In 2007, Denmark launched the Programme for Monitoring of the Greenland Ice Sheet (PROMICE) to assess changes in the mass balance of the ice sheet. The two major contributors to the ice sheet mass loss are surface melt and a larger production of icebergs through faster ice flow. PROMICE is focused on both processes. Ice movement and discharge is tracked by satellites and GPSs. The surface mass balance is monitored by a network of weather stations in the melt zone of the ice sheet, providing ground truth data to calibrate mass budget models.

The Greenland Climate Network (GC-Net) was established in 1995 by Prof. Konrad Steffen at CIRES, to obtain knowledge of the mass gain and climatology of the ice sheet. The programme was funded by the USA until 2020, at which point Denmark assumed responsibility for the operation and maintenance of the weather station network. The snowfall and climatology are monitored by a network of weather stations in the accumulation zone of the ice sheet, supplemented by satellite-derived data products.

Together, the two monitoring programmes deliver data about the mass balance of the Greenland ice sheet in near real-time. Explore our project dataverses and datasets below.
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4,001 to 4,010 of 4,043 Results
Plain Text - 32.1 KB - MD5: 8419420c15384085350d08b5cb01005c
Plain Text - 23.3 KB - MD5: 05a21e6f72d6bddb31f399b50948cbc1
Unknown - 735.6 KB - MD5: 0801436a8bb9bed304734e91d74545a7
initial assessment (1995-2015)
Unknown - 370.9 KB - MD5: 2679a51ed8cca925642e0527653ad834
updated assessment (1995-2019)
Plain Text - 250.5 MB - MD5: 6ddff99d44514faccfaa4b7e358593dd
Basal melt rates as csv file
Unknown - 151.8 MB - MD5: b8c1c283e15bfc8021d3b33dfeb69137
Basal melt rates as MATLAB file
Unknown - 312.4 MB - MD5: b54b06952b4f512d649573953e844023
Basal melt rates as NetCDF file
Unknown - 156.2 MB - MD5: dc0a8aab973686d0f8e96ad68ee1f8d1
This file contains the individual heat sources used for calculating the basal melt.
Plain Text - 5.3 KB - MD5: b03b6fab67374b70aa37ea91ab304538
Calculating and plotting the basal melt rates from the heat sources.
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