Global Patterns and Dynamics of Burned Area and Burn Severity

It is a widespread assumption that burned area and severity are increasing worldwide due to climate change. This issue has motivated former analysis based on satellite imagery, revealing a decreasing trend in global burned areas. However, few studies have addressed burn severity trends, rarely relat...

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Published in:Remote Sensing
Main Authors: Víctor Fernández-García, Esteban Alonso-González
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15133401
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spelling ftmdpi:oai:mdpi.com:/2072-4292/15/13/3401/ 2023-08-20T04:10:06+02:00 Global Patterns and Dynamics of Burned Area and Burn Severity Víctor Fernández-García Esteban Alonso-González agris 2023-07-04 application/pdf https://doi.org/10.3390/rs15133401 EN eng Multidisciplinary Digital Publishing Institute Forest Remote Sensing https://dx.doi.org/10.3390/rs15133401 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 13; Pages: 3401 fire severity burn severity spatial patterns trends biomes continents climate warming Text 2023 ftmdpi https://doi.org/10.3390/rs15133401 2023-08-01T10:44:39Z It is a widespread assumption that burned area and severity are increasing worldwide due to climate change. This issue has motivated former analysis based on satellite imagery, revealing a decreasing trend in global burned areas. However, few studies have addressed burn severity trends, rarely relating them to climate variables, and none of them at the global scale. Within this context, we characterized the spatiotemporal patterns of burned area and severity by biomes and continents and we analyzed their relationships with climate over 17 years. African flooded and non-flooded grasslands and savannas were the most fire-prone biomes on Earth, whereas taiga and tundra exhibited the highest burn severity. Our temporal analysis updated the evidence of a decreasing trend in the global burned area (−1.50% year−1; p < 0.01) and revealed increases in the fraction of burned area affected by high severity (0.95% year−1; p < 0.05). Likewise, the regions with significant increases in mean burn severity, and burned areas at high severity outnumbered those with significant decreases. Among them, increases in severely burned areas in the temperate broadleaf and mixed forests of South America and tropical moist broadleaf forests of Australia were particularly intense. Although the spatial patterns of burned area and severity are clearly driven by climate, we did not find climate warming to increase burned area and burn severity over time, suggesting other factors as the primary drivers of current shifts in fire regimes at the planetary scale. Text taiga Tundra MDPI Open Access Publishing Remote Sensing 15 13 3401
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic fire severity
burn severity
spatial patterns
trends
biomes
continents
climate warming
spellingShingle fire severity
burn severity
spatial patterns
trends
biomes
continents
climate warming
Víctor Fernández-García
Esteban Alonso-González
Global Patterns and Dynamics of Burned Area and Burn Severity
topic_facet fire severity
burn severity
spatial patterns
trends
biomes
continents
climate warming
description It is a widespread assumption that burned area and severity are increasing worldwide due to climate change. This issue has motivated former analysis based on satellite imagery, revealing a decreasing trend in global burned areas. However, few studies have addressed burn severity trends, rarely relating them to climate variables, and none of them at the global scale. Within this context, we characterized the spatiotemporal patterns of burned area and severity by biomes and continents and we analyzed their relationships with climate over 17 years. African flooded and non-flooded grasslands and savannas were the most fire-prone biomes on Earth, whereas taiga and tundra exhibited the highest burn severity. Our temporal analysis updated the evidence of a decreasing trend in the global burned area (−1.50% year−1; p < 0.01) and revealed increases in the fraction of burned area affected by high severity (0.95% year−1; p < 0.05). Likewise, the regions with significant increases in mean burn severity, and burned areas at high severity outnumbered those with significant decreases. Among them, increases in severely burned areas in the temperate broadleaf and mixed forests of South America and tropical moist broadleaf forests of Australia were particularly intense. Although the spatial patterns of burned area and severity are clearly driven by climate, we did not find climate warming to increase burned area and burn severity over time, suggesting other factors as the primary drivers of current shifts in fire regimes at the planetary scale.
format Text
author Víctor Fernández-García
Esteban Alonso-González
author_facet Víctor Fernández-García
Esteban Alonso-González
author_sort Víctor Fernández-García
title Global Patterns and Dynamics of Burned Area and Burn Severity
title_short Global Patterns and Dynamics of Burned Area and Burn Severity
title_full Global Patterns and Dynamics of Burned Area and Burn Severity
title_fullStr Global Patterns and Dynamics of Burned Area and Burn Severity
title_full_unstemmed Global Patterns and Dynamics of Burned Area and Burn Severity
title_sort global patterns and dynamics of burned area and burn severity
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15133401
op_coverage agris
genre taiga
Tundra
genre_facet taiga
Tundra
op_source Remote Sensing; Volume 15; Issue 13; Pages: 3401
op_relation Forest Remote Sensing
https://dx.doi.org/10.3390/rs15133401
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15133401
container_title Remote Sensing
container_volume 15
container_issue 13
container_start_page 3401
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