Back to Search Start Over

The Physical Climate at Global Warming Thresholds as Seen in the U.K. Earth System Model.

Authors :
Swaminathan, Ranjini
Parker, Robert J.
Jones, Colin G.
Allan, Richard P.
Quaife, Tristan
Kelley, Douglas I.
de Mora, Lee
Walton, Jeremy
Source :
Journal of Climate; Jan2022, Vol. 35 Issue 1, p29-48, 20p, 1 Chart, 15 Graphs
Publication Year :
2022

Abstract

A key goal of the 2015 Paris Climate Agreement is to keep global mean temperature change at 2°C and if possible under 1.5°C by the end of the century. To investigate the likelihood of achieving this target, we calculate the year of exceedance of a given global warming threshold (GWT) temperature across 32 CMIP6 models for Shared Socioeconomic Pathway (SSP) and radiative forcing combinations included in the Tier 1 ScenarioMIP simulations. Threshold exceedance year calculations reveal that a majority of CMIP6 models project warming beyond 2°C by the end of the century under every scenario or pathway apart from the lowest emission scenarios considered, SSP1–1.9 and SSP1–2.6, which is largely a function of the ScenarioMIP experiment design. The U.K. Earth System Model (UKESM1) ScenarioMIP projections are analyzed in detail to assess the regional and seasonal variations in climate at different warming levels. The warming signal emerging by midcentury is identified as significant and distinct from internal climate variability in all scenarios considered and includes warming summers in the Mediterranean, drying in the Amazon, and heavier Indian monsoons. Arctic sea ice depletion results in prominent amplification of warming and tropical warming patterns emerge that are distinct from interannual variability. Climate changes projected for a 2°C warmer world are in almost all cases exacerbated with further global warming (e.g., to a 4°C warmer world). Significance Statement: In this study, we look into changes occurring in climate due to global warming by analyzing data from the latest global climate models to see when the Earth will warm by 2° or 4°C, compared to preindustrial temperatures. We then use the UKESM1 climate model to identify regions on Earth where significant climate change is simulated in the future and discuss possible reasons for these changes. Simulations from this model also show that regions such as the Mediterranean, Amazon forests, and tropical countries are likely to see significant changes in climate impacting human lives. Future work to study the regional changes in greater detail will help us improve climate policies to protect society. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
08948755
Volume :
35
Issue :
1
Database :
Complementary Index
Journal :
Journal of Climate
Publication Type :
Academic Journal
Accession number :
154176429
Full Text :
https://doi.org/10.1175/JCLI-D-21-0234.1