Climate change hotspots in the CMIP5 global climate model ensemble
We use a statistical metric of multi-dimensional climate change to quantify the emergence of global climate change hotspots in the CMIP5 climate model ensemble. Our hotspot metric extends previous work through the inclusion of extreme seasonal temperature and precipitation, which exert critical infl...
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ftpubmed:oai:pubmedcentral.nih.gov:3765072 2023-05-15T14:59:12+02:00 Climate change hotspots in the CMIP5 global climate model ensemble Diffenbaugh, Noah S. Giorgi, Filippo 2012-08-25 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3765072 http://www.ncbi.nlm.nih.gov/pubmed/24014154 https://doi.org/10.1007/s10584-012-0570-x en eng http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3765072 http://www.ncbi.nlm.nih.gov/pubmed/24014154 http://dx.doi.org/10.1007/s10584-012-0570-x Article Text 2012 ftpubmed https://doi.org/10.1007/s10584-012-0570-x 2013-09-15T00:48:17Z We use a statistical metric of multi-dimensional climate change to quantify the emergence of global climate change hotspots in the CMIP5 climate model ensemble. Our hotspot metric extends previous work through the inclusion of extreme seasonal temperature and precipitation, which exert critical influence on climate change impacts. The results identify areas of the Amazon, the Sahel and tropical West Africa, Indonesia, and the Tibetan Plateau as persistent regional climate change hotspots throughout the 21st century of the RCP8.5 and RCP4.5 forcing pathways. In addition, areas of southern Africa, the Mediterranean, the Arctic, and Central America/western North America also emerge as prominent regional climate change hotspots in response to intermediate and high levels of forcing. Comparisons of different periods of the two forcing pathways suggest that the pattern of aggregate change is fairly robust to the level of global warming below approximately 2°C of global warming (relative to the late-20th-century baseline), but not at the higher levels of global warming that occur in the late-21st-century period of the RCP8.5 pathway, with areas of southern Africa, the Mediterranean, and the Arctic exhibiting particular intensification of relative aggregate climate change in response to high levels of forcing. Although specific impacts will clearly be shaped by the interaction of climate change with human and biological vulnerabilities, our identification of climate change hotspots can help to inform mitigation and adaptation decisions by quantifying the rate, magnitude and causes of the aggregate climate response in different parts of the world. Text Arctic Climate change Global warming PubMed Central (PMC) Arctic Climatic Change 114 3-4 813 822 |
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Article Diffenbaugh, Noah S. Giorgi, Filippo Climate change hotspots in the CMIP5 global climate model ensemble |
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We use a statistical metric of multi-dimensional climate change to quantify the emergence of global climate change hotspots in the CMIP5 climate model ensemble. Our hotspot metric extends previous work through the inclusion of extreme seasonal temperature and precipitation, which exert critical influence on climate change impacts. The results identify areas of the Amazon, the Sahel and tropical West Africa, Indonesia, and the Tibetan Plateau as persistent regional climate change hotspots throughout the 21st century of the RCP8.5 and RCP4.5 forcing pathways. In addition, areas of southern Africa, the Mediterranean, the Arctic, and Central America/western North America also emerge as prominent regional climate change hotspots in response to intermediate and high levels of forcing. Comparisons of different periods of the two forcing pathways suggest that the pattern of aggregate change is fairly robust to the level of global warming below approximately 2°C of global warming (relative to the late-20th-century baseline), but not at the higher levels of global warming that occur in the late-21st-century period of the RCP8.5 pathway, with areas of southern Africa, the Mediterranean, and the Arctic exhibiting particular intensification of relative aggregate climate change in response to high levels of forcing. Although specific impacts will clearly be shaped by the interaction of climate change with human and biological vulnerabilities, our identification of climate change hotspots can help to inform mitigation and adaptation decisions by quantifying the rate, magnitude and causes of the aggregate climate response in different parts of the world. |
format |
Text |
author |
Diffenbaugh, Noah S. Giorgi, Filippo |
author_facet |
Diffenbaugh, Noah S. Giorgi, Filippo |
author_sort |
Diffenbaugh, Noah S. |
title |
Climate change hotspots in the CMIP5 global climate model ensemble |
title_short |
Climate change hotspots in the CMIP5 global climate model ensemble |
title_full |
Climate change hotspots in the CMIP5 global climate model ensemble |
title_fullStr |
Climate change hotspots in the CMIP5 global climate model ensemble |
title_full_unstemmed |
Climate change hotspots in the CMIP5 global climate model ensemble |
title_sort |
climate change hotspots in the cmip5 global climate model ensemble |
publishDate |
2012 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3765072 http://www.ncbi.nlm.nih.gov/pubmed/24014154 https://doi.org/10.1007/s10584-012-0570-x |
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Arctic |
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Arctic Climate change Global warming |
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Arctic Climate change Global warming |
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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3765072 http://www.ncbi.nlm.nih.gov/pubmed/24014154 http://dx.doi.org/10.1007/s10584-012-0570-x |
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https://doi.org/10.1007/s10584-012-0570-x |
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Climatic Change |
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