Diffusive smoothing of isotopic signals in ice cores: the grain-scale signature of excess diffusion as a testable prediction

Ng, F.S.L. orcid.org/0000-0001-6352-0351 (2024) Diffusive smoothing of isotopic signals in ice cores: the grain-scale signature of excess diffusion as a testable prediction. In: EGU General Assembly 2024. EGU General Assembly 2024, 14-19 Apr 2024, Vienna, Austria. Copernicus Publications

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Item Type: Proceedings Paper
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© Author(s) 2024. This work is distributed under the Creative Commons Attribution 4.0 License. (http://creativecommons.org/licenses/by/4.0/)
Keywords: Earth Sciences; Physical Geography and Environmental Geoscience; Geology
Dates:
  • Published (online): 8 March 2024
  • Published: 8 March 2024
Institution: The University of Sheffield
Academic Units: The University of Sheffield > Faculty of Social Sciences (Sheffield) > Department of Geography (Sheffield)
Depositing User: Symplectic Sheffield
Date Deposited: 16 Aug 2024 14:36
Last Modified: 16 Aug 2024 14:37
Status: Published
Publisher: Copernicus Publications
Refereed: Yes
Identification Number: 10.5194/egusphere-egu24-5175
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