Changes to population-based emergence of climate change from CMIP5 to CMIP6

The Coupled Model Intercomparison Project Phase 6 (CMIP6) model ensemble projects climate change emerging soonest and most strongly at low latitudes, regardless of the emissions pathway taken. In terms of signal-to-noise (S/N) ratios of average annual temperatures, these models project earlier and s...

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Main Authors: Hunter C Douglas, Luke J Harrington, Manoj Joshi, Ed Hawkins, Laura E Revell, David J Frame
Format: Article
Language:English
Published: IOP Publishing 2022-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/aca91e
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author Hunter C Douglas
Luke J Harrington
Manoj Joshi
Ed Hawkins
Laura E Revell
David J Frame
author_facet Hunter C Douglas
Luke J Harrington
Manoj Joshi
Ed Hawkins
Laura E Revell
David J Frame
author_sort Hunter C Douglas
collection DOAJ
description The Coupled Model Intercomparison Project Phase 6 (CMIP6) model ensemble projects climate change emerging soonest and most strongly at low latitudes, regardless of the emissions pathway taken. In terms of signal-to-noise (S/N) ratios of average annual temperatures, these models project earlier and stronger emergence under the Shared Socio-economic Pathways than the previous generation did under corresponding Representative Concentration Pathways. Spatial patterns of emergence also change between generations of models; under a high emissions scenario, mid-century S/N is lower than previous studies indicated in Central Africa, South Asia, and parts of South America, West Africa, East Asia, and Western Europe, but higher in most other populated areas. We show that these global and regional changes are caused by a combination of higher effective climate sensitivity in the CMIP6 ensemble, as well as changes to emissions pathways, component-wise effective radiative forcing, and region-scale climate responses between model generations. We also present the first population-weighted calculation of climate change emergence for the CMIP6 ensemble, quantifying the number of people exposed to increasing degrees of abnormal temperatures now and into the future. Our results confirm the expected inequity of climate change-related impacts in the decades between now and the 2050 target for net-zero emissions held by many countries. These findings underscore the importance of concurrent investments in both mitigation and adaptation.
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spelling doaj.art-5b6ce241c9024e8e833324a0dbaac8872023-08-09T15:20:02ZengIOP PublishingEnvironmental Research Letters1748-93262022-01-0118101401310.1088/1748-9326/aca91eChanges to population-based emergence of climate change from CMIP5 to CMIP6Hunter C Douglas0https://orcid.org/0000-0002-5411-7656Luke J Harrington1https://orcid.org/0000-0002-1699-6119Manoj Joshi2https://orcid.org/0000-0002-2948-2811Ed Hawkins3https://orcid.org/0000-0001-9477-3677Laura E Revell4https://orcid.org/0000-0002-8974-7703David J Frame5https://orcid.org/0000-0002-0949-3994New Zealand Climate Change Research Institute, Victoria University of Wellington Te Herenga Waka , Wellington, New ZealandTe Aka Mātuatua School of Science, University of Waikato , Hamilton, New ZealandClimatic Research Unit, University of East Anglia , Norwich, United Kingdom; School of Environmental Sciences, University of East Anglia , Norwich, United KingdomDepartment of Meteorology, University of Reading , Reading, United KingdomSchool of Physical and Chemical Sciences, University of Canterbury , Christchurch, New ZealandSchool of Physical and Chemical Sciences, University of Canterbury , Christchurch, New Zealand; School of Earth and Environment, University of Canterbury , Christchurch, New ZealandThe Coupled Model Intercomparison Project Phase 6 (CMIP6) model ensemble projects climate change emerging soonest and most strongly at low latitudes, regardless of the emissions pathway taken. In terms of signal-to-noise (S/N) ratios of average annual temperatures, these models project earlier and stronger emergence under the Shared Socio-economic Pathways than the previous generation did under corresponding Representative Concentration Pathways. Spatial patterns of emergence also change between generations of models; under a high emissions scenario, mid-century S/N is lower than previous studies indicated in Central Africa, South Asia, and parts of South America, West Africa, East Asia, and Western Europe, but higher in most other populated areas. We show that these global and regional changes are caused by a combination of higher effective climate sensitivity in the CMIP6 ensemble, as well as changes to emissions pathways, component-wise effective radiative forcing, and region-scale climate responses between model generations. We also present the first population-weighted calculation of climate change emergence for the CMIP6 ensemble, quantifying the number of people exposed to increasing degrees of abnormal temperatures now and into the future. Our results confirm the expected inequity of climate change-related impacts in the decades between now and the 2050 target for net-zero emissions held by many countries. These findings underscore the importance of concurrent investments in both mitigation and adaptation.https://doi.org/10.1088/1748-9326/aca91eclimate change emergenceCMIP6SSPsRCPsinequalityCMIP5
spellingShingle Hunter C Douglas
Luke J Harrington
Manoj Joshi
Ed Hawkins
Laura E Revell
David J Frame
Changes to population-based emergence of climate change from CMIP5 to CMIP6
Environmental Research Letters
climate change emergence
CMIP6
SSPs
RCPs
inequality
CMIP5
title Changes to population-based emergence of climate change from CMIP5 to CMIP6
title_full Changes to population-based emergence of climate change from CMIP5 to CMIP6
title_fullStr Changes to population-based emergence of climate change from CMIP5 to CMIP6
title_full_unstemmed Changes to population-based emergence of climate change from CMIP5 to CMIP6
title_short Changes to population-based emergence of climate change from CMIP5 to CMIP6
title_sort changes to population based emergence of climate change from cmip5 to cmip6
topic climate change emergence
CMIP6
SSPs
RCPs
inequality
CMIP5
url https://doi.org/10.1088/1748-9326/aca91e
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