A long-term Arctic snow depth record from Abisko, northern Sweden, 1913–2004

A newly digitized record of snow depth from the Abisko Scientifi c Research Station in northern Sweden covers the period 1913–present. Mean snow depths were taken from paper records of measurements made on a profi le comprising 10 permanent stakes. This long-term record yields snow depths consistent...

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Published in:Polar Research
Main Author: Jack Kohler, Ola Brandt
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2006
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/2042
https://doi.org/10.3402/polar.v25i2.6240
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spelling ftjpolarres:oai:journals.openacademia.net:article/2042 2023-05-15T12:59:10+02:00 A long-term Arctic snow depth record from Abisko, northern Sweden, 1913–2004 Jack Kohler, Ola Brandt 2006-06-01 application/pdf https://polarresearch.net/index.php/polar/article/view/2042 https://doi.org/10.3402/polar.v25i2.6240 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2042/5293 https://polarresearch.net/index.php/polar/article/view/2042 doi:10.3402/polar.v25i2.6240 Copyright (c) 2018 Polar Research Polar Research; Vol. 25 No. 2 (2006); 91-113 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2006 ftjpolarres https://doi.org/10.3402/polar.v25i2.6240 2021-11-11T19:11:56Z A newly digitized record of snow depth from the Abisko Scientifi c Research Station in northern Sweden covers the period 1913–present. Mean snow depths were taken from paper records of measurements made on a profi le comprising 10 permanent stakes. This long-term record yields snow depths consistent with two other shorter term Abisko records: measurements made at another 10-stake profi le (1974–present) and at a single stake (1956–present). The measurement interval is variable, ranging from daily to monthly, and there are no data for about half of the winter months in the period 1930–1956. To fi ll the gaps, we use a simple snowpack model driven by concurrent temperature and precipitation measurements at Abisko. Model snow depths are similar to observed; differences between the two records are comparable to those between profi le and single stake measurements. For both model and observed snow depth records, the most statistically signifi cant trend is in winter mean snow depths, amounting to an increase of about 2 cm or 5 % of the mean per decade over the whole measurement period, and 10 % per decade since the 1930–40s, but all seasonal means of snow depth show positive trends on the longest timescales. However, the start, end, and length of the snow season do not show any statistically signifi cant long-term trends. Finally, the relation between the Arctic Oscillation index and Abisko temperature, precipitation and snow depth is positive and highly signifi cant, with the best correlations for winter. Article in Journal/Newspaper Abisko Arctic Northern Sweden Polar Research Polar Research (E-Journal) Arctic Abisko ENVELOPE(18.829,18.829,68.349,68.349) Polar Research 25 2 91 113
institution Open Polar
collection Polar Research (E-Journal)
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language English
description A newly digitized record of snow depth from the Abisko Scientifi c Research Station in northern Sweden covers the period 1913–present. Mean snow depths were taken from paper records of measurements made on a profi le comprising 10 permanent stakes. This long-term record yields snow depths consistent with two other shorter term Abisko records: measurements made at another 10-stake profi le (1974–present) and at a single stake (1956–present). The measurement interval is variable, ranging from daily to monthly, and there are no data for about half of the winter months in the period 1930–1956. To fi ll the gaps, we use a simple snowpack model driven by concurrent temperature and precipitation measurements at Abisko. Model snow depths are similar to observed; differences between the two records are comparable to those between profi le and single stake measurements. For both model and observed snow depth records, the most statistically signifi cant trend is in winter mean snow depths, amounting to an increase of about 2 cm or 5 % of the mean per decade over the whole measurement period, and 10 % per decade since the 1930–40s, but all seasonal means of snow depth show positive trends on the longest timescales. However, the start, end, and length of the snow season do not show any statistically signifi cant long-term trends. Finally, the relation between the Arctic Oscillation index and Abisko temperature, precipitation and snow depth is positive and highly signifi cant, with the best correlations for winter.
format Article in Journal/Newspaper
author Jack Kohler, Ola Brandt
spellingShingle Jack Kohler, Ola Brandt
A long-term Arctic snow depth record from Abisko, northern Sweden, 1913–2004
author_facet Jack Kohler, Ola Brandt
author_sort Jack Kohler, Ola Brandt
title A long-term Arctic snow depth record from Abisko, northern Sweden, 1913–2004
title_short A long-term Arctic snow depth record from Abisko, northern Sweden, 1913–2004
title_full A long-term Arctic snow depth record from Abisko, northern Sweden, 1913–2004
title_fullStr A long-term Arctic snow depth record from Abisko, northern Sweden, 1913–2004
title_full_unstemmed A long-term Arctic snow depth record from Abisko, northern Sweden, 1913–2004
title_sort long-term arctic snow depth record from abisko, northern sweden, 1913–2004
publisher Norwegian Polar Institute
publishDate 2006
url https://polarresearch.net/index.php/polar/article/view/2042
https://doi.org/10.3402/polar.v25i2.6240
long_lat ENVELOPE(18.829,18.829,68.349,68.349)
geographic Arctic
Abisko
geographic_facet Arctic
Abisko
genre Abisko
Arctic
Northern Sweden
Polar Research
genre_facet Abisko
Arctic
Northern Sweden
Polar Research
op_source Polar Research; Vol. 25 No. 2 (2006); 91-113
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2042/5293
https://polarresearch.net/index.php/polar/article/view/2042
doi:10.3402/polar.v25i2.6240
op_rights Copyright (c) 2018 Polar Research
op_doi https://doi.org/10.3402/polar.v25i2.6240
container_title Polar Research
container_volume 25
container_issue 2
container_start_page 91
op_container_end_page 113
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