Isotopic diffusion in ice enhanced by vein-water flow
Diffusive smoothing of signals on the water stable isotopes (18O and D) in ice sheets fundamentally limits the climatic information retrievable from these ice-core proxies. Past theories explained how, in polycrystalline ice below the firn, fast diffusion in the network of intergranular water veins...
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Published in | The cryosphere Vol. 17; no. 7; pp. 3063 - 3082 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Katlenburg-Lindau
Copernicus GmbH
26.07.2023
Copernicus Publications |
Subjects | |
Online Access | Get full text |
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