Identification of key processes in bridging the Arctic warming impact and its variation on decadal timescale (D3.2)
Summary: Observational analysis of the Arctic warming impacts: The key driver bridging the winter Arctic warming (1980 to 2014) impact to the Northern Hemisphere has been identified, my means of an advanced multi-variable statistical analysis, to be a tropospheric pathway, linking interannual variab...
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ftzenodo:oai:zenodo.org:3559466 2024-09-15T17:52:57+00:00 Identification of key processes in bridging the Arctic warming impact and its variation on decadal timescale (D3.2) Manzini, Elisa Ghosh, Rohit Matei, Daniela Gastineau, Guillaume Simon, Amélie Kwon, Young-Oh Yang, Shuting 2019-09-30 https://doi.org/10.5281/zenodo.3559466 eng eng Zenodo https://zenodo.org/communities/eu https://zenodo.org/communities/blue-actionh2020 https://doi.org/10.5281/zenodo.3559465 https://doi.org/10.5281/zenodo.3559466 oai:zenodo.org:3559466 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/report 2019 ftzenodo https://doi.org/10.5281/zenodo.355946610.5281/zenodo.3559465 2024-07-25T21:49:14Z Summary: Observational analysis of the Arctic warming impacts: The key driver bridging the winter Arctic warming (1980 to 2014) impact to the Northern Hemisphere has been identified, my means of an advanced multi-variable statistical analysis, to be a tropospheric pathway, linking interannual variability in Arctic warming to the Northern Hemisphere lower atmosphere variability with one month lag. Clearly, the analysis has shown, that the response to the pan-Arctic sea-ice changes does not involve the stratosphere. A covariation of sea-ice variability with Siberian snow cover may be responsible of previously proposed pathways of influences involving the stratosphere. In addition, the analysis suggests that the mechanism of the tropospheric pathway may include the intensification of the Ural anticyclone. Coordinated experiments on Arctic warming impact and its variation on decadal timescale: Warm Arctic Cold Eurasia in winter surface air temperature. Making use of the ensembles of atmospheric model experiment with and without Arctic sea ice forcing it has emerged that the large scale pattern of winter surface air temperature variability is an internal mode of atmospheric variability. At shorter time scales (interannual) the project models capture this internal mode of atmospheric variability. At longer time scales (multi-annual, decadal), however, the models fail to capture the variability/trend of the winter surface air temperature (over 1980-2014). Arctic sea-ice driven variability . Within the Arctic Circle, the sea-ice driven variability explains about 3% of the total variance for sea level pressure and about 23% for surface air temperature in boreal winter at interannual and longer time scales. Regionally, the sea-ice driven variability is 1-1.5 times as large as the variability driven by the other forcings over the Arctic and northern Eurasia. Contrasting Summer and Winter Impact of Arctic sea-ice loss. Large scale features of atmospheric circulation trends over the period 1980-2014 are not reproduced by ... Report Arctic Sea ice Zenodo |
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Open Polar |
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Zenodo |
op_collection_id |
ftzenodo |
language |
English |
description |
Summary: Observational analysis of the Arctic warming impacts: The key driver bridging the winter Arctic warming (1980 to 2014) impact to the Northern Hemisphere has been identified, my means of an advanced multi-variable statistical analysis, to be a tropospheric pathway, linking interannual variability in Arctic warming to the Northern Hemisphere lower atmosphere variability with one month lag. Clearly, the analysis has shown, that the response to the pan-Arctic sea-ice changes does not involve the stratosphere. A covariation of sea-ice variability with Siberian snow cover may be responsible of previously proposed pathways of influences involving the stratosphere. In addition, the analysis suggests that the mechanism of the tropospheric pathway may include the intensification of the Ural anticyclone. Coordinated experiments on Arctic warming impact and its variation on decadal timescale: Warm Arctic Cold Eurasia in winter surface air temperature. Making use of the ensembles of atmospheric model experiment with and without Arctic sea ice forcing it has emerged that the large scale pattern of winter surface air temperature variability is an internal mode of atmospheric variability. At shorter time scales (interannual) the project models capture this internal mode of atmospheric variability. At longer time scales (multi-annual, decadal), however, the models fail to capture the variability/trend of the winter surface air temperature (over 1980-2014). Arctic sea-ice driven variability . Within the Arctic Circle, the sea-ice driven variability explains about 3% of the total variance for sea level pressure and about 23% for surface air temperature in boreal winter at interannual and longer time scales. Regionally, the sea-ice driven variability is 1-1.5 times as large as the variability driven by the other forcings over the Arctic and northern Eurasia. Contrasting Summer and Winter Impact of Arctic sea-ice loss. Large scale features of atmospheric circulation trends over the period 1980-2014 are not reproduced by ... |
format |
Report |
author |
Manzini, Elisa Ghosh, Rohit Matei, Daniela Gastineau, Guillaume Simon, Amélie Kwon, Young-Oh Yang, Shuting |
spellingShingle |
Manzini, Elisa Ghosh, Rohit Matei, Daniela Gastineau, Guillaume Simon, Amélie Kwon, Young-Oh Yang, Shuting Identification of key processes in bridging the Arctic warming impact and its variation on decadal timescale (D3.2) |
author_facet |
Manzini, Elisa Ghosh, Rohit Matei, Daniela Gastineau, Guillaume Simon, Amélie Kwon, Young-Oh Yang, Shuting |
author_sort |
Manzini, Elisa |
title |
Identification of key processes in bridging the Arctic warming impact and its variation on decadal timescale (D3.2) |
title_short |
Identification of key processes in bridging the Arctic warming impact and its variation on decadal timescale (D3.2) |
title_full |
Identification of key processes in bridging the Arctic warming impact and its variation on decadal timescale (D3.2) |
title_fullStr |
Identification of key processes in bridging the Arctic warming impact and its variation on decadal timescale (D3.2) |
title_full_unstemmed |
Identification of key processes in bridging the Arctic warming impact and its variation on decadal timescale (D3.2) |
title_sort |
identification of key processes in bridging the arctic warming impact and its variation on decadal timescale (d3.2) |
publisher |
Zenodo |
publishDate |
2019 |
url |
https://doi.org/10.5281/zenodo.3559466 |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_relation |
https://zenodo.org/communities/eu https://zenodo.org/communities/blue-actionh2020 https://doi.org/10.5281/zenodo.3559465 https://doi.org/10.5281/zenodo.3559466 oai:zenodo.org:3559466 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode |
op_doi |
https://doi.org/10.5281/zenodo.355946610.5281/zenodo.3559465 |
_version_ |
1810294970064568320 |