Working Group of the Arctic Council
Figure 6.22 Bed elevation of the Greenland ice sheet color-coded up to 2000 m, with submarine areas in blue. Details of the large-scale map for (a) Petermann, Steensby and Ryder Gletscher, (b) Hayes Gletscher, Allison Gletscher and Illullip Sermia, (c) Upernavik Isstrøm and Nunatakassaap Sermia, (d) Marie Sophie Gletscher, Academy Gletscher and Hagen Bræ, (e) F. Graae, Charcot and Daugaard-Jensen, and (f ) Kangerlussuaq Gletscher; glaciers within each of the six categories are listed in clockwise order. The white contour line delineates the limit of land ice. The mass conservation method is employed for the glaciers. Kriging is used to map the interior regions (after Morlighem et al., 2014).
Meta Data
Publication:
Snow, Water, Ice and Permafrost in the Arctic (SWIPA) 2017
Page number:
156
Type:
Map
Caption:
Figure 6.22 Bed elevation of the Greenland ice sheet color-coded up to 2000 m, with submarine areas in blue. Details of the large-scale map for (a) Petermann, Steensby and Ryder Gletscher, (b) Hayes Gletscher, Allison Gletscher and Illullip Sermia, (c) Upernavik Isstrøm and Nunatakassaap Sermia, (d) Marie Sophie Gletscher, Academy Gletscher and Hagen Bræ, (e) F. Graae, Charcot and Daugaard-Jensen, and (f ) Kangerlussuaq Gletscher; glaciers within each of the six categories are listed in clockwise order. The white contour line delineates the limit of land ice. The mass conservation method is employed for the glaciers. Kriging is used to map the interior regions (after Morlighem et al., 2014).
Location:
Greenland ice sheet
Copyright:
Arctic Monitoring and Assessment Programme (AMAP)
Cartographer / Designer:
Burnthebook.co.uk