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Heat stress in Africa under high intensity climate change
Extreme weather events are major causes of loss of life and damage infrastructure worldwide. High temperatures cause heat stress on humans, livestock, crops and infrastructure. Heat stress exposure is projected to increase with ongoing climate change. Extremes of temperature are common in Africa and...
Autores principales: | , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Springer Berlin Heidelberg
2022
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9300535/ https://www.ncbi.nlm.nih.gov/pubmed/35713697 http://dx.doi.org/10.1007/s00484-022-02295-1 |
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author | Parkes, B. Buzan, J. R. Huber, M. |
author_facet | Parkes, B. Buzan, J. R. Huber, M. |
author_sort | Parkes, B. |
collection | PubMed |
description | Extreme weather events are major causes of loss of life and damage infrastructure worldwide. High temperatures cause heat stress on humans, livestock, crops and infrastructure. Heat stress exposure is projected to increase with ongoing climate change. Extremes of temperature are common in Africa and infrastructure is often incapable of providing adequate cooling. We show how easily accessible cooling technology, such as evaporative coolers, prevent heat stress in historic timescales but are unsuitable as a solution under climate change. As temperatures increase, powered cooling, such as air conditioning, is necessary to prevent overheating. This will, in turn, increase demand on already stretched infrastructure. We use high temporal resolution climate model data to estimate the demand for cooling according to two metrics, firstly the apparent temperature and secondly the discomfort index. For each grid cell we calculate the heat stress value and the amount of cooling required to turn a heat stress event into a non heat stress event. We show the increase in demand for cooling in Africa is non uniform and that equatorial countries are exposed to higher heat stress than higher latitude countries. We further show that evaporative coolers are less effective in tropical regions than in the extra tropics. Finally, we show that neither low nor high efficiency coolers are sufficient to return Africa to current levels of heat stress under climate change. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s00484-022-02295-1. |
format | Online Article Text |
id | pubmed-9300535 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2022 |
publisher | Springer Berlin Heidelberg |
record_format | MEDLINE/PubMed |
spelling | pubmed-93005352022-07-22 Heat stress in Africa under high intensity climate change Parkes, B. Buzan, J. R. Huber, M. Int J Biometeorol Original Paper Extreme weather events are major causes of loss of life and damage infrastructure worldwide. High temperatures cause heat stress on humans, livestock, crops and infrastructure. Heat stress exposure is projected to increase with ongoing climate change. Extremes of temperature are common in Africa and infrastructure is often incapable of providing adequate cooling. We show how easily accessible cooling technology, such as evaporative coolers, prevent heat stress in historic timescales but are unsuitable as a solution under climate change. As temperatures increase, powered cooling, such as air conditioning, is necessary to prevent overheating. This will, in turn, increase demand on already stretched infrastructure. We use high temporal resolution climate model data to estimate the demand for cooling according to two metrics, firstly the apparent temperature and secondly the discomfort index. For each grid cell we calculate the heat stress value and the amount of cooling required to turn a heat stress event into a non heat stress event. We show the increase in demand for cooling in Africa is non uniform and that equatorial countries are exposed to higher heat stress than higher latitude countries. We further show that evaporative coolers are less effective in tropical regions than in the extra tropics. Finally, we show that neither low nor high efficiency coolers are sufficient to return Africa to current levels of heat stress under climate change. SUPPLEMENTARY INFORMATION: The online version contains supplementary material available at 10.1007/s00484-022-02295-1. Springer Berlin Heidelberg 2022-06-17 2022 /pmc/articles/PMC9300535/ /pubmed/35713697 http://dx.doi.org/10.1007/s00484-022-02295-1 Text en © The Author(s) 2022 https://creativecommons.org/licenses/by/4.0/Open AccessThis 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 licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence 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 licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Original Paper Parkes, B. Buzan, J. R. Huber, M. Heat stress in Africa under high intensity climate change |
title | Heat stress in Africa under high intensity climate change |
title_full | Heat stress in Africa under high intensity climate change |
title_fullStr | Heat stress in Africa under high intensity climate change |
title_full_unstemmed | Heat stress in Africa under high intensity climate change |
title_short | Heat stress in Africa under high intensity climate change |
title_sort | heat stress in africa under high intensity climate change |
topic | Original Paper |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9300535/ https://www.ncbi.nlm.nih.gov/pubmed/35713697 http://dx.doi.org/10.1007/s00484-022-02295-1 |
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