Eurasian snow depth in long-term climate reanalyses

Snow cover variability has significant effects on local and global climate evolution. By changing surface energy fluxes and hydrological conditions, changes in snow cover can alter atmospheric circulation and lead to remote climate effects. To document such multi-scale climate effects, atmospheric r...

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Published in:The Cryosphere
Main Authors: Wegmann, Martin, Orsolini, Yvan, Dutra, Emanuel, Bulygina, Olga, Sterin, Alexander, Brönnimann, Stefan
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2017
Subjects:
Online Access:https://boris.unibe.ch/100216/1/tc-11-923-2017.pdf
https://boris.unibe.ch/100216/
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author Wegmann, Martin
Orsolini, Yvan
Dutra, Emanuel
Bulygina, Olga
Sterin, Alexander
Brönnimann, Stefan
author_facet Wegmann, Martin
Orsolini, Yvan
Dutra, Emanuel
Bulygina, Olga
Sterin, Alexander
Brönnimann, Stefan
author_sort Wegmann, Martin
collection BORIS (Bern Open Repository and Information System, University of Bern)
container_issue 2
container_start_page 923
container_title The Cryosphere
container_volume 11
description Snow cover variability has significant effects on local and global climate evolution. By changing surface energy fluxes and hydrological conditions, changes in snow cover can alter atmospheric circulation and lead to remote climate effects. To document such multi-scale climate effects, atmospheric reanalysis and derived products offer the opportunity to analyze snow variability in great detail far back to the early 20th century. So far only little is know about their quality. Comparing snow depth in four long-term reanalysis datasets with Russian in situ snow depth data, we find a moderately high daily correlation (around 0.6–0.7), which is comparable to correlations for the recent era (1981–2010), and a good representation of sub-decadal variability. However, the representation of pre-1950 inter-decadal snow variability is questionable, since reanalysis products divert towards different base states. Limited availability of independent long-term snow data makes it difficult to assess the exact cause for this bifurcation in snow states, but initial investigations point towards representation of the atmosphere rather than differences in assimilated data or snow schemes. This study demonstrates the ability of long-term reanalysis to reproduce snow variability accordingly.
format Article in Journal/Newspaper
genre The Cryosphere
genre_facet The Cryosphere
id ftunivbern:oai:boris.unibe.ch:100216
institution Open Polar
language English
op_collection_id ftunivbern
op_container_end_page 935
op_doi https://doi.org/10.5194/tc-11-923-2017
op_relation https://boris.unibe.ch/100216/
op_rights info:eu-repo/semantics/openAccess
op_source Wegmann, Martin; Orsolini, Yvan; Dutra, Emanuel; Bulygina, Olga; Sterin, Alexander; Brönnimann, Stefan (2017). Eurasian snow depth in long-term climate reanalyses. The Cryosphere, 11(2), pp. 923-935. Copernicus Publications 10.5194/tc-11-923-2017 <http://dx.doi.org/10.5194/tc-11-923-2017>
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spelling ftunivbern:oai:boris.unibe.ch:100216 2025-05-18T14:07:39+00:00 Eurasian snow depth in long-term climate reanalyses Wegmann, Martin Orsolini, Yvan Dutra, Emanuel Bulygina, Olga Sterin, Alexander Brönnimann, Stefan 2017 application/pdf https://boris.unibe.ch/100216/1/tc-11-923-2017.pdf https://boris.unibe.ch/100216/ eng eng Copernicus Publications https://boris.unibe.ch/100216/ info:eu-repo/semantics/openAccess Wegmann, Martin; Orsolini, Yvan; Dutra, Emanuel; Bulygina, Olga; Sterin, Alexander; Brönnimann, Stefan (2017). Eurasian snow depth in long-term climate reanalyses. The Cryosphere, 11(2), pp. 923-935. Copernicus Publications 10.5194/tc-11-923-2017 <http://dx.doi.org/10.5194/tc-11-923-2017> 910 Geography & travel info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed 2017 ftunivbern https://doi.org/10.5194/tc-11-923-2017 2025-04-28T06:49:44Z Snow cover variability has significant effects on local and global climate evolution. By changing surface energy fluxes and hydrological conditions, changes in snow cover can alter atmospheric circulation and lead to remote climate effects. To document such multi-scale climate effects, atmospheric reanalysis and derived products offer the opportunity to analyze snow variability in great detail far back to the early 20th century. So far only little is know about their quality. Comparing snow depth in four long-term reanalysis datasets with Russian in situ snow depth data, we find a moderately high daily correlation (around 0.6–0.7), which is comparable to correlations for the recent era (1981–2010), and a good representation of sub-decadal variability. However, the representation of pre-1950 inter-decadal snow variability is questionable, since reanalysis products divert towards different base states. Limited availability of independent long-term snow data makes it difficult to assess the exact cause for this bifurcation in snow states, but initial investigations point towards representation of the atmosphere rather than differences in assimilated data or snow schemes. This study demonstrates the ability of long-term reanalysis to reproduce snow variability accordingly. Article in Journal/Newspaper The Cryosphere BORIS (Bern Open Repository and Information System, University of Bern) The Cryosphere 11 2 923 935
spellingShingle 910 Geography & travel
Wegmann, Martin
Orsolini, Yvan
Dutra, Emanuel
Bulygina, Olga
Sterin, Alexander
Brönnimann, Stefan
Eurasian snow depth in long-term climate reanalyses
title Eurasian snow depth in long-term climate reanalyses
title_full Eurasian snow depth in long-term climate reanalyses
title_fullStr Eurasian snow depth in long-term climate reanalyses
title_full_unstemmed Eurasian snow depth in long-term climate reanalyses
title_short Eurasian snow depth in long-term climate reanalyses
title_sort eurasian snow depth in long-term climate reanalyses
topic 910 Geography & travel
topic_facet 910 Geography & travel
url https://boris.unibe.ch/100216/1/tc-11-923-2017.pdf
https://boris.unibe.ch/100216/