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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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 |
work_keys_str_mv |
AT salahbasemajjur globalhotspotsforfutureabsolutetemperatureextremesfromcmip6models AT samigalghamdi globalhotspotsforfutureabsolutetemperatureextremesfromcmip6models |
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