CAJ | 학술논문

对1951-1992年青藏高原古里雅冰芯中δ18O与I(南方涛动指数)，δ18O与赤道东太平洋 SST(海表面温度)的关系进行了分析．在EI Nino年．无论是隆冬还是盛夏，古里雅冰芯中δ18O均减小．表现为明显的降温，平均降温幅度分别为1.2℃和0.45℃．在特强El Nino年，平均降温幅度分别为2.03℃和1.46℃．在La Nina年．盛夏古里雅冰芯中δ18O增大．表现为明显的增温，平均升腽幅度为1.02℃，在特强La Nina年，平均升温幅度为1.6℃，但隆冬古里雅冰芯中δ18O变化不明显．在非La Nina年．隆冬古里雅冰芯中δ18O与同期3月SOI和同期1月赤道东太平洋SST的线性相关关系变得显著．
대1951-1992년청장고원고리아빙심중δ18O여I(남방도동지수)，δ18O여적도동태평양 SST(해표면온도)적관계진행료분석．재EI Nino년．무론시륭동환시성하，고리아빙심중δ18O균감 소．표현위명현적강온，평균강온폭도분별위1.2℃화0.45℃．재특강El Nino년，평균강온폭도분 별위2.03℃화1.46℃．재La Nina년．성하고리아빙심중δ18O증대．표현위명현적증온，평균승올폭도위1.02℃，재특강La Nina년，평균승온폭도위1.6℃，단륭동고리아빙심중δ18O변화불명 현．재비La Nina년．륭동고리아빙심중δ18O여동기3월SOI화동기1월적도동태평양SST적선 성상관관계변득현저．
The relationships between the δ18O in the Guliya ice core on the Tibetan Plateau and the SOI, as well as between the δ18O and the SST in the eastern Equatorial Pacific are analyzed. In the El Nino years, no matter in midsummer or in midwinter, δ18O in the Guliya ice core decreased, showing a marked decrease of temperature. The mean extents of the decrease were 1.2℃ and 0.45℃ respectively, and were 2.03℃ and 1.46℃ respectively in the strongest El Nino years; In the La Nina years, δ18O in the Guliya ice core in mid- summer increased, showing a marked rise of tempera- ture. The mean extents of rising was 1.02 ℃, and was 1.6 ℃ in the strongest La Nina years. However, the va- riation of δ18O in midwinter was undefined; In non-La Nina years, the linear correlation between δ18O in midwinter and SOI in March of the corre- sponding period, as well as between ,δ18O and SST in January of the corresponding period became obvious.