CAJ | 학술논문

根据1979-2008年青藏高原地区14个探空站对流层项气压资料以及同期各标准等压面上的温度资料，分析了不同季节高原上空两类对流层顶高度与高空各层温度之间的关系；在此基础上，结合同期的NCEP／NCAR月平均再分析资料以及NASA提供的TOMS／SBUV月平均臭氧总量资料，分别讨论了高原上升运动以及高原臭氧总量与对流层顸高度的耦合关系。结果表明：高原第一（二）对流层顶高度全年处在300～200hPa（100hPa附近）高度，在季节变化、年际变化以及长期变化趋势上，两类对流层顸高度与各自对应高度层上的温度存在着密切的反相变化关系，当对流层顶高度偏高（低）时，相应高度上的温度偏低（高）。上升运动有助于两类对流层顶高度的抬升，尤其是当高空200（100）hPa附近有上升运动时，有利于第一（二）对流层项高度抬升。各季节高原臭氧总量与第二对流层顶高度均呈显著的负相关关系，当臭氧含量减少（增加）时，该对流层顶高度将偏高（偏低），近年来伴随着高原臭氧总量的减少，高原第二对流层顸高度出现了明显的抬升。
근거1979-2008년청장고원지구14개탐공참대류층항기압자료이급동기각표준등압면상적온도자료，분석료불동계절고원상공량류대류층정고도여고공각층온도지간적관계；재차기출상，결합동기적NCEP／NCAR월평균재분석자료이급NASA제공적TOMS／SBUV월평균취양총량자료，분별토론료고원상승운동이급고원취양총량여대류층한고도적우합관계。결과표명：고원제일（이）대류층정고도전년처재300～200hPa（100hPa부근）고도，재계절변화、년제변화이급장기변화추세상，량류대류층한고도여각자대응고도층상적온도존재착밀절적반상변화관계，당대류층정고도편고（저）시，상응고도상적온도편저（고）。상승운동유조우량류대류층정고도적태승，우기시당고공200（100）hPa부근유상승운동시，유리우제일（이）대류층항고도태승。각계절고원취양총량여제이대류층정고도균정현저적부상관관계，당취양함량감소（증가）시，해대류층정고도장편고（편저），근년래반수착고원취양총량적감소，고원제이대류층한고도출현료명현적태승。
Using tropopause pressure data and upper temperature data of 14 sounding stations over the Tibetan Plateau from 1979 to 2008, the relationships between two types of tropopause heights and upper air temperature in different seasons are analyzed. Based on these, the coupling connection between as-cending motion（total ozone） and tropopause height is discussed by monthly NCEP/NCAR reanalysis data from NOAA and monthly TOMS/SBUV total ozone data from NASA. The results indicate that the first（second） tropopause is at 300-200 hPa（ near 100 hPa） over the year. The seasonal, interannual variations and long-term trend of the two types of tropopause heights display closely opposite relation to those of temperature at their corresponding altitudes, respectively, namely the higher（lower） tropopause height,the lower（higher） temperature at the corresponding altitude. The ascending motion is conducive to the rising of the tropopause height, especially the ascending motion at about 200 hPa（ 100 hPa） is helpful to the rising of the first（second） tropopause height. There is an obvious negative correlation be-tween the total ozone and the second tropopause height at each season. The second tropopause rises （re-duces） with the losing（increasing） of total ozone over the Tibetan Plateau. In recent years, the second tropopause height clearly lifts with the reducing of the total ozone.