Deuterium Excess in a Deep Greenland Ice Core: A proxy for Arctic Sea Ice Concentration
Rising ocean temperatures over the last several decades have led to an accelerated rate of sea ice decline in the northern latitudes. This study is motivated by a need to accurately model and predict sea ice dynamics in a rapidly changing climate. This study uses isotope data from the Renland ice co...
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Carleton Digital Commons
2017
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Online Access: | https://digitalcommons.carleton.edu/comps/939 |