贵州气象
貴州氣象
귀주기상
JOURNAL OF GUIZHOU METEOROLOGY
2012年
1期
6-12
,共7页
朱文达%张新月%沈新勇%赵小平
硃文達%張新月%瀋新勇%趙小平
주문체%장신월%침신용%조소평
越赤道气流%台风路径%大气季节内振荡%低频气旋
越赤道氣流%檯風路徑%大氣季節內振盪%低頻氣鏇
월적도기류%태풍로경%대기계절내진탕%저빈기선
Cross-equatorial flows%Typhoon track%ISO%Low-frequency cyclone
越赤道气流作为南北半球物质、能量和水汽的输送通道,它的季节内变化引起台风水汽源变化,影响台风的生成频数和路径。该文研究了越赤道气流ISO特征在台风季节预报中的可行性。台风路径在传统的分类基础上细分为7种,对不同路径的台风所对应的低频流场进行超前和滞后合成,发现不同台风路径对应着不同的低频越赤道气流通道,低层20°N附近的低频气旋外围气流总是预示着台风路径未来的走向。低层低频流场的演变表明,越赤道气流的振荡周期为准40 d,它的ISO特征影响低纬地区的低频气旋的位置和强度,进而影响台风路径。高层低频流场刚好与低层反向,越赤道气流不再是以通道出现而是呈现区域特征。越赤道气流ISO特征可以作为台风季节预报的参考量之一。
越赤道氣流作為南北半毬物質、能量和水汽的輸送通道,它的季節內變化引起檯風水汽源變化,影響檯風的生成頻數和路徑。該文研究瞭越赤道氣流ISO特徵在檯風季節預報中的可行性。檯風路徑在傳統的分類基礎上細分為7種,對不同路徑的檯風所對應的低頻流場進行超前和滯後閤成,髮現不同檯風路徑對應著不同的低頻越赤道氣流通道,低層20°N附近的低頻氣鏇外圍氣流總是預示著檯風路徑未來的走嚮。低層低頻流場的縯變錶明,越赤道氣流的振盪週期為準40 d,它的ISO特徵影響低緯地區的低頻氣鏇的位置和彊度,進而影響檯風路徑。高層低頻流場剛好與低層反嚮,越赤道氣流不再是以通道齣現而是呈現區域特徵。越赤道氣流ISO特徵可以作為檯風季節預報的參攷量之一。
월적도기류작위남북반구물질、능량화수기적수송통도,타적계절내변화인기태풍수기원변화,영향태풍적생성빈수화로경。해문연구료월적도기류ISO특정재태풍계절예보중적가행성。태풍로경재전통적분류기출상세분위7충,대불동로경적태풍소대응적저빈류장진행초전화체후합성,발현불동태풍로경대응착불동적저빈월적도기류통도,저층20°N부근적저빈기선외위기류총시예시착태풍로경미래적주향。저층저빈류장적연변표명,월적도기류적진탕주기위준40 d,타적ISO특정영향저위지구적저빈기선적위치화강도,진이영향태풍로경。고층저빈류장강호여저층반향,월적도기류불재시이통도출현이시정현구역특정。월적도기류ISO특정가이작위태풍계절예보적삼고량지일。
The cross-equatorial flows are the main passages for exchanges of material and energy between northern and southern hemisphere.And its intra-seasonal oscillations(ISO) have very influences on typhoon,typhoon intensity and the typhoon tracks.The modulation of the cross-equatorial flow in the ISO on the typhoon tracks over the Western North Pacific is studied by observation data analysis.The authors divide the main classes tracks of typhoon into seven types based on the traditional methods.The results show that the cross-equatorial flow in the ISO may affect the tracks of typhoon.The low-frequency cross-equatorial flow influences the position or strength of the low-frequency cyclone,low-frequency anticyclone and then influences the typhoon tracks.Preliminary view is that different types typhoon track have different low-frequency cross-equatorial flow channels,the low-frequency flows to the north of the low-frequency cyclone around 20°N lead the approaching typhoon track.Further more,the cycle of cross-equatorial flow in the ISO is quasi-40 day.As a whole,the cross-equatorial flow in the ISO can be used as a basis for the typhoon seasonal forecasting.