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Greenland’s hidden fjord floors in BedMachine v3

A 150 m Greenland bed and fjord map raises sea-level potential by 7 cm and shows 30–100% more glaciers can meet warm Atlantic Water.

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Why do Greenland fjord sills matter?

They can block warm (>2.5°C) Atlantic Water from calving fronts.

Source: BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation · DOI · quote verified

How is the coastal bed mapped?

Mass conservation plus 30 bathymetry sources, seamless within 50 km of the coast at up to 150 m.

Source: BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation · DOI · quote verified

What ice volume does v3 imply?

2.99 ± 0.02 × 10^6 km³ (2.74 ± 0.02 × 10^6 Gt).

Source: BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation · DOI · quote verified

What sea-level potential is reported?

7.42 ± 0.05 m, 7 cm above the prior published value.

Source: BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation · DOI · quote verified

How many listed glaciers can meet 200 m-deep ocean water?

67 of 243, versus 32 in B2013 and 17 in RTopo-2.

Source: BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation · DOI · quote verified

What fraction of drainage area is newly more exposed to AW?

About 55% of ice-sheet drainage (vs 45% B2013, 35% RTopo-2).

Source: BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation · DOI · quote verified

Where is mass conservation applied?

Mostly where ice velocity exceeds 50 m/yr along the coast.

Source: BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation · DOI · quote verified

What Hayes Glacier lesson comes from the new bathymetry?

It left a ~200 m sill in 2005 into a retrograde bed and may retreat another 3 km.

Source: BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation · DOI · quote verified

How well did unconstrained v2 beds match new bathymetry?

For 70% of remapped glaciers, v2 was within 100 m of the new soundings.

Source: BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation · DOI · quote verified

What grid is the product assembled on?

150 m Polar Stereographic North; true resolution 150–1000 m by source.

Source: BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation · DOI · quote verified