A Century of Reforestation Reduced Anthropogenic Warming in the Eastern United States

Abstract Restoring and preserving the world's forests are promising natural pathways to mitigate some aspects of climate change. In addition to regulating atmospheric carbon dioxide concentrations, forests modify surface and near‐surface air temperatures through biophysical processes. In the ea...

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Main Authors: Mallory L. Barnes, Quan Zhang, Scott M. Robeson, Lily Young, Elizabeth A. Burakowski, A. Christopher. Oishi, Paul C. Stoy, Gaby Katul, Kimberly A. Novick
Format: Article
Language:English
Published: Wiley 2024-02-01
Series:Earth's Future
Subjects:
Online Access:https://doi.org/10.1029/2023EF003663
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author Mallory L. Barnes
Quan Zhang
Scott M. Robeson
Lily Young
Elizabeth A. Burakowski
A. Christopher. Oishi
Paul C. Stoy
Gaby Katul
Kimberly A. Novick
author_facet Mallory L. Barnes
Quan Zhang
Scott M. Robeson
Lily Young
Elizabeth A. Burakowski
A. Christopher. Oishi
Paul C. Stoy
Gaby Katul
Kimberly A. Novick
author_sort Mallory L. Barnes
collection DOAJ
description Abstract Restoring and preserving the world's forests are promising natural pathways to mitigate some aspects of climate change. In addition to regulating atmospheric carbon dioxide concentrations, forests modify surface and near‐surface air temperatures through biophysical processes. In the eastern United States (EUS), widespread reforestation during the 20th century coincided with an anomalous lack of warming, raising questions about reforestation's contribution to local cooling and climate mitigation. Using new cross‐scale approaches and multiple independent sources of data, we uncovered links between reforestation and the response of both surface and air temperature in the EUS. Ground‐ and satellite‐based observations showed that EUS forests cool the land surface by 1–2°C annually compared to nearby grasslands and croplands, with the strongest cooling effect during midday in the growing season, when cooling is 2–5°C. Young forests (20–40 years) have the strongest cooling effect on surface temperature. Surface cooling extends to the near‐surface air, with forests reducing midday air temperature by up to 1°C compared to nearby non‐forests. Analyses of historical land cover and air temperature trends showed that the cooling benefits of reforestation extend across the landscape. Locations surrounded by reforestation were up to 1°C cooler than neighboring locations that did not undergo land cover change, and areas dominated by regrowing forests were associated with cooling temperature trends in much of the EUS. Our work indicates reforestation contributed to the historically slow pace of warming in the EUS, underscoring reforestation's potential as a local climate adaptation strategy in temperate regions.
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spelling doaj.art-061bce387fd2481cb50769b4f5a387b52024-03-05T11:10:50ZengWileyEarth's Future2328-42772024-02-01122n/an/a10.1029/2023EF003663A Century of Reforestation Reduced Anthropogenic Warming in the Eastern United StatesMallory L. Barnes0Quan Zhang1Scott M. Robeson2Lily Young3Elizabeth A. Burakowski4A. Christopher. Oishi5Paul C. Stoy6Gaby Katul7Kimberly A. Novick8O'Neill School of Public and Environmental Affairs Indiana University Bloomington IN USAState Key Laboratory of Water Resources and Hydropower Engineering Science Wuhan University Wuhan ChinaDepartment of Geography Indiana University Bloomington IN USAO'Neill School of Public and Environmental Affairs Indiana University Bloomington IN USAInstitute for the Study of Earth, Oceans, and Space University of New Hampshire Durham NH USACoweeta Hydrologic Laboratory USDA Forest Service Southern Research Station Otto NC USADepartment of Biological Systems Engineering University of Wisconsin–Madison Madison WI USADepartment of Civil and Environmental Engineering Duke University Durham NC USAO'Neill School of Public and Environmental Affairs Indiana University Bloomington IN USAAbstract Restoring and preserving the world's forests are promising natural pathways to mitigate some aspects of climate change. In addition to regulating atmospheric carbon dioxide concentrations, forests modify surface and near‐surface air temperatures through biophysical processes. In the eastern United States (EUS), widespread reforestation during the 20th century coincided with an anomalous lack of warming, raising questions about reforestation's contribution to local cooling and climate mitigation. Using new cross‐scale approaches and multiple independent sources of data, we uncovered links between reforestation and the response of both surface and air temperature in the EUS. Ground‐ and satellite‐based observations showed that EUS forests cool the land surface by 1–2°C annually compared to nearby grasslands and croplands, with the strongest cooling effect during midday in the growing season, when cooling is 2–5°C. Young forests (20–40 years) have the strongest cooling effect on surface temperature. Surface cooling extends to the near‐surface air, with forests reducing midday air temperature by up to 1°C compared to nearby non‐forests. Analyses of historical land cover and air temperature trends showed that the cooling benefits of reforestation extend across the landscape. Locations surrounded by reforestation were up to 1°C cooler than neighboring locations that did not undergo land cover change, and areas dominated by regrowing forests were associated with cooling temperature trends in much of the EUS. Our work indicates reforestation contributed to the historically slow pace of warming in the EUS, underscoring reforestation's potential as a local climate adaptation strategy in temperate regions.https://doi.org/10.1029/2023EF003663natural climate solutionsreforestationbiophysical impactsclimate adaptation
spellingShingle Mallory L. Barnes
Quan Zhang
Scott M. Robeson
Lily Young
Elizabeth A. Burakowski
A. Christopher. Oishi
Paul C. Stoy
Gaby Katul
Kimberly A. Novick
A Century of Reforestation Reduced Anthropogenic Warming in the Eastern United States
Earth's Future
natural climate solutions
reforestation
biophysical impacts
climate adaptation
title A Century of Reforestation Reduced Anthropogenic Warming in the Eastern United States
title_full A Century of Reforestation Reduced Anthropogenic Warming in the Eastern United States
title_fullStr A Century of Reforestation Reduced Anthropogenic Warming in the Eastern United States
title_full_unstemmed A Century of Reforestation Reduced Anthropogenic Warming in the Eastern United States
title_short A Century of Reforestation Reduced Anthropogenic Warming in the Eastern United States
title_sort century of reforestation reduced anthropogenic warming in the eastern united states
topic natural climate solutions
reforestation
biophysical impacts
climate adaptation
url https://doi.org/10.1029/2023EF003663
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