江西农业学报
江西農業學報
강서농업학보
ACTA AGRICULTURAE JIANGXI
2014年
3期
116-119
,共4页
葫芦岛%夏季%降水特征%大气环流异常
葫蘆島%夏季%降水特徵%大氣環流異常
호호도%하계%강수특정%대기배류이상
Huludao%Summer%Precipitation characteristics%Atmospheric circulation anomalies
利用NCEP/NCAR再分析月平均资料及葫芦岛地区4个气象站1981~2010年的夏季(6~8月)降水资料,研究了葫芦岛地区夏季降水的年际变化特征及其与大气环流的联系。结果表明:近30年来,葫芦岛沿海地区的夏季降水呈线性下降趋势,变化趋势不显著,西部地区呈线性上升的趋势,且变化趋势显著;葫芦岛地区夏季降水量的空间分布为全区一致型。在葫芦岛地区偏涝年份的200 hPa位势高度距平场上,东北地区反气旋性环流异常偏强,西风风速偏大;在偏涝年份的500 hPa位势高度距平场上,中高纬地区存在经向环流,副热带高压势力偏强、位置偏北;在偏涝年份的850 hPa风距平场上,中国东部存在偏南风异常偏强,带来较多的水汽。
利用NCEP/NCAR再分析月平均資料及葫蘆島地區4箇氣象站1981~2010年的夏季(6~8月)降水資料,研究瞭葫蘆島地區夏季降水的年際變化特徵及其與大氣環流的聯繫。結果錶明:近30年來,葫蘆島沿海地區的夏季降水呈線性下降趨勢,變化趨勢不顯著,西部地區呈線性上升的趨勢,且變化趨勢顯著;葫蘆島地區夏季降水量的空間分佈為全區一緻型。在葫蘆島地區偏澇年份的200 hPa位勢高度距平場上,東北地區反氣鏇性環流異常偏彊,西風風速偏大;在偏澇年份的500 hPa位勢高度距平場上,中高緯地區存在經嚮環流,副熱帶高壓勢力偏彊、位置偏北;在偏澇年份的850 hPa風距平場上,中國東部存在偏南風異常偏彊,帶來較多的水汽。
이용NCEP/NCAR재분석월평균자료급호호도지구4개기상참1981~2010년적하계(6~8월)강수자료,연구료호호도지구하계강수적년제변화특정급기여대기배류적련계。결과표명:근30년래,호호도연해지구적하계강수정선성하강추세,변화추세불현저,서부지구정선성상승적추세,차변화추세현저;호호도지구하계강수량적공간분포위전구일치형。재호호도지구편로년빈적200 hPa위세고도거평장상,동북지구반기선성배류이상편강,서풍풍속편대;재편로년빈적500 hPa위세고도거평장상,중고위지구존재경향배류,부열대고압세력편강、위치편북;재편로년빈적850 hPa풍거평장상,중국동부존재편남풍이상편강,대래교다적수기。
The NCEP/NCAR reanalysis monthly mean data and the summer ( from June to August ) precipitation data of 4 me-teorological stations in Huludao area during 1981~2010 were used to study the interannual variations in summer precipitation and atmospheric circulation.The results showed that:in the past 30 years, the summer rainfall in Huludao coastal region was linearly downward , but the trend was not significant;the summer rainfall in the western region was linearly upward , and the trend was sig-nificant .The spatial distribution of summer precipitation in Huludao area was of all -consistency .On 200 hPa geopotential height a-nomaly field of more precipitation year , Northeastern China had anticyclonic circulation anomalies , which caused larger west wind speed.On 500 hPa geopotential height anomaly field of more precipitation year , the meridional circulation existed in middle -high-latitude area;the influence of subtropical high was relatively strong , and its location was slightly northward .On 850 hPa wind a-nomaly field of more precipitation year , the southward wind in Eastern China was abnormally and relatively strong , which brought more vapor .