气象学报
氣象學報
기상학보
ACTA METEOROLOGICA SINICA
2014年
3期
542-553
,共12页
樊雯璇%王颢樾%王卫国%杨芳园%张万诚
樊雯璇%王顥樾%王衛國%楊芳園%張萬誠
번문선%왕호월%왕위국%양방완%장만성
剩余环流%对流层顶%对流层%平流层%季节%时空结构
剩餘環流%對流層頂%對流層%平流層%季節%時空結構
잉여배류%대류층정%대류층%평류층%계절%시공결구
Residual circulation%Tropopause%Troposphere%Stratosphere%Season%Temporal-spatial structure
利用ERA-Interim资料,采用改进的变形欧拉平均方法对1979-2011年剩余环流季节内时空结构转换及其演变特征进行了分析。结果表明:(1)150 hPa附近4-8月剩余环流上升中心发生了整体向北移动的趋势,而9月至次年2月则表现为整体向南的移动,并且6-8月和9-11月的移动较为明显,分别向北和向南移动了3.168°和2.277°。(2)对流层内的剩余质量输送显著增强,但是热带环流上升区以及穿越对流层顶进入平流层的输送存在着减弱的趋势。(3)两半球高纬度100 hPa附近从最低平流层向下输送的质量通量以及热带对流层顶附近向上输送的质量通量在各季节年代际变化中基本都是减弱的,仅在6-8月和9-11月北半球向下质量通量出现了增强。
利用ERA-Interim資料,採用改進的變形歐拉平均方法對1979-2011年剩餘環流季節內時空結構轉換及其縯變特徵進行瞭分析。結果錶明:(1)150 hPa附近4-8月剩餘環流上升中心髮生瞭整體嚮北移動的趨勢,而9月至次年2月則錶現為整體嚮南的移動,併且6-8月和9-11月的移動較為明顯,分彆嚮北和嚮南移動瞭3.168°和2.277°。(2)對流層內的剩餘質量輸送顯著增彊,但是熱帶環流上升區以及穿越對流層頂進入平流層的輸送存在著減弱的趨勢。(3)兩半毬高緯度100 hPa附近從最低平流層嚮下輸送的質量通量以及熱帶對流層頂附近嚮上輸送的質量通量在各季節年代際變化中基本都是減弱的,僅在6-8月和9-11月北半毬嚮下質量通量齣現瞭增彊。
이용ERA-Interim자료,채용개진적변형구랍평균방법대1979-2011년잉여배류계절내시공결구전환급기연변특정진행료분석。결과표명:(1)150 hPa부근4-8월잉여배류상승중심발생료정체향북이동적추세,이9월지차년2월칙표현위정체향남적이동,병차6-8월화9-11월적이동교위명현,분별향북화향남이동료3.168°화2.277°。(2)대류층내적잉여질량수송현저증강,단시열대배류상승구이급천월대류층정진입평류층적수송존재착감약적추세。(3)량반구고위도100 hPa부근종최저평류층향하수송적질량통량이급열대대류층정부근향상수송적질량통량재각계절년대제변화중기본도시감약적,부재6-8월화9-11월북반구향하질량통량출현료증강。
Using the European Center for Medium Range Weather Forecasts Interim (ERA-Interim)data,temporal-spatial structural switch and evolution characteristics of the residual circulation derived from the improved transformed Eulerian-mean equation in the different seasons during 1979-2011 were analyzed.The results show that:(1)The center of the residual circu-lation upwelling in 150 hPa tends to shift toward the north from April to August,and reaches to a souther location from Sep-tember to February next year during 1979-2011.The change in June-August (JJA)and Septermber-November (SON)are most obvious;it extends 3.069 degree toward the north in JJA and 2.376 degree toward the south in SON,respectively.(2) The residual circulation in the troposphere observably strengthens in the different seasons during 1979-2011,but it weakens in the circulation upwelling area near the tropical and near tropopause.And,(3)both of downward mass flux in the high latitudes of the two hemispheres and upward mass flux in the tropics near 100 hPa almost all weaken in the different seasons during 1979-2011,except for downward mass flux in the Northern Hemisphere during JJA and SON.