Deforestation-induced surface warming is influenced by the fragmentation and spatial extent of forest loss in Maritime Southeast Asia

Deforestation in the tropics causes warming which contributes to regional climate change. Forest loss occurs over a broad range of spatial scales, producing a variety of spatial patterns of cleared and forested land. Whether the spatial attributes of these patterns influence the resulting temperatur...

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Main Authors: Octavia Crompton, Débora Corrêa, John Duncan, Sally Thompson
Format: Article
Language:English
Published: IOP Publishing 2021-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/ac2fdc
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author Octavia Crompton
Débora Corrêa
John Duncan
Sally Thompson
author_facet Octavia Crompton
Débora Corrêa
John Duncan
Sally Thompson
author_sort Octavia Crompton
collection DOAJ
description Deforestation in the tropics causes warming which contributes to regional climate change. Forest loss occurs over a broad range of spatial scales, producing a variety of spatial patterns of cleared and forested land. Whether the spatial attributes of these patterns influence the resulting temperature change remains largely unknown. We adopted a differences-in-differences approach to analyse remotely-sensed forest loss and land surface temperature (LST) data in maritime Southeast Asia. We found that deforestation increased LST, as expected, but that the temperature increases were smaller when forest loss produced more fragmented landscapes in which non-forest and forest edges were heavily interlaced. Temperature increases were greater where the forest loss was more extensive. Warming also extended beyond the location of forest removal, so that forest loss increased temperatures in undisturbed locations up to 6 km away. Different spatial patterns of land clearing, for example, as might be produced by small-holder agriculture as opposed to large-scale deforestation, would therefore have different impacts on the local climate. Conserving forests within 4 km of farmland, urban areas or other sensitive environments may help to avoid temperature increases that reduce land productivity and worsen human health.
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spelling doaj.art-7d16682c2dcb45f8bf2b6ea7b8c18bdc2023-08-09T15:07:23ZengIOP PublishingEnvironmental Research Letters1748-93262021-01-01161111401810.1088/1748-9326/ac2fdcDeforestation-induced surface warming is influenced by the fragmentation and spatial extent of forest loss in Maritime Southeast AsiaOctavia Crompton0https://orcid.org/0000-0002-3576-6159Débora Corrêa1John Duncan2Sally Thompson3Department of Civil and Environmental Engineering, University of Western Australia, Perth, Australia , Crawley, WA 6009, AustraliaComplex Systems Group, Department of Mathematics and Statistics, University of Western Australia , Crawley, WA 6009, Australia; ARC Industrial Transformation Training Centre (Transforming Maintenance through Data Science), University of Western Australia , Crawley, WA 6009, AustraliaSchool of Agriculture and Environment, University of Western Australia , Crawley, WA 6009, AustraliaDepartment of Civil and Environmental Engineering, University of Western Australia, Perth, Australia , Crawley, WA 6009, AustraliaDeforestation in the tropics causes warming which contributes to regional climate change. Forest loss occurs over a broad range of spatial scales, producing a variety of spatial patterns of cleared and forested land. Whether the spatial attributes of these patterns influence the resulting temperature change remains largely unknown. We adopted a differences-in-differences approach to analyse remotely-sensed forest loss and land surface temperature (LST) data in maritime Southeast Asia. We found that deforestation increased LST, as expected, but that the temperature increases were smaller when forest loss produced more fragmented landscapes in which non-forest and forest edges were heavily interlaced. Temperature increases were greater where the forest loss was more extensive. Warming also extended beyond the location of forest removal, so that forest loss increased temperatures in undisturbed locations up to 6 km away. Different spatial patterns of land clearing, for example, as might be produced by small-holder agriculture as opposed to large-scale deforestation, would therefore have different impacts on the local climate. Conserving forests within 4 km of farmland, urban areas or other sensitive environments may help to avoid temperature increases that reduce land productivity and worsen human health.https://doi.org/10.1088/1748-9326/ac2fdcforestsfragmentationland use and land cover changeremote sensingtemperaturespatial pattern
spellingShingle Octavia Crompton
Débora Corrêa
John Duncan
Sally Thompson
Deforestation-induced surface warming is influenced by the fragmentation and spatial extent of forest loss in Maritime Southeast Asia
Environmental Research Letters
forests
fragmentation
land use and land cover change
remote sensing
temperature
spatial pattern
title Deforestation-induced surface warming is influenced by the fragmentation and spatial extent of forest loss in Maritime Southeast Asia
title_full Deforestation-induced surface warming is influenced by the fragmentation and spatial extent of forest loss in Maritime Southeast Asia
title_fullStr Deforestation-induced surface warming is influenced by the fragmentation and spatial extent of forest loss in Maritime Southeast Asia
title_full_unstemmed Deforestation-induced surface warming is influenced by the fragmentation and spatial extent of forest loss in Maritime Southeast Asia
title_short Deforestation-induced surface warming is influenced by the fragmentation and spatial extent of forest loss in Maritime Southeast Asia
title_sort deforestation induced surface warming is influenced by the fragmentation and spatial extent of forest loss in maritime southeast asia
topic forests
fragmentation
land use and land cover change
remote sensing
temperature
spatial pattern
url https://doi.org/10.1088/1748-9326/ac2fdc
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