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Relationships between δ~(18)O in precipitation and surface air temperature in the Urumqi River Basin, east Tianshan Mountains, China

机译:天山东部乌鲁木齐河流域降水中δ〜(18)O与地表气温的关系

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摘要

In order to evaluate the dependency of present-day δ~(18)O in precipitation with temperature, individual precipitation events have been continuously sampled since 1996 at three stations along the Urumqi River Basin, eastern Tianshan mountains, north High China. Both the correlation and the positive slope of δ~(18)O versus temperature increase with elevation for monthly averages, indicating that on long time scales high altitude precipitation δ~(18)O should be a reliable indicator of regional temperature fluctuations, and supporting future ice core drilling.
机译:为了评估当今δ〜(18)O对降水量与温度的关系,自1996年以来,在沿乌鲁木齐河流域,天山东部,华北北部的三个站点连续采样了个别降水事件。 δ〜(18)O的相关性和正斜率与温度的正斜率随月平均水平的升高而增加,这表明在长期尺度上,高海拔降水δ〜(18)O应该是区域温度波动的可靠指标,并为未来的冰芯钻探。

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