Exploiting SMILEs and the CMIP5 Archive to Understand Arctic Climate Change Seasonality and Uncertainty

Abstract Arctic Amplification (AA) exhibits a distinct seasonal dependence; it is weakest in boreal summer and strongest in winter. Here, we analyze simulations from single‐model initial‐condition large ensembles and Coupled Model Intercomparison Project Phase 5 to decipher the seasonal evolution of...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: You‐Ting Wu, Yu‐Chiao Liang, Yan‐Ning Kuo, Flavio Lehner, Michael Previdi, Lorenzo M. Polvani, Min‐Hui Lo, Chia‐Wei Lan
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2022GL100745
https://doaj.org/article/5155281f068b4fbc8bbc38924fd46a8e
id ftdoajarticles:oai:doaj.org/article:5155281f068b4fbc8bbc38924fd46a8e
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:5155281f068b4fbc8bbc38924fd46a8e 2024-09-15T18:02:10+00:00 Exploiting SMILEs and the CMIP5 Archive to Understand Arctic Climate Change Seasonality and Uncertainty You‐Ting Wu Yu‐Chiao Liang Yan‐Ning Kuo Flavio Lehner Michael Previdi Lorenzo M. Polvani Min‐Hui Lo Chia‐Wei Lan 2023-01-01T00:00:00Z https://doi.org/10.1029/2022GL100745 https://doaj.org/article/5155281f068b4fbc8bbc38924fd46a8e EN eng Wiley https://doi.org/10.1029/2022GL100745 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2022GL100745 https://doaj.org/article/5155281f068b4fbc8bbc38924fd46a8e Geophysical Research Letters, Vol 50, Iss 2, Pp n/a-n/a (2023) Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2022GL100745 2024-08-05T17:49:23Z Abstract Arctic Amplification (AA) exhibits a distinct seasonal dependence; it is weakest in boreal summer and strongest in winter. Here, we analyze simulations from single‐model initial‐condition large ensembles and Coupled Model Intercomparison Project Phase 5 to decipher the seasonal evolution of Arctic climate change. Models agree that the annual maximum AA shifts from autumn into winter over the 21st century, accompanied by similar shifts in sea‐ice loss and surface turbulent heat fluxes, whereas the maximum precipitation shifts only into late autumn. However, the exact seasonal timing and magnitude of these shifts are highly uncertain. Decomposing the uncertainty into model structural differences, emission scenarios, and internal variability reveals that model differences dominate the total uncertainty, which also undergo autumn‐to‐winter shifts. We also find that the scenario uncertainty is unimportant for projections of AA. These results highlight that understanding model differences is critical to reducing uncertainty in projected Arctic climate change. Article in Journal/Newspaper Climate change Sea ice Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 2
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Geophysics. Cosmic physics
QC801-809
spellingShingle Geophysics. Cosmic physics
QC801-809
You‐Ting Wu
Yu‐Chiao Liang
Yan‐Ning Kuo
Flavio Lehner
Michael Previdi
Lorenzo M. Polvani
Min‐Hui Lo
Chia‐Wei Lan
Exploiting SMILEs and the CMIP5 Archive to Understand Arctic Climate Change Seasonality and Uncertainty
topic_facet Geophysics. Cosmic physics
QC801-809
description Abstract Arctic Amplification (AA) exhibits a distinct seasonal dependence; it is weakest in boreal summer and strongest in winter. Here, we analyze simulations from single‐model initial‐condition large ensembles and Coupled Model Intercomparison Project Phase 5 to decipher the seasonal evolution of Arctic climate change. Models agree that the annual maximum AA shifts from autumn into winter over the 21st century, accompanied by similar shifts in sea‐ice loss and surface turbulent heat fluxes, whereas the maximum precipitation shifts only into late autumn. However, the exact seasonal timing and magnitude of these shifts are highly uncertain. Decomposing the uncertainty into model structural differences, emission scenarios, and internal variability reveals that model differences dominate the total uncertainty, which also undergo autumn‐to‐winter shifts. We also find that the scenario uncertainty is unimportant for projections of AA. These results highlight that understanding model differences is critical to reducing uncertainty in projected Arctic climate change.
format Article in Journal/Newspaper
author You‐Ting Wu
Yu‐Chiao Liang
Yan‐Ning Kuo
Flavio Lehner
Michael Previdi
Lorenzo M. Polvani
Min‐Hui Lo
Chia‐Wei Lan
author_facet You‐Ting Wu
Yu‐Chiao Liang
Yan‐Ning Kuo
Flavio Lehner
Michael Previdi
Lorenzo M. Polvani
Min‐Hui Lo
Chia‐Wei Lan
author_sort You‐Ting Wu
title Exploiting SMILEs and the CMIP5 Archive to Understand Arctic Climate Change Seasonality and Uncertainty
title_short Exploiting SMILEs and the CMIP5 Archive to Understand Arctic Climate Change Seasonality and Uncertainty
title_full Exploiting SMILEs and the CMIP5 Archive to Understand Arctic Climate Change Seasonality and Uncertainty
title_fullStr Exploiting SMILEs and the CMIP5 Archive to Understand Arctic Climate Change Seasonality and Uncertainty
title_full_unstemmed Exploiting SMILEs and the CMIP5 Archive to Understand Arctic Climate Change Seasonality and Uncertainty
title_sort exploiting smiles and the cmip5 archive to understand arctic climate change seasonality and uncertainty
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2022GL100745
https://doaj.org/article/5155281f068b4fbc8bbc38924fd46a8e
genre Climate change
Sea ice
genre_facet Climate change
Sea ice
op_source Geophysical Research Letters, Vol 50, Iss 2, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2022GL100745
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2022GL100745
https://doaj.org/article/5155281f068b4fbc8bbc38924fd46a8e
op_doi https://doi.org/10.1029/2022GL100745
container_title Geophysical Research Letters
container_volume 50
container_issue 2
_version_ 1810439470263042048