Eurasian autumn snow impact on winter North Atlantic Oscillation depends on cryospheric variability
In recent years, many components of the connection between Eurasian autumn snow cover and wintertime North Atlantic Oscillation (NAO) were investigated, suggesting that November snow cover distribution has strong prediction power for the upcoming Northern Hemisphere winter climate. However, non-stat...
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ftcopernicus:oai:publications.copernicus.org:esdd81567 2023-05-15T16:59:54+02:00 Eurasian autumn snow impact on winter North Atlantic Oscillation depends on cryospheric variability Wegmann, Martin Rohrer, Marco Santolaria-Otín, María Lohmann, Gerrit 2019-11-20 application/pdf https://doi.org/10.5194/esd-2019-68 https://www.earth-syst-dynam-discuss.net/esd-2019-68/ eng eng doi:10.5194/esd-2019-68 https://www.earth-syst-dynam-discuss.net/esd-2019-68/ eISSN: 2190-4987 Text 2019 ftcopernicus https://doi.org/10.5194/esd-2019-68 2019-12-24T09:48:12Z In recent years, many components of the connection between Eurasian autumn snow cover and wintertime North Atlantic Oscillation (NAO) were investigated, suggesting that November snow cover distribution has strong prediction power for the upcoming Northern Hemisphere winter climate. However, non-stationarity of this relationship could impact its use for prediction routines. Here we use snow products from long-term reanalyses to investigate interannual and interdecadal links between autumnal snow cover and atmospheric conditions in winter. We find evidence for a negative NAO tendency after November with a strong west-to-east snow cover gradient, which is valid throughout the last 150 years. This correlation is linked with a consistent impact of November snow on a slowed stratospheric polar vortex. Nevertheless, interdecadal variability for this relationship shows episodes of decreased correlation power, which co-occur with episodes of low variability in the November snow index. We find that the same is also true for sea ice as an NAO predictor. The snow dipole itself is associated with reduced Barents-Kara sea ice concentration, increased Ural blocking frequency and negative temperature anomalies in eastern Eurasia. Increased sea ice variability in recent years is linked to increased snow variability, thus increasing its power in predicting the winter NAO. Text Kara Sea North Atlantic North Atlantic oscillation Sea ice Copernicus Publications: E-Journals Kara Sea |
institution |
Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
In recent years, many components of the connection between Eurasian autumn snow cover and wintertime North Atlantic Oscillation (NAO) were investigated, suggesting that November snow cover distribution has strong prediction power for the upcoming Northern Hemisphere winter climate. However, non-stationarity of this relationship could impact its use for prediction routines. Here we use snow products from long-term reanalyses to investigate interannual and interdecadal links between autumnal snow cover and atmospheric conditions in winter. We find evidence for a negative NAO tendency after November with a strong west-to-east snow cover gradient, which is valid throughout the last 150 years. This correlation is linked with a consistent impact of November snow on a slowed stratospheric polar vortex. Nevertheless, interdecadal variability for this relationship shows episodes of decreased correlation power, which co-occur with episodes of low variability in the November snow index. We find that the same is also true for sea ice as an NAO predictor. The snow dipole itself is associated with reduced Barents-Kara sea ice concentration, increased Ural blocking frequency and negative temperature anomalies in eastern Eurasia. Increased sea ice variability in recent years is linked to increased snow variability, thus increasing its power in predicting the winter NAO. |
format |
Text |
author |
Wegmann, Martin Rohrer, Marco Santolaria-Otín, María Lohmann, Gerrit |
spellingShingle |
Wegmann, Martin Rohrer, Marco Santolaria-Otín, María Lohmann, Gerrit Eurasian autumn snow impact on winter North Atlantic Oscillation depends on cryospheric variability |
author_facet |
Wegmann, Martin Rohrer, Marco Santolaria-Otín, María Lohmann, Gerrit |
author_sort |
Wegmann, Martin |
title |
Eurasian autumn snow impact on winter North Atlantic Oscillation depends on cryospheric variability |
title_short |
Eurasian autumn snow impact on winter North Atlantic Oscillation depends on cryospheric variability |
title_full |
Eurasian autumn snow impact on winter North Atlantic Oscillation depends on cryospheric variability |
title_fullStr |
Eurasian autumn snow impact on winter North Atlantic Oscillation depends on cryospheric variability |
title_full_unstemmed |
Eurasian autumn snow impact on winter North Atlantic Oscillation depends on cryospheric variability |
title_sort |
eurasian autumn snow impact on winter north atlantic oscillation depends on cryospheric variability |
publishDate |
2019 |
url |
https://doi.org/10.5194/esd-2019-68 https://www.earth-syst-dynam-discuss.net/esd-2019-68/ |
geographic |
Kara Sea |
geographic_facet |
Kara Sea |
genre |
Kara Sea North Atlantic North Atlantic oscillation Sea ice |
genre_facet |
Kara Sea North Atlantic North Atlantic oscillation Sea ice |
op_source |
eISSN: 2190-4987 |
op_relation |
doi:10.5194/esd-2019-68 https://www.earth-syst-dynam-discuss.net/esd-2019-68/ |
op_doi |
https://doi.org/10.5194/esd-2019-68 |
_version_ |
1766052526725005312 |