Observed snow depth trends in the European Alps: 1971 to 2019
Michael Matiu, Alice Crespi, Giacomo Bertoldi, Carlo Maria Carmagnola, Christoph Marty, Samuel Morin, Wolfgang Schöner, Daniele Cat Berro, Gabriele Chiogna, Ludovica De Gregorio, Sven Kotlarski, Bruno Majone, Gernot Resch, Silvia Terzago, Mauro Valt, Walter Beozzo, Paola Cianfarra, Isabelle Gouttevin, Giorgia Marcolini, Claudia Notarnicola, Marcello Petitta, Simon C. Scherrer, Ulrich Strasser, Michael Winkler, Marc Zebisch, A. Cicogna, R. Cremonini, Andrea Debernardi, Mattia Faletto, Mauro Gaddo, Lorenzo Giovannini, Luca Mercalli, Jean Michel Soubeyroux, Andrea Sušnik, Alberto Trenti, Stefano Urbani, Viktor Weilguni
Abstract
Abstract. The European Alps stretch over a range of climate zones which affect the spatial distribution of snow. Previous analyses of station observations of snow were confined to regional analyses. Here, we present an Alpine-wide analysis of snow depth from six Alpine countries – Austria, France, Germany, Italy, Slovenia, and Switzerland – including altogether more than 2000 stations of which more than 800 were used for the trend assessment. Using a principal component analysis and k-means clustering, we identified five main modes of variability and five regions which match the climatic forcing zones: north and high Alpine, north-east, north-west, south-east, and south and high Alpine. Linear trends of monthly mean snow depth between 1971 and 2019 showed decreases in snow depth for most stations from November to May. The average trend among all stations for seasonal (November to May) mean snow depth was −8.4 % per decade, for seasonal maximum snow depth −5.6 % per decade, and for seasonal snow cover duration −5.6 % per decade. Stronger and more significant trends were observed for periods and elevations where the transition from snow to snow-free occurs, which is consistent with an enhanced albedo feedback. Additionally, regional trends differed substantially at the same elevation, which challenges the notion of generalizing results from one region to another or to the whole Alps. This study presents an analysis of station snow depth series with the most comprehensive spatial coverage in the European Alps to date.- Cite:
- Michael Matiu, Alice Crespi, Giacomo Bertoldi, Carlo Maria Carmagnola, Christoph Marty, Samuel Morin, Wolfgang Schöner, Daniele Cat Berro, Gabriele Chiogna, Ludovica De Gregorio, Sven Kotlarski, Bruno Majone, Gernot Resch, Silvia Terzago, Mauro Valt, Walter Beozzo, Paola Cianfarra, Isabelle Gouttevin, Giorgia Marcolini, et al.. 2021. Observed snow depth trends in the European Alps: 1971 to 2019. The Cryosphere, Volume 15, Issue 3, 15(3):1343–1382.
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@article{Matiu-2021-Observed,
title = "Observed snow depth trends in the European Alps: 1971 to 2019",
author = {Matiu, Michael and
Crespi, Alice and
Bertoldi, Giacomo and
Carmagnola, Carlo Maria and
Marty, Christoph and
Morin, Samuel and
Sch{\"o}ner, Wolfgang and
Berro, Daniele Cat and
Chiogna, Gabriele and
Gregorio, Ludovica De and
Kotlarski, Sven and
Majone, Bruno and
Resch, Gernot and
Terzago, Silvia and
Valt, Mauro and
Beozzo, Walter and
Cianfarra, Paola and
Gouttevin, Isabelle and
Marcolini, Giorgia and
Notarnicola, Claudia and
Petitta, Marcello and
Scherrer, Simon C. and
Strasser, Ulrich and
Winkler, Michael and
Zebisch, Marc and
Cicogna, A. and
Cremonini, R. and
Debernardi, Andrea and
Faletto, Mattia and
Gaddo, Mauro and
Giovannini, Lorenzo and
Mercalli, Luca and
Soubeyroux, Jean Michel and
Su{\v{s}}nik, Andrea and
Trenti, Alberto and
Urbani, Stefano and
Weilguni, Viktor},
journal = "The Cryosphere, Volume 15, Issue 3",
volume = "15",
number = "3",
year = "2021",
publisher = "Copernicus GmbH",
url = "https://gwf-uwaterloo.github.io/gwf-publications/G21-74001",
doi = "10.5194/tc-15-1343-2021",
pages = "1343--1382",
abstract = "Abstract. The European Alps stretch over a range of climate zones which affect the spatial distribution of snow. Previous analyses of station observations of snow were confined to regional analyses. Here, we present an Alpine-wide analysis of snow depth from six Alpine countries {--} Austria, France, Germany, Italy, Slovenia, and Switzerland {--} including altogether more than 2000 stations of which more than 800 were used for the trend assessment. Using a principal component analysis and k-means clustering, we identified five main modes of variability and five regions which match the climatic forcing zones: north and high Alpine, north-east, north-west, south-east, and south and high Alpine. Linear trends of monthly mean snow depth between 1971 and 2019 showed decreases in snow depth for most stations from November to May. The average trend among all stations for seasonal (November to May) mean snow depth was −8.4 {\%} per decade, for seasonal maximum snow depth −5.6 {\%} per decade, and for seasonal snow cover duration −5.6 {\%} per decade. Stronger and more significant trends were observed for periods and elevations where the transition from snow to snow-free occurs, which is consistent with an enhanced albedo feedback. Additionally, regional trends differed substantially at the same elevation, which challenges the notion of generalizing results from one region to another or to the whole Alps. This study presents an analysis of station snow depth series with the most comprehensive spatial coverage in the European Alps to date.",
}
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<abstract>Abstract. The European Alps stretch over a range of climate zones which affect the spatial distribution of snow. Previous analyses of station observations of snow were confined to regional analyses. Here, we present an Alpine-wide analysis of snow depth from six Alpine countries – Austria, France, Germany, Italy, Slovenia, and Switzerland – including altogether more than 2000 stations of which more than 800 were used for the trend assessment. Using a principal component analysis and k-means clustering, we identified five main modes of variability and five regions which match the climatic forcing zones: north and high Alpine, north-east, north-west, south-east, and south and high Alpine. Linear trends of monthly mean snow depth between 1971 and 2019 showed decreases in snow depth for most stations from November to May. The average trend among all stations for seasonal (November to May) mean snow depth was −8.4 % per decade, for seasonal maximum snow depth −5.6 % per decade, and for seasonal snow cover duration −5.6 % per decade. Stronger and more significant trends were observed for periods and elevations where the transition from snow to snow-free occurs, which is consistent with an enhanced albedo feedback. Additionally, regional trends differed substantially at the same elevation, which challenges the notion of generalizing results from one region to another or to the whole Alps. This study presents an analysis of station snow depth series with the most comprehensive spatial coverage in the European Alps to date.</abstract>
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%0 Journal Article %T Observed snow depth trends in the European Alps: 1971 to 2019 %A Matiu, Michael %A Crespi, Alice %A Bertoldi, Giacomo %A Carmagnola, Carlo Maria %A Marty, Christoph %A Morin, Samuel %A Schöner, Wolfgang %A Berro, Daniele Cat %A Chiogna, Gabriele %A Gregorio, Ludovica De %A Kotlarski, Sven %A Majone, Bruno %A Resch, Gernot %A Terzago, Silvia %A Valt, Mauro %A Beozzo, Walter %A Cianfarra, Paola %A Gouttevin, Isabelle %A Marcolini, Giorgia %A Notarnicola, Claudia %A Petitta, Marcello %A Scherrer, Simon C. %A Strasser, Ulrich %A Winkler, Michael %A Zebisch, Marc %A Cicogna, A. %A Cremonini, R. %A Debernardi, Andrea %A Faletto, Mattia %A Gaddo, Mauro %A Giovannini, Lorenzo %A Mercalli, Luca %A Soubeyroux, Jean Michel %A Sušnik, Andrea %A Trenti, Alberto %A Urbani, Stefano %A Weilguni, Viktor %J The Cryosphere, Volume 15, Issue 3 %D 2021 %V 15 %N 3 %I Copernicus GmbH %F Matiu-2021-Observed %X Abstract. The European Alps stretch over a range of climate zones which affect the spatial distribution of snow. Previous analyses of station observations of snow were confined to regional analyses. Here, we present an Alpine-wide analysis of snow depth from six Alpine countries – Austria, France, Germany, Italy, Slovenia, and Switzerland – including altogether more than 2000 stations of which more than 800 were used for the trend assessment. Using a principal component analysis and k-means clustering, we identified five main modes of variability and five regions which match the climatic forcing zones: north and high Alpine, north-east, north-west, south-east, and south and high Alpine. Linear trends of monthly mean snow depth between 1971 and 2019 showed decreases in snow depth for most stations from November to May. The average trend among all stations for seasonal (November to May) mean snow depth was −8.4 % per decade, for seasonal maximum snow depth −5.6 % per decade, and for seasonal snow cover duration −5.6 % per decade. Stronger and more significant trends were observed for periods and elevations where the transition from snow to snow-free occurs, which is consistent with an enhanced albedo feedback. Additionally, regional trends differed substantially at the same elevation, which challenges the notion of generalizing results from one region to another or to the whole Alps. This study presents an analysis of station snow depth series with the most comprehensive spatial coverage in the European Alps to date. %R 10.5194/tc-15-1343-2021 %U https://gwf-uwaterloo.github.io/gwf-publications/G21-74001 %U https://doi.org/10.5194/tc-15-1343-2021 %P 1343-1382
Markdown (Informal)
[Observed snow depth trends in the European Alps: 1971 to 2019](https://gwf-uwaterloo.github.io/gwf-publications/G21-74001) (Matiu et al., GWF 2021)
- Observed snow depth trends in the European Alps: 1971 to 2019 (Matiu et al., GWF 2021)
ACL
- Michael Matiu, Alice Crespi, Giacomo Bertoldi, Carlo Maria Carmagnola, Christoph Marty, Samuel Morin, Wolfgang Schöner, Daniele Cat Berro, Gabriele Chiogna, Ludovica De Gregorio, Sven Kotlarski, Bruno Majone, Gernot Resch, Silvia Terzago, Mauro Valt, Walter Beozzo, Paola Cianfarra, Isabelle Gouttevin, Giorgia Marcolini, et al.. 2021. Observed snow depth trends in the European Alps: 1971 to 2019. The Cryosphere, Volume 15, Issue 3, 15(3):1343–1382.