Quantifying the irreducible uncertainty in near-term climate projections

If the Paris agreement at the Conference of Parties 21 is implemented very effectively, greenhouse-gas emissions might decrease after year 2020. Whether this would lead to identifiable near-term responses in “iconic” climate quantities of wide scientific and public interest is unclear, because the c...

Full description

Bibliographic Details
Published in:Wiley Interdisciplinary Reviews: Climate Change
Main Author: Marotzke, J.
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:http://hdl.handle.net/21.11116/0000-0002-5A51-E
http://hdl.handle.net/21.11116/0000-0002-708D-1
http://hdl.handle.net/21.11116/0000-0002-B6CF-8
id ftpubman:oai:pure.mpg.de:item_3003838
record_format openpolar
spelling ftpubman:oai:pure.mpg.de:item_3003838 2023-08-27T04:08:08+02:00 Quantifying the irreducible uncertainty in near-term climate projections Marotzke, J. 2019-01-24 application/zip application/pdf http://hdl.handle.net/21.11116/0000-0002-5A51-E http://hdl.handle.net/21.11116/0000-0002-708D-1 http://hdl.handle.net/21.11116/0000-0002-B6CF-8 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1002/wcc.563 http://hdl.handle.net/21.11116/0000-0002-5A51-E http://hdl.handle.net/21.11116/0000-0002-708D-1 http://hdl.handle.net/21.11116/0000-0002-B6CF-8 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Wiley Interdisciplinary Reviews - Climate Change info:eu-repo/semantics/article 2019 ftpubman https://doi.org/10.1002/wcc.563 2023-08-02T01:15:04Z If the Paris agreement at the Conference of Parties 21 is implemented very effectively, greenhouse-gas emissions might decrease after year 2020. Whether this would lead to identifiable near-term responses in “iconic” climate quantities of wide scientific and public interest is unclear, because the climate response would be obscured by quasi-random internal variability. I define the climate response as an increase or decrease in a linear climate trend over the period 2021–2035, compared to 2006–2020, and establish the probability of such a trend change being caused by an assumed policy shift toward emissions reductions after 2020. I quantify the irreducible uncertainty in projecting such a trend change through very large (100-member) ensembles of the state-of-the-art climate model MPI-ESM-LR. Trends in global-mean surface temperature (GMST) are higher over the period 2021–2035 than over 2006–2020 in one-third of all realizations in the mitigation scenario RCP2.6, interpreted as implementing the Paris agreement, compared to around one-half in the no-mitigation scenario RCP4.5. Mitigation is sufficient to cause a GMST trend reduction with a probability of 0.40 and necessary with a probability of 0.33. Trend increases in Arctic September sea-ice area and the Atlantic meridional overturning circulation are caused by the emissions reductions with a probability of only around 0.1. By contrast, emissions reductions are necessary for a trend decrease in upper-ocean heat content with a probability of over one-half. Some iconic climate quantities might thus by year 2035 exhibit an identifiable response to a successful Paris agreement but sometimes with low probability, creating a substantial communication challenge. This article is categorized under: Climate Models and Modeling > Knowledge Generation with Models. © 2018 The Authors. WIREs Climate Change published by Wiley Periodicals, Inc. Article in Journal/Newspaper Arctic Climate change Sea ice Max Planck Society: MPG.PuRe Arctic Wiley Interdisciplinary Reviews: Climate Change 10 1 e563
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
description If the Paris agreement at the Conference of Parties 21 is implemented very effectively, greenhouse-gas emissions might decrease after year 2020. Whether this would lead to identifiable near-term responses in “iconic” climate quantities of wide scientific and public interest is unclear, because the climate response would be obscured by quasi-random internal variability. I define the climate response as an increase or decrease in a linear climate trend over the period 2021–2035, compared to 2006–2020, and establish the probability of such a trend change being caused by an assumed policy shift toward emissions reductions after 2020. I quantify the irreducible uncertainty in projecting such a trend change through very large (100-member) ensembles of the state-of-the-art climate model MPI-ESM-LR. Trends in global-mean surface temperature (GMST) are higher over the period 2021–2035 than over 2006–2020 in one-third of all realizations in the mitigation scenario RCP2.6, interpreted as implementing the Paris agreement, compared to around one-half in the no-mitigation scenario RCP4.5. Mitigation is sufficient to cause a GMST trend reduction with a probability of 0.40 and necessary with a probability of 0.33. Trend increases in Arctic September sea-ice area and the Atlantic meridional overturning circulation are caused by the emissions reductions with a probability of only around 0.1. By contrast, emissions reductions are necessary for a trend decrease in upper-ocean heat content with a probability of over one-half. Some iconic climate quantities might thus by year 2035 exhibit an identifiable response to a successful Paris agreement but sometimes with low probability, creating a substantial communication challenge. This article is categorized under: Climate Models and Modeling > Knowledge Generation with Models. © 2018 The Authors. WIREs Climate Change published by Wiley Periodicals, Inc.
format Article in Journal/Newspaper
author Marotzke, J.
spellingShingle Marotzke, J.
Quantifying the irreducible uncertainty in near-term climate projections
author_facet Marotzke, J.
author_sort Marotzke, J.
title Quantifying the irreducible uncertainty in near-term climate projections
title_short Quantifying the irreducible uncertainty in near-term climate projections
title_full Quantifying the irreducible uncertainty in near-term climate projections
title_fullStr Quantifying the irreducible uncertainty in near-term climate projections
title_full_unstemmed Quantifying the irreducible uncertainty in near-term climate projections
title_sort quantifying the irreducible uncertainty in near-term climate projections
publishDate 2019
url http://hdl.handle.net/21.11116/0000-0002-5A51-E
http://hdl.handle.net/21.11116/0000-0002-708D-1
http://hdl.handle.net/21.11116/0000-0002-B6CF-8
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Sea ice
genre_facet Arctic
Climate change
Sea ice
op_source Wiley Interdisciplinary Reviews - Climate Change
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1002/wcc.563
http://hdl.handle.net/21.11116/0000-0002-5A51-E
http://hdl.handle.net/21.11116/0000-0002-708D-1
http://hdl.handle.net/21.11116/0000-0002-B6CF-8
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1002/wcc.563
container_title Wiley Interdisciplinary Reviews: Climate Change
container_volume 10
container_issue 1
container_start_page e563
_version_ 1775348847917137920