Variations and changes in snow depth at meteorological stations Barentsburg and Hornsund (Spitsbergen)

In this study, seasonality and interannual variability of snow depth at two stations (Hornsund and Barentsburg) located in western Spitsbergen are investigated. For this purpose, the novel Moving Average over Shifting Horizon method combined with trend estimation was used. The Hornsund and Barentsbu...

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Published in:Annals of Glaciology
Main Authors: Marzena Osuch, Tomasz Wawrzyniak
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2017
Subjects:
Online Access:https://doi.org/10.1017/aog.2017.20
https://doaj.org/article/0ea4d05ac1bd4d9ca9b5b73c9e963ce3
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spelling ftdoajarticles:oai:doaj.org/article:0ea4d05ac1bd4d9ca9b5b73c9e963ce3 2023-05-15T13:29:30+02:00 Variations and changes in snow depth at meteorological stations Barentsburg and Hornsund (Spitsbergen) Marzena Osuch Tomasz Wawrzyniak 2017-07-01T00:00:00Z https://doi.org/10.1017/aog.2017.20 https://doaj.org/article/0ea4d05ac1bd4d9ca9b5b73c9e963ce3 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0260305517000209/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2017.20 0260-3055 1727-5644 https://doaj.org/article/0ea4d05ac1bd4d9ca9b5b73c9e963ce3 Annals of Glaciology, Vol 58, Pp 11-20 (2017) Arctic climate change snow accumulation snow depth Spitsbergen Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.1017/aog.2017.20 2023-03-12T01:31:57Z In this study, seasonality and interannual variability of snow depth at two stations (Hornsund and Barentsburg) located in western Spitsbergen are investigated. For this purpose, the novel Moving Average over Shifting Horizon method combined with trend estimation was used. The Hornsund and Barentsburg stations exhibit similar snow depth trends during early autumn and late spring when statistically significant decreases were estimated at both stations (for August 1984–July 2016). In the remaining period, there are differences in outcomes between stations. The results for Barentsburg from October till the end of May are characterised by the lack of a trend while at Hornsund decreases of snow depth were estimated. The largest changes occur in May when the snow depth was at its maximum. Differences in the estimated tendencies were explained with the help of a trend analysis for air temperature and precipitation. An analysis of maximum snow depth, snow onset date, snow disappearance date and snow-cover duration is included. The results of the assessment depend on the location, with a lack of statistically significant changes in Barentsburg, and later snow onset date, shorter duration and decrease of maximum depth in Hornsund. Article in Journal/Newspaper Annals of Glaciology Arctic Barentsburg Climate change Hornsund Spitsbergen Directory of Open Access Journals: DOAJ Articles Arctic Hornsund ENVELOPE(15.865,15.865,76.979,76.979) Barentsburg ENVELOPE(14.212,14.212,78.064,78.064) Annals of Glaciology 58 75pt1 11 20
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Arctic
climate change
snow accumulation
snow depth
Spitsbergen
Meteorology. Climatology
QC851-999
spellingShingle Arctic
climate change
snow accumulation
snow depth
Spitsbergen
Meteorology. Climatology
QC851-999
Marzena Osuch
Tomasz Wawrzyniak
Variations and changes in snow depth at meteorological stations Barentsburg and Hornsund (Spitsbergen)
topic_facet Arctic
climate change
snow accumulation
snow depth
Spitsbergen
Meteorology. Climatology
QC851-999
description In this study, seasonality and interannual variability of snow depth at two stations (Hornsund and Barentsburg) located in western Spitsbergen are investigated. For this purpose, the novel Moving Average over Shifting Horizon method combined with trend estimation was used. The Hornsund and Barentsburg stations exhibit similar snow depth trends during early autumn and late spring when statistically significant decreases were estimated at both stations (for August 1984–July 2016). In the remaining period, there are differences in outcomes between stations. The results for Barentsburg from October till the end of May are characterised by the lack of a trend while at Hornsund decreases of snow depth were estimated. The largest changes occur in May when the snow depth was at its maximum. Differences in the estimated tendencies were explained with the help of a trend analysis for air temperature and precipitation. An analysis of maximum snow depth, snow onset date, snow disappearance date and snow-cover duration is included. The results of the assessment depend on the location, with a lack of statistically significant changes in Barentsburg, and later snow onset date, shorter duration and decrease of maximum depth in Hornsund.
format Article in Journal/Newspaper
author Marzena Osuch
Tomasz Wawrzyniak
author_facet Marzena Osuch
Tomasz Wawrzyniak
author_sort Marzena Osuch
title Variations and changes in snow depth at meteorological stations Barentsburg and Hornsund (Spitsbergen)
title_short Variations and changes in snow depth at meteorological stations Barentsburg and Hornsund (Spitsbergen)
title_full Variations and changes in snow depth at meteorological stations Barentsburg and Hornsund (Spitsbergen)
title_fullStr Variations and changes in snow depth at meteorological stations Barentsburg and Hornsund (Spitsbergen)
title_full_unstemmed Variations and changes in snow depth at meteorological stations Barentsburg and Hornsund (Spitsbergen)
title_sort variations and changes in snow depth at meteorological stations barentsburg and hornsund (spitsbergen)
publisher Cambridge University Press
publishDate 2017
url https://doi.org/10.1017/aog.2017.20
https://doaj.org/article/0ea4d05ac1bd4d9ca9b5b73c9e963ce3
long_lat ENVELOPE(15.865,15.865,76.979,76.979)
ENVELOPE(14.212,14.212,78.064,78.064)
geographic Arctic
Hornsund
Barentsburg
geographic_facet Arctic
Hornsund
Barentsburg
genre Annals of Glaciology
Arctic
Barentsburg
Climate change
Hornsund
Spitsbergen
genre_facet Annals of Glaciology
Arctic
Barentsburg
Climate change
Hornsund
Spitsbergen
op_source Annals of Glaciology, Vol 58, Pp 11-20 (2017)
op_relation https://www.cambridge.org/core/product/identifier/S0260305517000209/type/journal_article
https://doaj.org/toc/0260-3055
https://doaj.org/toc/1727-5644
doi:10.1017/aog.2017.20
0260-3055
1727-5644
https://doaj.org/article/0ea4d05ac1bd4d9ca9b5b73c9e963ce3
op_doi https://doi.org/10.1017/aog.2017.20
container_title Annals of Glaciology
container_volume 58
container_issue 75pt1
container_start_page 11
op_container_end_page 20
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