平流層環(huán)狀模的分類特征及其與對(duì)流層的關(guān)系

doi:10.3969/2012jms.00**

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平流層環(huán)狀模的分類特征及其與對(duì)流層的關(guān)系
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                        10.3969/2012jms.00**
                    
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中圖分類號(hào):P434
基金項(xiàng)目:國(guó)家自然科學(xué)基金資助項(xiàng)目(40775059);江蘇省高校自然科學(xué)基礎(chǔ)研究面上項(xiàng)目(07KJB170067);江蘇省“六大人才高峰”計(jì)劃資助項(xiàng)目;教育部留學(xué)回國(guó)人員科研啟動(dòng)基金項(xiàng)目

Classification and characteristics of stratospheric northern annular mode anomalies and their relationships with troposphere

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采用NCEP／NCAR逐日再分析資料,通過對(duì)北半球環(huán)狀模指數(shù)的分析,將平流層異常分為兩類:S型和D型,研究了兩類平流層異常過程的差異及其與對(duì)流層的關(guān)系。結(jié)果表明,兩種類型的異常特征在平流層類似,而主要的差別發(fā)生在對(duì)流層。在S型平流層異常期間,平流層緯向風(fēng)異常有隨時(shí)間向下傳播的趨勢(shì),對(duì)流層表現(xiàn)為與平流層一致連續(xù)的緯向風(fēng)異常;位勢(shì)高度和溫度距平場(chǎng)的分布中,最顯著的特征是對(duì)流層與平流層呈相當(dāng)正壓結(jié)構(gòu),極區(qū)和中緯度異常表現(xiàn)為反位相的振蕩,呈現(xiàn)典型的北極濤動(dòng)特征。在D型平流層異常期間,平流層緯向風(fēng)異常隨時(shí)間向下傳播的趨勢(shì)不存在,另外平流層緯向風(fēng)異常僅局限在平流層范圍內(nèi),對(duì)流層表現(xiàn)為與平流層相反的緯向風(fēng)異常;位勢(shì)高度和溫度距平場(chǎng)的分布中,平流層中低層與高層呈現(xiàn)反位相的距平分布,在對(duì)流層中低層,溫度和位勢(shì)高度的距平場(chǎng)呈現(xiàn)無(wú)規(guī)則的分布。

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Based on the daily NCEP/NCAR reanalysis data,the northern annular mode index is analyzed and the stratospheric northern annular mode anomalies are divided into two types, i.e. the type S and type D.The differences of two types and their relationships with troposphere are measured.Results show that the features of the two types are very similar in the stratosphere,while their differences are great in the troposphere.During the period of type S,the zonal wind anomalies show a downward propagation trend from the stratosphere to the troposphere and a consistent continuity in the two levels.In the geopotential height and temperature anomaly fields,the most remarkable characteristic is the equivalent barotropic structure from the stratosphere to the troposphere,and the inverse phase oscillation exists between the polar region and the middle latitude.Therefore,the type S demonstrates a typical feature of Arctic Oscillation.During the period of type D,the downward propagation trend of the zonal wind anomalies from the stratosphere to the troposphere disappears,and the stratospheric zonal wind anomalies are confined to the stratosphere,which display opposite changes in the troposphere.In the geopotential height and temperature anomaly fields,the anomalies at the middle and low levels of stratosphere show a reverse phase with those at the high level, and the anomalies in the middle and low troposphere show ruleless distributions.

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謝再紅,孫照渤,曾剛,陳海山.平流層環(huán)狀模的分類特征及其與對(duì)流層的關(guān)系.氣象科學(xué),2009,(4):498-506 Xie Zaihong, Sun Zhaobo, Zeng Gang, Chen Haishan. Classification and characteristics of stratospheric northern annular mode anomalies and their relationships with troposphere. Journal of the Meteorological Sciences,2009,(4):498-506

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