In:
Annals of Glaciology, International Glaciological Society, Vol. 21 ( 1995), p. 196-200
Abstract:
Oxygen-isotope ratios ( δ 18 O) 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 18 O content of precipitation and the simultaneous air temperatures needed to compute the temperature increase corresponding to the increase in δ 18 O are currently made at the Delingha Meteorological Station, but the amount of data is not yet sufficient to obtain a reliable result.
Type of Medium:
Online Resource
ISSN:
0260-3055
,
1727-5644
DOI:
10.1017/S0260305500015810
Language:
English
Publisher:
International Glaciological Society
Publication Date:
1995
detail.hit.zdb_id:
2122400-6
SSG:
14
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