Historical snow and ice temperature observations document the recent warming of the Greenland ice sheet

• Main Authors: Vandecrux, Baptiste, Fausto, Robert S., Box, Jason E., Covi, Federico, Hock, Regine, Rennermalm, Asa K., Heilig, Achim, Abermann, Jakob, As, Dirk, Bjerre, Elisa, Fettweis, Xavier, Smeets, Paul C. J. P., Kuipers Munneke, Peter, Broeke, Michiel R., Brils, Max, Langen, Peter L., Mottram, Ruth, Ahlstrøm, Andreas P.
• Format: Text
• Language: English
• Published: 2023
• Subjects: Arctic; Greenland; Ice Sheet
• Online Access: https://doi.org/10.5194/tc-2023-105; https://tc.copernicus.org/preprints/tc-2023-105/

The surface melting of the Greenland ice sheet has been increasing over the last decades due to Arctic atmospheric warming. Surface melt depends on the energy balance which includes the atmospheric forcing but also the thermal budget of the snow, firn and ice near the ice sheet surface. We present a compilation of more than 4500 measurements of ice, snow and firn temperature at 10 m below the surface (T 10m ) across Greenland spanning from 1912 to 2022. The measurements are either instantaneous or monthly averages. We train an Artificial Neural Network model (ANN) on these observations, weighted by their relative representativity, and use it to reconstruct T 10m over the entire Greenland ice sheet. We use 10 year averages and mean annual values of air temperature and snowfall from the ERA5 reanalysis dataset (1950–2022) as model input. The ANN indicates a Greenland-wide positive trend of T 10m at 0.2 °C decade -1 during the 1950–2022 period, with a cooling during 1950–1985 (-0.3 °C decade -1 ) followed by a warming during 1985–2022 (+0.7 °C decade -1 ). Regional climate models HIRHAM5, RACMO2.3p2 and MARv3.12 show mixed results compared to the observational T 10m dataset with mean differences ranging from -0.4 °C (HIRHAM) to 1.3 °C (MAR) and root mean squared differences ranging from 2.8 °C (HIRHAM) to 4.7 °C (MAR). The corresponding values for the ANN are -0.2 °C and 1.7 °C. The observation-based ANN also reveals an underestimation of the subsurface warming trends in climate models for the bare ice and dry snow areas. The subsurface warming brings the Greenland ice sheet surface closer to the melting point, reducing the amount of summer energy input required for melting. Our compilation documents the response of the ice sheet subsurface to atmospheric warming and will enable further improvements of models used for ice sheet mass loss assessment and reduce the uncertainty in projections.