Holocene ice sheet dynamics and detrital provenance shifts along the West Greenland Margin recorded by radiogenic isotopes (Sr, Nd, Pb)
Due to the effect of Arctic Amplification the Arctic is currently warming at least twice as fast as the rest of the planet. Seasonal sea-ice extent has been alarmingly declining in the past decade. Glaciers and ice caps along the Greenland coast and in the Canadian Arctic have been losing mass on an...
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| Format: | Other/Unknown Material |
| Language: | English |
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Universität Bremen
2021
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| Online Access: | https://dx.doi.org/10.26092/elib/1186 https://media.suub.uni-bremen.de/handle/elib/5453 |