Seasonal Changes in Poleward Atmospheric Heat Transport Under Increased CO2

Arctic warming under increased CO2 peaks in winter, but is influenced by summer forcing via seasonal ocean heat storage. Yet changes in atmospheric heat transport into the Arctic have mainly been investigated in the annual mean or winter, with limited focus on other seasons. We investigate the full...

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Main Authors: Hahn, Lily Caroline, Armour, Kyle, Battisti, David S., Donohoe, Aaron, Fajber, Robert
Format: Other/Unknown Material
Language:unknown
Published: Authorea, Inc. 2023
Subjects:
Online Access:http://dx.doi.org/10.22541/essoar.168881933.38512692/v1
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spelling crwinnower:10.22541/essoar.168881933.38512692/v1 2024-06-02T08:00:18+00:00 Seasonal Changes in Poleward Atmospheric Heat Transport Under Increased CO2 Hahn, Lily Caroline Armour, Kyle Battisti, David S. Donohoe, Aaron Fajber, Robert 2023 http://dx.doi.org/10.22541/essoar.168881933.38512692/v1 unknown Authorea, Inc. https://creativecommons.org/licenses/by/4.0/ posted-content 2023 crwinnower https://doi.org/10.22541/essoar.168881933.38512692/v1 2024-05-07T14:19:26Z Arctic warming under increased CO2 peaks in winter, but is influenced by summer forcing via seasonal ocean heat storage. Yet changes in atmospheric heat transport into the Arctic have mainly been investigated in the annual mean or winter, with limited focus on other seasons. We investigate the full seasonal cycle of poleward heat transport modelled with increased CO2 or with individually applied Arctic sea-ice loss and global sea-surface warming. We find that a winter reduction in dry heat transport is driven by Arctic sea-ice loss and warming, while a summer increase in moist heat transport is driven by sub-Arctic warming and moistening. Intermodel spread in Arctic warming controls spread in seasonal poleward heat transport. These seasonal changes and their intermodel spread are well-captured by down-gradient diffusive heat transport. While changes in moist and dry heat transport compensate in the annual-mean, their opposite seasonality may support non-compensating effects on Arctic warming. Other/Unknown Material Arctic Sea ice The Winnower Arctic
institution Open Polar
collection The Winnower
op_collection_id crwinnower
language unknown
description Arctic warming under increased CO2 peaks in winter, but is influenced by summer forcing via seasonal ocean heat storage. Yet changes in atmospheric heat transport into the Arctic have mainly been investigated in the annual mean or winter, with limited focus on other seasons. We investigate the full seasonal cycle of poleward heat transport modelled with increased CO2 or with individually applied Arctic sea-ice loss and global sea-surface warming. We find that a winter reduction in dry heat transport is driven by Arctic sea-ice loss and warming, while a summer increase in moist heat transport is driven by sub-Arctic warming and moistening. Intermodel spread in Arctic warming controls spread in seasonal poleward heat transport. These seasonal changes and their intermodel spread are well-captured by down-gradient diffusive heat transport. While changes in moist and dry heat transport compensate in the annual-mean, their opposite seasonality may support non-compensating effects on Arctic warming.
format Other/Unknown Material
author Hahn, Lily Caroline
Armour, Kyle
Battisti, David S.
Donohoe, Aaron
Fajber, Robert
spellingShingle Hahn, Lily Caroline
Armour, Kyle
Battisti, David S.
Donohoe, Aaron
Fajber, Robert
Seasonal Changes in Poleward Atmospheric Heat Transport Under Increased CO2
author_facet Hahn, Lily Caroline
Armour, Kyle
Battisti, David S.
Donohoe, Aaron
Fajber, Robert
author_sort Hahn, Lily Caroline
title Seasonal Changes in Poleward Atmospheric Heat Transport Under Increased CO2
title_short Seasonal Changes in Poleward Atmospheric Heat Transport Under Increased CO2
title_full Seasonal Changes in Poleward Atmospheric Heat Transport Under Increased CO2
title_fullStr Seasonal Changes in Poleward Atmospheric Heat Transport Under Increased CO2
title_full_unstemmed Seasonal Changes in Poleward Atmospheric Heat Transport Under Increased CO2
title_sort seasonal changes in poleward atmospheric heat transport under increased co2
publisher Authorea, Inc.
publishDate 2023
url http://dx.doi.org/10.22541/essoar.168881933.38512692/v1
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.22541/essoar.168881933.38512692/v1
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