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...

Full description

Saved in:
Bibliographic Details
Published inThe cryosphere Vol. 17; no. 7; pp. 3063 - 3082
Main Author Ng, Felix S. L
Format Journal Article
LanguageEnglish
Published Katlenburg-Lindau Copernicus GmbH 26.07.2023
Copernicus Publications
Subjects
Online AccessGet full text

Cover

Loading…