Simplified model of thermal energy balance beneath the Antarctic ice sheet
This code uses a thermal energy balance of the Antarctic subglacial system to simulate basal melting over the past 800,000 years. It parameterizes climate-drive fluctuations in the basal environment using the EPICA Dome C Ice Core δD record.
Main Authors: | , |
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Format: | Other/Unknown Material |
Language: | unknown |
Published: |
Zenodo
2024
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Subjects: | |
Online Access: | https://doi.org/10.5281/zenodo.11126839 |
Summary: | This code uses a thermal energy balance of the Antarctic subglacial system to simulate basal melting over the past 800,000 years. It parameterizes climate-drive fluctuations in the basal environment using the EPICA Dome C Ice Core δD record. |
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