Global Hotspots for Future Absolute Temperature Extremes From CMIP6 Models

Abstract Two questions motivated this study: (a) Are global land regions exposed to future changes in absolute temperature extremes? (b) And to which degree? To answer these questions, we projected the trend in four indices, recommended by the Expert Team on Climate Change Detection and Indices (ETC...

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Main Authors: Salah Basem Ajjur, Sami G. Al‐Ghamdi
Format: Article
Language:English
Published: American Geophysical Union (AGU) 2021-09-01
Series:Earth and Space Science
Subjects:
Online Access:https://doi.org/10.1029/2021EA001817
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spelling doaj-6a1bdb5e1dd047c586ccdac5a3c329412021-09-27T21:10:35ZengAmerican Geophysical Union (AGU)Earth and Space Science2333-50842021-09-0189n/an/a10.1029/2021EA001817Global Hotspots for Future Absolute Temperature Extremes From CMIP6 ModelsSalah Basem Ajjur0Sami G. Al‐Ghamdi1Division of Sustainable Development College of Science and Engineering Hamad Bin Khalifa University Qatar Foundation Doha QatarDivision of Sustainable Development College of Science and Engineering Hamad Bin Khalifa University Qatar Foundation Doha QatarAbstract Two questions motivated this study: (a) Are global land regions exposed to future changes in absolute temperature extremes? (b) And to which degree? To answer these questions, we projected the trend in four indices, recommended by the Expert Team on Climate Change Detection and Indices (ETCCDI), through the 21st century. Observational (HadEX3) and reanalyses (ERA5, JRA‐55, NCEP‐R‐1, and NCEP‐R‐2) datasets were used to validate and correct the bias in the Coupled Model Intercomparison Project phase 6 (CMIP6) models. CMIP6 models were then used to evaluate the changes globally and in 44 reference regions under two shared socioeconomic pathways (SSPs): SSP2‐4.5 and SSP5‐8.5. Globally, the analysis showed that, under SSP5‐8.5, TXx and TNx would increase by 0.07°C/year, and TXn (TNn) would increase by 0.09 (0.08)°C/year, during the middle of the 21st century (2021–2050), compared with the reference period (1981–2010). These trends are larger during the end of the 21st century (2071–2100). The analysis also showed that all land reference regions are projected to indices growth up to 3.5°C in TXx; 2.8°C in TNx; 4.5°C in TXn; and 4°C in TNn, during the mid‐21st century under SSP5‐8.5. The latter growth in indices increased by 211% for TXx, 237% for TNx, 242% for TXn, and 300% for TNn during the end‐21st century. The global hotspots affected by absolute temperature extremes are in the Northern Hemisphere, including North America, Iceland, Central Asia, Tibetan Plateau, Russian Arctic, Siberia, Mediterranean, Sahara, and Arabian Peninsula. The study's findings help understand the evolution of climate extremes, which is essential for climate change mitigation and adaptation plans.https://doi.org/10.1029/2021EA001817climate changeabsolute temperature extremesETCCDI indicesCMIP6regional evaluation
collection DOAJ
language English
format Article
sources DOAJ
author Salah Basem Ajjur
Sami G. Al‐Ghamdi
spellingShingle Salah Basem Ajjur
Sami G. Al‐Ghamdi
Global Hotspots for Future Absolute Temperature Extremes From CMIP6 Models
Earth and Space Science
climate change
absolute temperature extremes
ETCCDI indices
CMIP6
regional evaluation
author_facet Salah Basem Ajjur
Sami G. Al‐Ghamdi
author_sort Salah Basem Ajjur
title Global Hotspots for Future Absolute Temperature Extremes From CMIP6 Models
title_short Global Hotspots for Future Absolute Temperature Extremes From CMIP6 Models
title_full Global Hotspots for Future Absolute Temperature Extremes From CMIP6 Models
title_fullStr Global Hotspots for Future Absolute Temperature Extremes From CMIP6 Models
title_full_unstemmed Global Hotspots for Future Absolute Temperature Extremes From CMIP6 Models
title_sort global hotspots for future absolute temperature extremes from cmip6 models
publisher American Geophysical Union (AGU)
series Earth and Space Science
issn 2333-5084
publishDate 2021-09-01
description Abstract Two questions motivated this study: (a) Are global land regions exposed to future changes in absolute temperature extremes? (b) And to which degree? To answer these questions, we projected the trend in four indices, recommended by the Expert Team on Climate Change Detection and Indices (ETCCDI), through the 21st century. Observational (HadEX3) and reanalyses (ERA5, JRA‐55, NCEP‐R‐1, and NCEP‐R‐2) datasets were used to validate and correct the bias in the Coupled Model Intercomparison Project phase 6 (CMIP6) models. CMIP6 models were then used to evaluate the changes globally and in 44 reference regions under two shared socioeconomic pathways (SSPs): SSP2‐4.5 and SSP5‐8.5. Globally, the analysis showed that, under SSP5‐8.5, TXx and TNx would increase by 0.07°C/year, and TXn (TNn) would increase by 0.09 (0.08)°C/year, during the middle of the 21st century (2021–2050), compared with the reference period (1981–2010). These trends are larger during the end of the 21st century (2071–2100). The analysis also showed that all land reference regions are projected to indices growth up to 3.5°C in TXx; 2.8°C in TNx; 4.5°C in TXn; and 4°C in TNn, during the mid‐21st century under SSP5‐8.5. The latter growth in indices increased by 211% for TXx, 237% for TNx, 242% for TXn, and 300% for TNn during the end‐21st century. The global hotspots affected by absolute temperature extremes are in the Northern Hemisphere, including North America, Iceland, Central Asia, Tibetan Plateau, Russian Arctic, Siberia, Mediterranean, Sahara, and Arabian Peninsula. The study's findings help understand the evolution of climate extremes, which is essential for climate change mitigation and adaptation plans.
topic climate change
absolute temperature extremes
ETCCDI indices
CMIP6
regional evaluation
url https://doi.org/10.1029/2021EA001817
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