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...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Theakstone, Wilfred H.
Format: Article in Journal/Newspaper
Language:English
Published: 2003
Subjects:
Online Access:https://research.manchester.ac.uk/en/publications/f29e34f3-4f56-4eac-ab45-1c10f5da58f4
https://doi.org/10.3189/172756503781830700