Water balance investigations in Svalbard
This paper reviews and summarizes all known previous water balance studies in Svalbard. An updated water balance computation was then done for the three water catchments with the best data: Bayelva, De Geerdalen and Isdammen/Endalen for 10 hydrological years 1990-2001. The computations were based on...
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Norwegian Polar Institute
2003
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ftjpolarres:oai:journals.openacademia.net:article/2106 2024-09-15T18:07:56+00:00 Water balance investigations in Svalbard Killingtveit, Ånund Pettersson, Lars-Evan Sand, Knut 2003-01-12 application/pdf https://polarresearch.net/index.php/polar/article/view/2106 https://doi.org/10.3402/polar.v22i2.6453 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2106/5357 https://polarresearch.net/index.php/polar/article/view/2106 doi:10.3402/polar.v22i2.6453 Polar Research; Vol. 22 No. 2 (2003); 161-174 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2003 ftjpolarres https://doi.org/10.3402/polar.v22i2.6453 2024-06-28T03:10:15Z This paper reviews and summarizes all known previous water balance studies in Svalbard. An updated water balance computation was then done for the three water catchments with the best data: Bayelva, De Geerdalen and Isdammen/Endalen for 10 hydrological years 1990-2001. The computations were based on the best available data and correction methods. Special emphasis was put on correction of precipitation data, both for catch errors and gradients in precipitation. Areal precipitation in the three catchments is more than two times the measured precipitation at the closest meteorological station: 548 mm/year in De Geerdalen, 486 mm/year in Endalen/Isdammen and 890 mm/year in Bayelva. Compared to this, average measured precipitation is only 199 mm/year at Svalbard Airport, close to Endalen/Isdammen and De Geerdalen, and 426 mm/year in Ny-Ålesund, close to Bayelva. Evaporation is not well understood in Svalbard; the best estimates indicate an average annual evaporation of ca. 80 mm/year from glacier-free areas, and no net evaporation from glaciers. Glacial mass balance has in general been negative in Svalbard during the last 40 years, leading to a significant contribution to the water balance, on the order of 450 mm/year on average. Annual runoff ranges from 545 mm in Endalen/Isdammen, 539 mm/year in De Geerdalen up to 1050 mm/year in Bayelva. Runoff computed from water balance compares well with observed runoff, and average error in water balance is less than ±30 mm/year in all three catchments. Article in Journal/Newspaper glacier Ny Ålesund Ny-Ålesund Polar Research Svalbard Polar Research Polar Research 22 2 161 174 |
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English |
description |
This paper reviews and summarizes all known previous water balance studies in Svalbard. An updated water balance computation was then done for the three water catchments with the best data: Bayelva, De Geerdalen and Isdammen/Endalen for 10 hydrological years 1990-2001. The computations were based on the best available data and correction methods. Special emphasis was put on correction of precipitation data, both for catch errors and gradients in precipitation. Areal precipitation in the three catchments is more than two times the measured precipitation at the closest meteorological station: 548 mm/year in De Geerdalen, 486 mm/year in Endalen/Isdammen and 890 mm/year in Bayelva. Compared to this, average measured precipitation is only 199 mm/year at Svalbard Airport, close to Endalen/Isdammen and De Geerdalen, and 426 mm/year in Ny-Ålesund, close to Bayelva. Evaporation is not well understood in Svalbard; the best estimates indicate an average annual evaporation of ca. 80 mm/year from glacier-free areas, and no net evaporation from glaciers. Glacial mass balance has in general been negative in Svalbard during the last 40 years, leading to a significant contribution to the water balance, on the order of 450 mm/year on average. Annual runoff ranges from 545 mm in Endalen/Isdammen, 539 mm/year in De Geerdalen up to 1050 mm/year in Bayelva. Runoff computed from water balance compares well with observed runoff, and average error in water balance is less than ±30 mm/year in all three catchments. |
format |
Article in Journal/Newspaper |
author |
Killingtveit, Ånund Pettersson, Lars-Evan Sand, Knut |
spellingShingle |
Killingtveit, Ånund Pettersson, Lars-Evan Sand, Knut Water balance investigations in Svalbard |
author_facet |
Killingtveit, Ånund Pettersson, Lars-Evan Sand, Knut |
author_sort |
Killingtveit, Ånund |
title |
Water balance investigations in Svalbard |
title_short |
Water balance investigations in Svalbard |
title_full |
Water balance investigations in Svalbard |
title_fullStr |
Water balance investigations in Svalbard |
title_full_unstemmed |
Water balance investigations in Svalbard |
title_sort |
water balance investigations in svalbard |
publisher |
Norwegian Polar Institute |
publishDate |
2003 |
url |
https://polarresearch.net/index.php/polar/article/view/2106 https://doi.org/10.3402/polar.v22i2.6453 |
genre |
glacier Ny Ålesund Ny-Ålesund Polar Research Svalbard |
genre_facet |
glacier Ny Ålesund Ny-Ålesund Polar Research Svalbard |
op_source |
Polar Research; Vol. 22 No. 2 (2003); 161-174 1751-8369 |
op_relation |
https://polarresearch.net/index.php/polar/article/view/2106/5357 https://polarresearch.net/index.php/polar/article/view/2106 doi:10.3402/polar.v22i2.6453 |
op_doi |
https://doi.org/10.3402/polar.v22i2.6453 |
container_title |
Polar Research |
container_volume |
22 |
container_issue |
2 |
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161 |
op_container_end_page |
174 |
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1810445301141471232 |