Oxygen isotopes in glacier-river water, Austre Okstindbreen, Okstindan, Norway
There is no discernible river discharge from Austre Okstindbreen, Norway, in winter; any water formed by basal melting is likely to be stored in isolated cavities or sediments at the bed. In summer, a baseflow component of discharge, relatively depleted of 18O, is diluted by water more enriched in 1...
Published in: | Journal of Glaciology |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2003
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Online Access: | https://research.manchester.ac.uk/en/publications/f29e34f3-4f56-4eac-ab45-1c10f5da58f4 https://doi.org/10.3189/172756503781830700 |