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
Metadata
Item Type: | Proceedings Paper |
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Authors/Creators: |
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Copyright, Publisher and Additional Information: | © 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: |
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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 |
Related URLs: | |
Open Archives Initiative ID (OAI ID): | oai:eprints.whiterose.ac.uk:216169 |