Modeling post-depositional changes of delta-D in ice due to sublimation
Ice cores are a valuable component with regards to paleoclimate reconstruction due to the ability to use stable water isotopic concentrations in ice as a proxy for paleo-temperature records. It is therefore important to understand the processes and conditions under which isotopic concentrations can...
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| Language: | en_US |
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2019
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| Online Access: | https://hdl.handle.net/2144/33222 |