Atlantic weather regimes and poleward heat transport by transient eddies
Transport of heat by transient atmospheric eddies is a key component of the heat budget of the Arctic and high latitude regions. While transport in the midlatitudes is known to be modulated by large scale low frequency flow regimes, little is known about the link between heat flux in the polar cap a...
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ftdatacite:10.5281/zenodo.3060541 2023-05-15T15:13:23+02:00 Atlantic weather regimes and poleward heat transport by transient eddies Ruggieri, Paolo 2019 https://dx.doi.org/10.5281/zenodo.3060541 https://zenodo.org/record/3060541 unknown Zenodo https://dx.doi.org/10.5281/zenodo.3060542 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 Presentation article-journal ScholarlyArticle 2019 ftdatacite https://doi.org/10.5281/zenodo.3060541 https://doi.org/10.5281/zenodo.3060542 2021-11-05T12:55:41Z Transport of heat by transient atmospheric eddies is a key component of the heat budget of the Arctic and high latitude regions. While transport in the midlatitudes is known to be modulated by large scale low frequency flow regimes, little is known about the link between heat flux in the polar cap and midlatitude circulation regimes. Recent studies suggest that heat and moisture transport into the pole happens in “bursts” that are associated with atmospheric blocking. While the picture is evolving, a systematic assessment is still lacking. In this study we investigate the relationship between the poleward heat transport by atmospheric transient eddies and North Atlantic weather regimes in reanalysis data. Weather regimes are estimated via clustering methods, a jet latitude index and a blocking index. Heat transport is defined as advection of moist static energy and the transient component has been computed for selected frequency bands between the midlatitude baroclinic life cycle and the seasonal range. Results show that transient eddy heat flux is substantially modulated by midlatitude weather regimes on a regional scale also in polar regions. On a zonal mean sense, the phases of the North Atlantic Oscillation do not change significantly the synoptic heat flux, whereas Scandinavian blocking and Atlantic Ridge are associated with an intensification. The relationship between extreme events of strong heat flux and circulation regimes is also assessed and the analysis indicates a fundamental role of blocking in the North Atlantic sector. The implications of our findings for sub-seasonal predictability and systematic errors in coupled models are discussed. Applications of the proposed approach to seasonal forecast systems and multi-model frameworks are suggested. Conference Object Arctic North Atlantic North Atlantic oscillation DataCite Metadata Store (German National Library of Science and Technology) Arctic |
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description |
Transport of heat by transient atmospheric eddies is a key component of the heat budget of the Arctic and high latitude regions. While transport in the midlatitudes is known to be modulated by large scale low frequency flow regimes, little is known about the link between heat flux in the polar cap and midlatitude circulation regimes. Recent studies suggest that heat and moisture transport into the pole happens in “bursts” that are associated with atmospheric blocking. While the picture is evolving, a systematic assessment is still lacking. In this study we investigate the relationship between the poleward heat transport by atmospheric transient eddies and North Atlantic weather regimes in reanalysis data. Weather regimes are estimated via clustering methods, a jet latitude index and a blocking index. Heat transport is defined as advection of moist static energy and the transient component has been computed for selected frequency bands between the midlatitude baroclinic life cycle and the seasonal range. Results show that transient eddy heat flux is substantially modulated by midlatitude weather regimes on a regional scale also in polar regions. On a zonal mean sense, the phases of the North Atlantic Oscillation do not change significantly the synoptic heat flux, whereas Scandinavian blocking and Atlantic Ridge are associated with an intensification. The relationship between extreme events of strong heat flux and circulation regimes is also assessed and the analysis indicates a fundamental role of blocking in the North Atlantic sector. The implications of our findings for sub-seasonal predictability and systematic errors in coupled models are discussed. Applications of the proposed approach to seasonal forecast systems and multi-model frameworks are suggested. |
format |
Conference Object |
author |
Ruggieri, Paolo |
spellingShingle |
Ruggieri, Paolo Atlantic weather regimes and poleward heat transport by transient eddies |
author_facet |
Ruggieri, Paolo |
author_sort |
Ruggieri, Paolo |
title |
Atlantic weather regimes and poleward heat transport by transient eddies |
title_short |
Atlantic weather regimes and poleward heat transport by transient eddies |
title_full |
Atlantic weather regimes and poleward heat transport by transient eddies |
title_fullStr |
Atlantic weather regimes and poleward heat transport by transient eddies |
title_full_unstemmed |
Atlantic weather regimes and poleward heat transport by transient eddies |
title_sort |
atlantic weather regimes and poleward heat transport by transient eddies |
publisher |
Zenodo |
publishDate |
2019 |
url |
https://dx.doi.org/10.5281/zenodo.3060541 https://zenodo.org/record/3060541 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic North Atlantic North Atlantic oscillation |
genre_facet |
Arctic North Atlantic North Atlantic oscillation |
op_relation |
https://dx.doi.org/10.5281/zenodo.3060542 |
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.3060541 https://doi.org/10.5281/zenodo.3060542 |
_version_ |
1766343943158497280 |