Author:
Yao Tandong,Thompson Lonnie G.,Jiao Keqin,Mosley-Thompson Ellen,Yang Zhihong
Abstract
Oxygen-isotope ratios (δ
18O) measured on ice cores on the Qinghai-Tibetan Plateau, China, increased by 1.2-2.2‰ from the 1960s to the 1990s. Measurements of the δ
18O content of precipitation and the simultaneous air temperatures needed to compute the temperature increase corresponding to the increase in δ
18O are currently made at the Delingha Meteorological Station, but the amount of data is not yet sufficient to obtain a reliable result.
Publisher
International Glaciological Society
Cited by
29 articles.
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