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...

Full description

Bibliographic Details
Main Author: Ruggieri, Paolo
Format: Conference Object
Language:unknown
Published: Zenodo 2019
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.3060542
https://zenodo.org/record/3060542
id ftdatacite:10.5281/zenodo.3060542
record_format openpolar
spelling ftdatacite:10.5281/zenodo.3060542 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.3060542 https://zenodo.org/record/3060542 unknown Zenodo https://dx.doi.org/10.5281/zenodo.3060541 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.3060542 https://doi.org/10.5281/zenodo.3060541 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
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
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.3060542
https://zenodo.org/record/3060542
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.3060541
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.3060542
https://doi.org/10.5281/zenodo.3060541
_version_ 1766343943323123712