date: 2016-06-22T14:48:24Z
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pdf:docinfo:title:  New Evidence for Abrupt Sea-Ice Fluctuations in the Subpolar North Atlantic at the End of the Last Glacial in Relation with Thermohaline and Atmospheric Circulation 
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dc:description:  A temporally highly resolved reconstruction of sea-ice conditions in eastern Fram Strait, using the sea-ice proxy IP25, sheds new light on potential feedback mechanisms between sea-ice variability and ocean circulation changes during rapid deglacial climate shifts. While a post-LGM sea-ice maximum probably played an important role for the timing of Heinrich Event 1, distinct sea-ice discharge events seem to be intrinsically tied to perturbations in the oceanic overturning circulation. The herein presented sea-ice record is the hitherto only continuous documentation of sea-ice changes in the subpolar North Atlantic that covers the transition from the last glacial into the Holocene. These data strengthen the need for more studies of high-resolution sediment cores to better assess the short-term palaeoenvironmental development and the feedback mechanisms between sea-ice variability and oceanic/ atmospheric circulation fluctuations during this crucial time of climate change. 
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subject:  A temporally highly resolved reconstruction of sea-ice conditions in eastern Fram Strait, using the sea-ice proxy IP25, sheds new light on potential feedback mechanisms between sea-ice variability and ocean circulation changes during rapid deglacial climate shifts. While a post-LGM sea-ice maximum probably played an important role for the timing of Heinrich Event 1, distinct sea-ice discharge events seem to be intrinsically tied to perturbations in the oceanic overturning circulation. The herein presented sea-ice record is the hitherto only continuous documentation of sea-ice changes in the subpolar North Atlantic that covers the transition from the last glacial into the Holocene. These data strengthen the need for more studies of high-resolution sediment cores to better assess the short-term palaeoenvironmental development and the feedback mechanisms between sea-ice variability and oceanic/ atmospheric circulation fluctuations during this crucial time of climate change. 
dc:creator: Juliane Müller
description:  A temporally highly resolved reconstruction of sea-ice conditions in eastern Fram Strait, using the sea-ice proxy IP25, sheds new light on potential feedback mechanisms between sea-ice variability and ocean circulation changes during rapid deglacial climate shifts. While a post-LGM sea-ice maximum probably played an important role for the timing of Heinrich Event 1, distinct sea-ice discharge events seem to be intrinsically tied to perturbations in the oceanic overturning circulation. The herein presented sea-ice record is the hitherto only continuous documentation of sea-ice changes in the subpolar North Atlantic that covers the transition from the last glacial into the Holocene. These data strengthen the need for more studies of high-resolution sediment cores to better assess the short-term palaeoenvironmental development and the feedback mechanisms between sea-ice variability and oceanic/ atmospheric circulation fluctuations during this crucial time of climate change. 
dcterms:created: 2016-06-22T09:03:16Z
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title:  New Evidence for Abrupt Sea-Ice Fluctuations in the Subpolar North Atlantic at the End of the Last Glacial in Relation with Thermohaline and Atmospheric Circulation 
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dc:title:  New Evidence for Abrupt Sea-Ice Fluctuations in the Subpolar North Atlantic at the End of the Last Glacial in Relation with Thermohaline and Atmospheric Circulation 
modified: 2016-06-22T14:48:24Z
cp:subject:  A temporally highly resolved reconstruction of sea-ice conditions in eastern Fram Strait, using the sea-ice proxy IP25, sheds new light on potential feedback mechanisms between sea-ice variability and ocean circulation changes during rapid deglacial climate shifts. While a post-LGM sea-ice maximum probably played an important role for the timing of Heinrich Event 1, distinct sea-ice discharge events seem to be intrinsically tied to perturbations in the oceanic overturning circulation. The herein presented sea-ice record is the hitherto only continuous documentation of sea-ice changes in the subpolar North Atlantic that covers the transition from the last glacial into the Holocene. These data strengthen the need for more studies of high-resolution sediment cores to better assess the short-term palaeoenvironmental development and the feedback mechanisms between sea-ice variability and oceanic/ atmospheric circulation fluctuations during this crucial time of climate change. 
pdf:docinfo:subject:  A temporally highly resolved reconstruction of sea-ice conditions in eastern Fram Strait, using the sea-ice proxy IP25, sheds new light on potential feedback mechanisms between sea-ice variability and ocean circulation changes during rapid deglacial climate shifts. While a post-LGM sea-ice maximum probably played an important role for the timing of Heinrich Event 1, distinct sea-ice discharge events seem to be intrinsically tied to perturbations in the oceanic overturning circulation. The herein presented sea-ice record is the hitherto only continuous documentation of sea-ice changes in the subpolar North Atlantic that covers the transition from the last glacial into the Holocene. These data strengthen the need for more studies of high-resolution sediment cores to better assess the short-term palaeoenvironmental development and the feedback mechanisms between sea-ice variability and oceanic/ atmospheric circulation fluctuations during this crucial time of climate change. 
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pdf:docinfo:creator: Juliane Müller
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