。
By using the ground and high altitude data, and based on the reaction of high and low altitude circulation situation and some physical quantities, this study analyzed the blizzard occurring in central Gansu Province from February 17th to February 18th, 2013. The result showed that this blizzard occurred in this circulation situation:The cold air was eastward and moving down from north Xinjiang, running up against the strong southwest warm current from plateau?The major snow area was consistent with the 500 hPa convergence line, the vapor transportation focused on 500 hPa, and supplied on 700 hPa? A strong ascending motion appeared in the mid tropospheric near 500 hPa, and the appearance over time of extreme value was consistent with the snowfall time?There was a longer period of energy accumulation before the blizzard occurred, and the sudden acceleration of cold air triggered the blizzard.