Past and future climate variations in the Norwegian Arctic: overview and novel analyses

Sparse stations and serious measuring problems hamper analyses of climatic conditions in the Arctic. This paper presents a discussion of measuring problems in the Arctic and gives an overview of observed past and projected future climate variations in Svalbard and Jan Mayen. Novel analyses of temper...

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Published in:Polar Research
Main Authors: Førland, Eirik J., Hanssen-Bauer, Inger
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2003
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/2103
https://doi.org/10.3402/polar.v22i2.6450
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spelling ftjpolarres:oai:journals.openacademia.net:article/2103 2024-09-09T19:20:58+00:00 Past and future climate variations in the Norwegian Arctic: overview and novel analyses Førland, Eirik J. Hanssen-Bauer, Inger 2003-01-12 application/pdf https://polarresearch.net/index.php/polar/article/view/2103 https://doi.org/10.3402/polar.v22i2.6450 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2103/5354 https://polarresearch.net/index.php/polar/article/view/2103 doi:10.3402/polar.v22i2.6450 Polar Research; Vol. 22 No. 2 (2003); 113-124 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2003 ftjpolarres https://doi.org/10.3402/polar.v22i2.6450 2024-06-28T03:10:15Z Sparse stations and serious measuring problems hamper analyses of climatic conditions in the Arctic. This paper presents a discussion of measuring problems in the Arctic and gives an overview of observed past and projected future climate variations in Svalbard and Jan Mayen. Novel analyses of temperature conditions during precipitation and trends in fractions of solid/liquid precipitation at the Arctic weather stations are also outlined. Analyses based on combined and homogenized series from the regular weather stations in the region indicate that the measured annual precipitation has increased by more than 2.5% per decade since the measurements started in the beginning of the 20th century. The annual temperature has increased in Svalbard and Jan Mayen during the latest decades, but the present level is still lower than in the 1930s. Downscaled scenarios for Svalbard Airport indicate a further increase in temperature and precipitation. Analyses based on observations of precipitation types at the regular weather stations demonstrate that the annual fraction of solid precipitation has decreased at all stations during the latest decades. The reduced fraction of solid precipitation implies that the undercatch of the precipitation gauges is reduced. Consequently, part of the observed increase in the annual precipitation is fictitious and is due to a larger part of the “true” precipitation being caught by the gauges. With continued warming in the region, this virtual increase will be measured in addition to an eventual real increase. Article in Journal/Newspaper Arctic Jan Mayen Polar Research Svalbard Polar Research Arctic Svalbard Jan Mayen Svalbard ENVELOPE(20.000,20.000,78.000,78.000) Polar Research 22 2 113 124
institution Open Polar
collection Polar Research
op_collection_id ftjpolarres
language English
description Sparse stations and serious measuring problems hamper analyses of climatic conditions in the Arctic. This paper presents a discussion of measuring problems in the Arctic and gives an overview of observed past and projected future climate variations in Svalbard and Jan Mayen. Novel analyses of temperature conditions during precipitation and trends in fractions of solid/liquid precipitation at the Arctic weather stations are also outlined. Analyses based on combined and homogenized series from the regular weather stations in the region indicate that the measured annual precipitation has increased by more than 2.5% per decade since the measurements started in the beginning of the 20th century. The annual temperature has increased in Svalbard and Jan Mayen during the latest decades, but the present level is still lower than in the 1930s. Downscaled scenarios for Svalbard Airport indicate a further increase in temperature and precipitation. Analyses based on observations of precipitation types at the regular weather stations demonstrate that the annual fraction of solid precipitation has decreased at all stations during the latest decades. The reduced fraction of solid precipitation implies that the undercatch of the precipitation gauges is reduced. Consequently, part of the observed increase in the annual precipitation is fictitious and is due to a larger part of the “true” precipitation being caught by the gauges. With continued warming in the region, this virtual increase will be measured in addition to an eventual real increase.
format Article in Journal/Newspaper
author Førland, Eirik J.
Hanssen-Bauer, Inger
spellingShingle Førland, Eirik J.
Hanssen-Bauer, Inger
Past and future climate variations in the Norwegian Arctic: overview and novel analyses
author_facet Førland, Eirik J.
Hanssen-Bauer, Inger
author_sort Førland, Eirik J.
title Past and future climate variations in the Norwegian Arctic: overview and novel analyses
title_short Past and future climate variations in the Norwegian Arctic: overview and novel analyses
title_full Past and future climate variations in the Norwegian Arctic: overview and novel analyses
title_fullStr Past and future climate variations in the Norwegian Arctic: overview and novel analyses
title_full_unstemmed Past and future climate variations in the Norwegian Arctic: overview and novel analyses
title_sort past and future climate variations in the norwegian arctic: overview and novel analyses
publisher Norwegian Polar Institute
publishDate 2003
url https://polarresearch.net/index.php/polar/article/view/2103
https://doi.org/10.3402/polar.v22i2.6450
long_lat ENVELOPE(20.000,20.000,78.000,78.000)
geographic Arctic
Svalbard
Jan Mayen
Svalbard
geographic_facet Arctic
Svalbard
Jan Mayen
Svalbard
genre Arctic
Jan Mayen
Polar Research
Svalbard
genre_facet Arctic
Jan Mayen
Polar Research
Svalbard
op_source Polar Research; Vol. 22 No. 2 (2003); 113-124
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2103/5354
https://polarresearch.net/index.php/polar/article/view/2103
doi:10.3402/polar.v22i2.6450
op_doi https://doi.org/10.3402/polar.v22i2.6450
container_title Polar Research
container_volume 22
container_issue 2
container_start_page 113
op_container_end_page 124
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