气象
氣象
기상
METEOROLOGICAL MONTHLY
2009年
11期
55-63
,共9页
张俊岚%刘勇达%杨柳%罗继
張俊嵐%劉勇達%楊柳%囉繼
장준람%류용체%양류%라계
水汽源地%水汽输送路径%低空急流
水汽源地%水汽輸送路徑%低空急流
수기원지%수기수송로경%저공급류
water vapor source%water vapor transfer route%low level jet
应用2008年NCEP/NCAR全球再分析逐日网格点资料(2.5°×2.5°)和1970-2008年1-2月南疆29个气象站的日降雪量资料,分析了2008年初南疆盆地持续性降雪天气的大气环流形势演变、水汽源地、水汽输送以及低空急流对水汽输送和集中的作用.结果表明,可降水量场与水汽通量矢量场的分布不一致,水汽源地中以北海的水汽输送贡献最大;水汽输送通过西方和东方输送路径、在中层和中低层进行,西方和东方路径均在青藏高原西侧转为西南气流的水汽输送带,700hPa上的水汽输送较500hPa上强;低空西北和西南急流的建立和维持,对水汽长距离的输送至南疆发挥了重要作用.
應用2008年NCEP/NCAR全毬再分析逐日網格點資料(2.5°×2.5°)和1970-2008年1-2月南疆29箇氣象站的日降雪量資料,分析瞭2008年初南疆盆地持續性降雪天氣的大氣環流形勢縯變、水汽源地、水汽輸送以及低空急流對水汽輸送和集中的作用.結果錶明,可降水量場與水汽通量矢量場的分佈不一緻,水汽源地中以北海的水汽輸送貢獻最大;水汽輸送通過西方和東方輸送路徑、在中層和中低層進行,西方和東方路徑均在青藏高原西側轉為西南氣流的水汽輸送帶,700hPa上的水汽輸送較500hPa上彊;低空西北和西南急流的建立和維持,對水汽長距離的輸送至南疆髮揮瞭重要作用.
응용2008년NCEP/NCAR전구재분석축일망격점자료(2.5°×2.5°)화1970-2008년1-2월남강29개기상참적일강설량자료,분석료2008년초남강분지지속성강설천기적대기배류형세연변、수기원지、수기수송이급저공급류대수기수송화집중적작용.결과표명,가강수량장여수기통량시량장적분포불일치,수기원지중이북해적수기수송공헌최대;수기수송통과서방화동방수송로경、재중층화중저층진행,서방화동방로경균재청장고원서측전위서남기류적수기수송대,700hPa상적수기수송교500hPa상강;저공서북화서남급류적건립화유지,대수기장거리적수송지남강발휘료중요작용.
Using the daily NCEP/ NCAR reanalysis data (2.5°×2.5° lat/lon) in 2008 and daily rainfall data of 29 meteorological stations from January to February between 1970 and 2008 in the southern Xinjiang Basin, the variation of atmospheric circulation circumstances, water vapor source, water vapor transfer and the effect of low level jet were analyzed. The results showed that the distribution of the precipitable water field was different from the vector field of water vapor flux. In the water vapor transfer, the contribution of Beihai was the most, with water vapor transfer in middle and lower layers by west and east routes, respectively. Both water vapor transfers of the west route and east route were changed into that of southwest airflows in the westside of the Tibetan Plateau, with vapor transfer in 700 hPa obviously more than 500 hPa, thus the low level jet plays an important role in the long distance transportation of water vapor to the southern Xinjiang Basin.