Mapping radiative cooling potential for africa under different climate change scenarios

dc.contributor.author
Monterrubio, Jesús
dc.contributor.author
Vilà Miró, Roger
dc.contributor.author
Medrano Martorell, Marc
dc.contributor.author
Martorell, Ingrid
dc.contributor.author
Castell, Albert
dc.date.accessioned
2026-03-02T19:14:52Z
dc.date.available
2026-03-02T19:14:52Z
dc.date.issued
2026
dc.identifier
https://doi.org/10.3389/fenvs.2025.1722292
dc.identifier
2296-665X
dc.identifier
https://hdl.handle.net/10459.1/469692
dc.identifier.uri
https://hdl.handle.net/10459.1/469692
dc.description.abstract
Africa, with a significant portion of its territory located within the tropical latitudes, experiences high cooling demands. Addressing these requirements in a renewable way is possible thanks to Radiative Cooling (RC). RC utilizes the atmospheric window from 8 to 13 µm to emit radiation to outer space, enabling the achievement of sub-ambient temperatures. A Kriging geospatial interpolation method is applied in this work to develop maps of RC potential, considering broadband emitters, for the typical meteorological year from 1991 to 2010 and predictions for 2030–2050 based on future emissions scenarios of the Intergovernmental Panel on Climate Change. A comparison is made between nighttime and all-day RC potential. The results reveal that all-day RC power potential is at least 22% higher than nighttime potential, while in terms of energy, the difference exceeds 156%. No significant variation is observed among future emissions scenarios. The average nighttime RC power potential exceeds 70 W⋅m−2, while the average all-day potential surpasses 87 W⋅m−2. Mean values for the nighttime RC energy potential are above 294 kWh·m-2, while all-day results are over 763 kWh·m-2. The potential of RC in many regions of Africa is promising and these maps will be a useful resource to estimate this RC potential.
dc.description.abstract
The author(s) declared that financial support was received for this work and/or its publication. This publication is part of the grant PID2021-126643OB-I00, funded by MCIN/AEI/10.13039/ 501100011033/and by “ERDF A way of making Europe”. This publication is part of the grant TED2021-131446B-I00, funded by MCIN/AEI/10.13039/501100011033/and by the “European Union NextGenerationEU/PRTR”. This publication is part of the grant PDC2022-133215-I00, funded by MCIN/AEI/10.13039/ 501100011033/and by the “European Union NextGenerationEU/ PRTR”. The authors would like to thank Generalitat de Catalunya for the project awarded to their research group (2021 SGR 01370). JM would like to thank the grant FPU22/01304 funded by MICIU/ AEI/10.13039/501100011033 and by “ESF+”.
dc.language
eng
dc.publisher
Frontiers Media
dc.relation
info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica, Técnica y de Innovación 2021-2023/PID2021-126643OB-I00/ES/
dc.relation
info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2021-2023/PDC2022-133215-I00/ES/PLUG AND PLAY RADIATIVE COLLECTOR AND EMITTER/
dc.relation
Reproducció del document publicat a https://doi.org/10.3389/fenvs.2025.1722292
dc.relation
Frontiers in Environmental Science, 2026, vol. 13, 1722292
dc.rights
cc-by (c) Jesús Monterrubio et al., 2026
dc.rights
Attribution 4.0 International
dc.rights
info:eu-repo/semantics/openAccess
dc.rights
http://creativecommons.org/licenses/by/4.0/
dc.subject
Africa
dc.subject
Climate change
dc.subject
Kriging
dc.subject
Mapping
dc.subject
Radiative cooling
dc.title
Mapping radiative cooling potential for africa under different climate change scenarios
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/publishedVersion


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