Treeline and Seasonal Sea ice meet today

Jan 5, 2020
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Description
In the Pliocene, the Canadian Arctic was a contiguous land mass and forests reached to the Arctic ocean even on Ellesmere Island and Meighen Island. Some suggest that sea ice in the arctic was seasonal (in winter). So where do forests and winter sea ice meet today? Are these areas good analogs for the warm mid_Pliocene?
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open source from Data Basin
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Creative Commons LicenseThis work is licensed under a Creative Commons Attribution 3.0 License.
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About the Map Author

Julie Brigham-Grette
Professor of Geosciences with University of Massachusetts Amherst

I am a Quaternary geologist interested in the climate evolution of the Arctic starting 5 million years ago to the present. I work on both marine and terrestrial archives and landscapes of climate change, with a focus on the Arctic Pacific Beringian gateway region.