Temporal Variations of Isotopic Composition of Glacier-River Water During Summer: Observations at Austre Okstindbreen, Okstindan, Norway
Abstract The isotopic composition of river water discharging from the Norwegian glacier, Austre Okstindbreen, in summer varies on both daily and longer-term scales. Most δ 18 o values of samples from the principal river are within the range −12.5 to −14.0‰). Because new snow tends to be relatively d...
Published in: | Journal of Glaciology |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Cambridge University Press (CUP)
1988
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Online Access: | http://dx.doi.org/10.1017/s0022143000007073 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000007073 |