Response of Northern Hemisphere Weather and Climate to Arctic Sea Ice Decline: Resolution Independence in Polar Amplification Model Intercomparison Project (PAMIP) Simulations

The impact of Arctic sea ice decline on the weather and climate in midlatitudes is still much debated, with observations suggesting a strong link and models a much weaker link. In this study, we use the atmospheric model OpenIFS in a set of model experiments following the protocol outlined in the Po...

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Published in:Journal of Climate
Main Authors: Streffing, Jan, Semmler, T., Zampieri, Lorenzo, Jung, Thomas
Format: Article in Journal/Newspaper
Language:unknown
Published: AMER METEOROLOGICAL SOC 2021
Subjects:
Online Access:https://epic.awi.de/id/eprint/56473/
https://epic.awi.de/id/eprint/56473/1/Streffing_2021_JCLI.pdf
https://journals.ametsoc.org/view/journals/clim/34/20/JCLI-D-19-1005.1.xml
https://hdl.handle.net/10013/epic.1a77f3ca-e147-4870-8a34-48425c02cb0e
id ftawi:oai:epic.awi.de:56473
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spelling ftawi:oai:epic.awi.de:56473 2024-09-15T17:51:42+00:00 Response of Northern Hemisphere Weather and Climate to Arctic Sea Ice Decline: Resolution Independence in Polar Amplification Model Intercomparison Project (PAMIP) Simulations Streffing, Jan Semmler, T. Zampieri, Lorenzo Jung, Thomas 2021-10-01 application/pdf https://epic.awi.de/id/eprint/56473/ https://epic.awi.de/id/eprint/56473/1/Streffing_2021_JCLI.pdf https://journals.ametsoc.org/view/journals/clim/34/20/JCLI-D-19-1005.1.xml https://hdl.handle.net/10013/epic.1a77f3ca-e147-4870-8a34-48425c02cb0e unknown AMER METEOROLOGICAL SOC https://epic.awi.de/id/eprint/56473/1/Streffing_2021_JCLI.pdf Streffing, J. orcid:0000-0001-9515-3322 , Semmler, T. orcid:0000-0002-2254-4901 , Zampieri, L. orcid:0000-0003-1703-4162 and Jung, T. orcid:0000-0002-2651-1293 (2021) Response of Northern Hemisphere Weather and Climate to Arctic Sea Ice Decline: Resolution Independence in Polar Amplification Model Intercomparison Project (PAMIP) Simulations , Journal of Climate, 34 (20), pp. 8445-8457 . doi:10.1175/JCLI-D-19-1005.1 <https://doi.org/10.1175/JCLI-D-19-1005.1> , hdl:10013/epic.1a77f3ca-e147-4870-8a34-48425c02cb0e info:eu-repo/semantics/openAccess EPIC3Journal of Climate, AMER METEOROLOGICAL SOC, 34(20), pp. 8445-8457, ISSN: 0894-8755 Article NonPeerReviewed info:eu-repo/semantics/article 2021 ftawi https://doi.org/10.1175/JCLI-D-19-1005.1 2024-06-24T04:28:46Z The impact of Arctic sea ice decline on the weather and climate in midlatitudes is still much debated, with observations suggesting a strong link and models a much weaker link. In this study, we use the atmospheric model OpenIFS in a set of model experiments following the protocol outlined in the Polar Amplification Model Intercomparison Project (PAMIP) to investigate whether the simulated atmospheric response to future changes in Arctic sea ice fundamentally depends on model resolution. More specifically, we increase the horizontal resolution of the model from 125 to 39 km with 91 vertical levels; in a second step, resolution is further increased to 16 km with 137 levels in the vertical. The model does produce a response to sea ice decline with a weaker midlatitude Atlantic jet and increased blocking in the high-latitude Atlantic, but no sensitivity to resolution can be detected with 100 members. Furthermore, we find that the ensemble convergence toward the mean is not impacted by the model resolutions considered here. Article in Journal/Newspaper Arctic Sea ice Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Journal of Climate 1 39
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description The impact of Arctic sea ice decline on the weather and climate in midlatitudes is still much debated, with observations suggesting a strong link and models a much weaker link. In this study, we use the atmospheric model OpenIFS in a set of model experiments following the protocol outlined in the Polar Amplification Model Intercomparison Project (PAMIP) to investigate whether the simulated atmospheric response to future changes in Arctic sea ice fundamentally depends on model resolution. More specifically, we increase the horizontal resolution of the model from 125 to 39 km with 91 vertical levels; in a second step, resolution is further increased to 16 km with 137 levels in the vertical. The model does produce a response to sea ice decline with a weaker midlatitude Atlantic jet and increased blocking in the high-latitude Atlantic, but no sensitivity to resolution can be detected with 100 members. Furthermore, we find that the ensemble convergence toward the mean is not impacted by the model resolutions considered here.
format Article in Journal/Newspaper
author Streffing, Jan
Semmler, T.
Zampieri, Lorenzo
Jung, Thomas
spellingShingle Streffing, Jan
Semmler, T.
Zampieri, Lorenzo
Jung, Thomas
Response of Northern Hemisphere Weather and Climate to Arctic Sea Ice Decline: Resolution Independence in Polar Amplification Model Intercomparison Project (PAMIP) Simulations
author_facet Streffing, Jan
Semmler, T.
Zampieri, Lorenzo
Jung, Thomas
author_sort Streffing, Jan
title Response of Northern Hemisphere Weather and Climate to Arctic Sea Ice Decline: Resolution Independence in Polar Amplification Model Intercomparison Project (PAMIP) Simulations
title_short Response of Northern Hemisphere Weather and Climate to Arctic Sea Ice Decline: Resolution Independence in Polar Amplification Model Intercomparison Project (PAMIP) Simulations
title_full Response of Northern Hemisphere Weather and Climate to Arctic Sea Ice Decline: Resolution Independence in Polar Amplification Model Intercomparison Project (PAMIP) Simulations
title_fullStr Response of Northern Hemisphere Weather and Climate to Arctic Sea Ice Decline: Resolution Independence in Polar Amplification Model Intercomparison Project (PAMIP) Simulations
title_full_unstemmed Response of Northern Hemisphere Weather and Climate to Arctic Sea Ice Decline: Resolution Independence in Polar Amplification Model Intercomparison Project (PAMIP) Simulations
title_sort response of northern hemisphere weather and climate to arctic sea ice decline: resolution independence in polar amplification model intercomparison project (pamip) simulations
publisher AMER METEOROLOGICAL SOC
publishDate 2021
url https://epic.awi.de/id/eprint/56473/
https://epic.awi.de/id/eprint/56473/1/Streffing_2021_JCLI.pdf
https://journals.ametsoc.org/view/journals/clim/34/20/JCLI-D-19-1005.1.xml
https://hdl.handle.net/10013/epic.1a77f3ca-e147-4870-8a34-48425c02cb0e
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_source EPIC3Journal of Climate, AMER METEOROLOGICAL SOC, 34(20), pp. 8445-8457, ISSN: 0894-8755
op_relation https://epic.awi.de/id/eprint/56473/1/Streffing_2021_JCLI.pdf
Streffing, J. orcid:0000-0001-9515-3322 , Semmler, T. orcid:0000-0002-2254-4901 , Zampieri, L. orcid:0000-0003-1703-4162 and Jung, T. orcid:0000-0002-2651-1293 (2021) Response of Northern Hemisphere Weather and Climate to Arctic Sea Ice Decline: Resolution Independence in Polar Amplification Model Intercomparison Project (PAMIP) Simulations , Journal of Climate, 34 (20), pp. 8445-8457 . doi:10.1175/JCLI-D-19-1005.1 <https://doi.org/10.1175/JCLI-D-19-1005.1> , hdl:10013/epic.1a77f3ca-e147-4870-8a34-48425c02cb0e
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1175/JCLI-D-19-1005.1
container_title Journal of Climate
container_start_page 1
op_container_end_page 39
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