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Observations and Projections of Heat Waves in South America
Although Heat Waves (HWs) are expected to increase due to global warming, they are a regional phenomenon that demands for local analyses. In this paper, we assess four HW metrics (HW duration, HW frequency, HW amplitude, and number of HWs per season) as well as the share of extremely warm days (TX95...
Autores principales: | , , , , , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Nature Publishing Group UK
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6547650/ https://www.ncbi.nlm.nih.gov/pubmed/31160642 http://dx.doi.org/10.1038/s41598-019-44614-4 |
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author | Feron, S. Cordero, R. R. Damiani, A. Llanillo, P. J. Jorquera, J. Sepulveda, E. Asencio, V. Laroze, D. Labbe, F. Carrasco, J. Torres, G. |
author_facet | Feron, S. Cordero, R. R. Damiani, A. Llanillo, P. J. Jorquera, J. Sepulveda, E. Asencio, V. Laroze, D. Labbe, F. Carrasco, J. Torres, G. |
author_sort | Feron, S. |
collection | PubMed |
description | Although Heat Waves (HWs) are expected to increase due to global warming, they are a regional phenomenon that demands for local analyses. In this paper, we assess four HW metrics (HW duration, HW frequency, HW amplitude, and number of HWs per season) as well as the share of extremely warm days (TX95, according to the 95th percentile) in South America (SA). Our analysis included observations as well as simulations from global and regional models. In particular, Regional Climate Models (RCMs) from the Coordinated Regional Climate Downscaling Experiment (CORDEX), and Global Climate Models (GCMs) from the Coupled Model Intercomparison Project Phase 5 (CMIP5) were used to project both TX95 estimates and HW metrics according to two representative concentration pathways (RCP4.5 and RCP8.5). We found that in recent decades the share of extremely warm days has at least doubled over the period December–January–February (DJF) in northern SA; less significant increases have been observed in southern SA. We also found that by midcentury, under the RCP4.5 scenario, extremely warm DJF days (as well as the number of HWs per season) are expected to increase by 5–10 times at locations close to the Equator and in the Atacama Desert. Increases are expected to be less pronounced in southern SA. Projections under the RCP8.5 scenario are more striking, particularly in tropical areas where half or more of the days could be extremely warm by midcentury. |
format | Online Article Text |
id | pubmed-6547650 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2019 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-65476502019-06-10 Observations and Projections of Heat Waves in South America Feron, S. Cordero, R. R. Damiani, A. Llanillo, P. J. Jorquera, J. Sepulveda, E. Asencio, V. Laroze, D. Labbe, F. Carrasco, J. Torres, G. Sci Rep Article Although Heat Waves (HWs) are expected to increase due to global warming, they are a regional phenomenon that demands for local analyses. In this paper, we assess four HW metrics (HW duration, HW frequency, HW amplitude, and number of HWs per season) as well as the share of extremely warm days (TX95, according to the 95th percentile) in South America (SA). Our analysis included observations as well as simulations from global and regional models. In particular, Regional Climate Models (RCMs) from the Coordinated Regional Climate Downscaling Experiment (CORDEX), and Global Climate Models (GCMs) from the Coupled Model Intercomparison Project Phase 5 (CMIP5) were used to project both TX95 estimates and HW metrics according to two representative concentration pathways (RCP4.5 and RCP8.5). We found that in recent decades the share of extremely warm days has at least doubled over the period December–January–February (DJF) in northern SA; less significant increases have been observed in southern SA. We also found that by midcentury, under the RCP4.5 scenario, extremely warm DJF days (as well as the number of HWs per season) are expected to increase by 5–10 times at locations close to the Equator and in the Atacama Desert. Increases are expected to be less pronounced in southern SA. Projections under the RCP8.5 scenario are more striking, particularly in tropical areas where half or more of the days could be extremely warm by midcentury. Nature Publishing Group UK 2019-06-03 /pmc/articles/PMC6547650/ /pubmed/31160642 http://dx.doi.org/10.1038/s41598-019-44614-4 Text en © The Author(s) 2019 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. |
spellingShingle | Article Feron, S. Cordero, R. R. Damiani, A. Llanillo, P. J. Jorquera, J. Sepulveda, E. Asencio, V. Laroze, D. Labbe, F. Carrasco, J. Torres, G. Observations and Projections of Heat Waves in South America |
title | Observations and Projections of Heat Waves in South America |
title_full | Observations and Projections of Heat Waves in South America |
title_fullStr | Observations and Projections of Heat Waves in South America |
title_full_unstemmed | Observations and Projections of Heat Waves in South America |
title_short | Observations and Projections of Heat Waves in South America |
title_sort | observations and projections of heat waves in south america |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6547650/ https://www.ncbi.nlm.nih.gov/pubmed/31160642 http://dx.doi.org/10.1038/s41598-019-44614-4 |
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