Article (Scientific journals)
A long-term dataset of climatic mass balance, snow conditions, and runoff in Svalbard (1957-2018)
Van Pelt, Ward; Pohjola, Veijo; Pettersson, Rickard et al.
2019In The Cryosphere, 13 (9), p. 2259 - 2280
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Keywords :
Water Science and Technology; Earth-Surface Processes
Abstract :
[en] 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 1km-1km 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 (C0.09mw.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 (-0.06mw.e. a-1 decade-1), and an increase in the equilibrium line altitude (ELA) by 17m 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 (C1.4 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.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Van Pelt, Ward ;  Department of Earth Sciences, Uppsala University, Uppsala, Sweden
Pohjola, Veijo;  Department of Earth Sciences, Uppsala University, Uppsala, Sweden
Pettersson, Rickard ;  Department of Earth Sciences, Uppsala University, Uppsala, Sweden
Marchenko, Sergey;  Department of Earth Sciences, Uppsala University, Uppsala, Sweden
Kohler, Jack;  Norwegian Polar Institute, Tromsø, Norway
Luks, Bartłomiej ;  Institute of Geophysics, Polish Academy of Sciences, Warsaw, Poland
Ove Hagen, Jon;  Department of Geosciences, University of Oslo, Oslo, Norway
Schuler, Thomas V. ;  Department of Geosciences, University of Oslo, Oslo, Norway ; Department of Arctic Geophysics, University Centre in Svalbard, Longyearbyen, Svalbard, Norway
Dunse, Thorben;  Department of Geosciences, University of Oslo, Oslo, Norway ; Department of Environmental Sciences, Western Norway University of Applied Sciences, Sogndal, Norway
Noël, Brice  ;  Université de Liège - ULiège > Département de géographie > Climatologie et Topoclimatologie ; Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, Netherlands
Reijmer, Carleen ;  Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, Netherlands
Language :
English
Title :
A long-term dataset of climatic mass balance, snow conditions, and runoff in Svalbard (1957-2018)
Publication date :
03 September 2019
Journal title :
The Cryosphere
ISSN :
1994-0416
eISSN :
1994-0424
Publisher :
Copernicus GmbH
Volume :
13
Issue :
9
Pages :
2259 - 2280
Peer reviewed :
Peer Reviewed verified by ORBi
Funding text :
Financial support. This research has been supported by the
Available on ORBi :
since 21 April 2023

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