How strong is influence of the tropics and midlatitudes on the Arctic atmospheric circulation and climate change?
Relaxation experiments with the atmosphere model from European Centre for Medium‐range Weather Forecasts are analyzed to understand influence of lower latitudes (south of about 52 °N) on climate variability and change over the Arctic region. Interannual variability of the Arctic troposphere is impac...
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ftdatacite:10.5281/zenodo.3565629 2023-05-15T14:33:56+02:00 How strong is influence of the tropics and midlatitudes on the Arctic atmospheric circulation and climate change? Ye, Kunhui Jung, Thomas 2019 https://dx.doi.org/10.5281/zenodo.3565629 https://zenodo.org/record/3565629 unknown Zenodo https://zenodo.org/communities/applicate https://dx.doi.org/10.5281/zenodo.3565630 https://zenodo.org/communities/applicate Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess CC-BY Text Journal article article-journal ScholarlyArticle 2019 ftdatacite https://doi.org/10.5281/zenodo.3565629 https://doi.org/10.5281/zenodo.3565630 2021-11-05T12:55:41Z Relaxation experiments with the atmosphere model from European Centre for Medium‐range Weather Forecasts are analyzed to understand influence of lower latitudes (south of about 52 °N) on climate variability and change over the Arctic region. Interannual variability of the Arctic troposphere is impacted strongly by both the tropics and the midlatitudes. In general, the link in winter is stronger than that in summer. Furthermore, the tropics and midlatitudes have different preferred pathways by which they influence the Arctic. Trend analysis suggests that winter surface warming trends over the Arctic are driven strongly by the local sea ice‐atmospheric interaction. Warming at higher altitudes is strongly tied to remote non‐Arctic drivers, with some local amplification. Summer warming trends in northeastern Canada and Greenland are driven strongly by sea surface temperature/sea ice changes and partly by the tropics. The summer warming in northern Europe and western Russia is more strongly driven by the midlatitudes. Text Arctic Climate change Greenland Sea ice DataCite Metadata Store (German National Library of Science and Technology) Arctic Canada Greenland |
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DataCite Metadata Store (German National Library of Science and Technology) |
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ftdatacite |
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description |
Relaxation experiments with the atmosphere model from European Centre for Medium‐range Weather Forecasts are analyzed to understand influence of lower latitudes (south of about 52 °N) on climate variability and change over the Arctic region. Interannual variability of the Arctic troposphere is impacted strongly by both the tropics and the midlatitudes. In general, the link in winter is stronger than that in summer. Furthermore, the tropics and midlatitudes have different preferred pathways by which they influence the Arctic. Trend analysis suggests that winter surface warming trends over the Arctic are driven strongly by the local sea ice‐atmospheric interaction. Warming at higher altitudes is strongly tied to remote non‐Arctic drivers, with some local amplification. Summer warming trends in northeastern Canada and Greenland are driven strongly by sea surface temperature/sea ice changes and partly by the tropics. The summer warming in northern Europe and western Russia is more strongly driven by the midlatitudes. |
format |
Text |
author |
Ye, Kunhui Jung, Thomas |
spellingShingle |
Ye, Kunhui Jung, Thomas How strong is influence of the tropics and midlatitudes on the Arctic atmospheric circulation and climate change? |
author_facet |
Ye, Kunhui Jung, Thomas |
author_sort |
Ye, Kunhui |
title |
How strong is influence of the tropics and midlatitudes on the Arctic atmospheric circulation and climate change? |
title_short |
How strong is influence of the tropics and midlatitudes on the Arctic atmospheric circulation and climate change? |
title_full |
How strong is influence of the tropics and midlatitudes on the Arctic atmospheric circulation and climate change? |
title_fullStr |
How strong is influence of the tropics and midlatitudes on the Arctic atmospheric circulation and climate change? |
title_full_unstemmed |
How strong is influence of the tropics and midlatitudes on the Arctic atmospheric circulation and climate change? |
title_sort |
how strong is influence of the tropics and midlatitudes on the arctic atmospheric circulation and climate change? |
publisher |
Zenodo |
publishDate |
2019 |
url |
https://dx.doi.org/10.5281/zenodo.3565629 https://zenodo.org/record/3565629 |
geographic |
Arctic Canada Greenland |
geographic_facet |
Arctic Canada Greenland |
genre |
Arctic Climate change Greenland Sea ice |
genre_facet |
Arctic Climate change Greenland Sea ice |
op_relation |
https://zenodo.org/communities/applicate https://dx.doi.org/10.5281/zenodo.3565630 https://zenodo.org/communities/applicate |
op_rights |
Open Access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5281/zenodo.3565629 https://doi.org/10.5281/zenodo.3565630 |
_version_ |
1766307094271623168 |