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Oxygen isotope composition of surface snow collected along the traverse route from Zhongshan Station toward Dome A, Antarctica

机译:从中山站向南极圆顶a的横向路径收集的表层雪的氧同位素组成

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摘要

Oxygen isotope composition of surface snow sampled in the austral summer of 1998/1999 along the traverse route from Zhongshan Station toward Dome A, Antarctica is measured with the conventional mass spectrometer technique. The results of measurement show that oxygen isotope composition of surface snow varies in a wide range from -22.51‰ to -50.67‰, and has a tendency that isotopic values gradually decrease with increase of distance from Zhongshan Station and altitude. Linear regression analysis indicates that there exists good correlation between oxygen isotope composition of surface snow and distance from Zhongshan Station, altitude and/or latitude, which actually reflects the close relation between stable isotope composition and air temperature.
机译:使用常规质谱仪测量1998/1999南方夏季从中山站到南极穹顶A的横断面采样的地表雪的氧同位素组成。测量结果表明,表雪的氧同位素组成在-22.51‰至-50.67‰的较大范围内变化,且随着离中山站的距离和海拔高度的增加,同位素值有逐渐减小的趋势。线性回归分析表明,表雪的氧同位素组成与距中山站的距离,海拔和/或纬度之间存在良好的相关性,这实际上反映了稳定同位素组成与气温之间的密切关系。

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