Summary We have produced an open and reproducible estimate of Greenland Ice Sheet solid ice discharge from 1986 through last month. Our results show three modes at the total ice-sheet scale: steady discharge from 1986 through 2000, increasing discharge from 2000 through 2005, and steady discharge from 2005 through last month. The behavior of individual sectors and glaciers is more complicated. This work was done to provide a 100 % reproducible estimate to help constrain mass balance and sea-level rise estimates.
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Comma Separated Values - 407.8 KB - MD5: e19b5377832fe24c7e445e68d8ceed95
Regional discharge. Git hash: 886d2c1
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Regional error. Git hash: 886d2c1
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Regional discharge, coverage, and error. Git hash: 886d2c1
Comma Separated Values - 3.4 MB - MD5: ecd40ab4781915515df534a0d34040e4
Sector coverage. Git hash: 886d2c1
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Sector discharge. Git hash: 886d2c1
Comma Separated Values - 9.6 MB - MD5: a4eece5e93fdca38d3005cea291738cd
Sector error. Git hash: 886d2c1
Plain Text - 7.0 MB - MD5: 53c68d468136b6744fa3201e4cff972c
Sector discharge, coverage, and error. Git hash: 886d2c1
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README. Git hash: 886d2c1
Comma Separated Values - 24.4 KB - MD5: de4de9831c35216eb9844213f609963a
Gate metadata. Git hash: 71a43044
Nov 29, 2024
Larsen, Signe Hillerup, 2024, "ESA CCI+ Phase 2 Mass Flux Ice Discharge ECV", https://doi.org/10.22008/FK2/T3Z6TU, GEUS Dataverse, V1
The Mass Flux and Ice Discharge (MFID) Essential Climate Variable (ECV) is produced as part of the ESA CCI+ Phase 2 project and currently updated every 2nd year. MFID is based on a forked version of the solid ice discharge algorithm using ice velocity and surface elevation data f...
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