A long-term dataset of climatic mass balance, snow conditions, and runoff in Svalbard (1957–2018)

• Published in: The Cryosphere
• Main Authors: van Pelt, Ward, Pohjola, Veijo, Pettersson, Rickard, Marchenko, Sergey, Kohler, Jack, Luks, Bartłomiej, Hagen, Jon Ove, Schuler, Thomas V., Dunse, Thorben, Noël, Brice, Reijmer, Carleen
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2019
• Subjects: article; Verlagsveröffentlichung; Ela; Svalbard; glacier; The Cryosphere
• Online Access: https://doi.org/10.5194/tc-13-2259-2019; https://noa.gwlb.de/receive/cop_mods_00000066; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00000047/tc-13-2259-2019.pdf; https://tc.copernicus.org/articles/13/2259/2019/tc-13-2259-2019.pdf

The climate in Svalbard is undergoing amplified change compared to the global mean. This has major implications for runoff from glaciers and seasonal snow on land. We use a coupled energy balance–subsurface model, forced with downscaled regional climate model fields, and apply it to both glacier-covered and land areas in Svalbard. This generates a long-term (1957–2018) distributed dataset of climatic mass balance (CMB) for the glaciers, snow conditions, and runoff with a 1 km×1 km spatial and 3-hourly temporal resolution. Observational data including stake measurements, automatic weather station data, and subsurface data across Svalbard are used for model calibration and validation. We find a weakly positive mean net CMB (+0.09 m w.e. a−1) over the simulation period, which only fractionally compensates for mass loss through calving. Pronounced warming and a small precipitation increase lead to a spatial-mean negative net CMB trend (−0.06 m w.e. a−1 decade−1), and an increase in the equilibrium line altitude (ELA) by 17 m decade−1, with the largest changes in southern and central Svalbard. The retreating ELA in turn causes firn air volume to decrease by 4 % decade−1, which in combination with winter warming induces a substantial reduction of refreezing in both glacier-covered and land areas (average −4 % decade−1). A combination of increased melt and reduced refreezing causes glacier runoff (average 34.3 Gt a−1) to double over the simulation period, while discharge from land (average 10.6 Gt a−1) remains nearly unchanged. As a result, the relative contribution of land runoff to total runoff drops from 30 % to 20 % during 1957–2018. Seasonal snow on land and in glacier ablation zones is found to arrive later in autumn (+1.4 d decade−1), while no significant changes occurred on the date of snow disappearance in spring–summer. Altogether, the output of the simulation provides an extensive dataset that may be of use in a wide range of applications ranging from runoff modelling to ecosystem studies.