The role of ocean and atmospheric dynamics in the marine-based collapse of the last Eurasian Ice Sheet

<p><strong>EIS_reconstruction.zip:&nbsp;</strong>&nbsp;.shp files of Eurasian Ice Sheet reconstruction 20-14 ka (1 ka time step)</p> <p><strong>EIS_thickness.zip</strong>:&nbsp; .shp files of Eurasian Ice Sheet thickness&nbsp;for 19 ka, 18 ka, 16 ka and 15 ka.</p> <p><strong>Supplementary Data 1:</strong>&nbsp;An Excel spreadsheet containing radiocarbon dates from the North Sea</p> <p><strong>Supplementary Data 2</strong>:&nbsp; An Excel spreadsheet containing radiocarbon dates from the Mid Norwegian margin</p> <p><strong>Supplementary Data</strong> <strong>3:&nbsp;</strong>An Excel spreadsheet&nbsp;containing radiocarbon dates from the Svalbard-Kara Sea-Barents Sea</p> <p><strong>Supplementary Data 4:&nbsp;</strong>&nbsp; An Excel spreadsheet&nbsp;containing model output GIA adjusted</p> <p><strong>Supplementary Data 5:&nbsp;</strong> An Excel spreadsheet&nbsp;containing Model output GIA adjusted -20%</p> <p><strong>Supplementary Data 6:</strong>&nbsp; An Excel spreadsheet&nbsp;containing Model output GIA adjusted +20%</p>