Cargando…

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...

Descripción completa

Detalles Bibliográficos
Autores principales: Parkes, B., Buzan, J. R., Huber, M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer Berlin Heidelberg 2022
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
_version_ 1784751233814233088
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
work_keys_str_mv AT parkesb heatstressinafricaunderhighintensityclimatechange
AT buzanjr heatstressinafricaunderhighintensityclimatechange
AT huberm heatstressinafricaunderhighintensityclimatechange