Impacts of forest loss on local climate across the conterminous United States: Evidence from satellite time-series observations.

Albedo Biophysical effects Evapotranspiration Forest loss Local land surface temperature

Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
01 Jan 2022
Historique:
received: 16 04 2021
revised: 09 08 2021
accepted: 09 08 2021
pubmed: 17 9 2021
medline: 16 11 2021
entrez: 16 9 2021
Statut: ppublish

Résumé

Forest disturbances alter land biophysics. Their impacts on local climate and land surface temperature (LST) cannot be directly measured by comparing pre- and post-disturbance observations of the same site over time (e.g., due to confounding such as background climate fluctuations); a common remedy is to compare spatially-adjacent undisturbed sites instead. This space-for-time substitution ignores the inherent biases in vegetation between two paired sites, interannual variations, and temporal dynamics of forest recovery. Besides, there is a lack of observation-based analyses at fine spatial resolutions capable of capturing spatial heterogeneity of small-scale forest disturbances. To address these limitations, here we report new satellite analyses on local climate impacts of forest loss at 30 m resolution. Our analyses combined multiple long-term satellite products (e.g., albedo and evapotranspiration [ET]) at 700 sites across major climate zones in the conterminous United States, using time-series trend and changepoint detection methods. Our method helped isolate the biophysical changes attributed to disturbances from those attributed to climate backgrounds and natural growth. On average, forest loss increased surface albedo, decreased ET, and reduced leaf area index (LAI). Net annual warming-an increase in LST-was observed after forest loss in the arid/semiarid, northern, tropical, and temperate regions, dominated by the warming from decreased ET and attenuated by the cooling from increased albedo. The magnitude of post-disturbance warming was related to precipitation; climate zones with greater precipitation showed stronger and longer warming. Reduction in leaf or LAI was larger in evergreen than deciduous forests, but the recovery in LAI did not always synchronize with those of albedo and ET. Overall, this study presents new evidence of biophysical effects of forest loss on LST at finer spatial resolutions; our time-series method can be further leveraged to derive local policy-relevant ecosystem climate regulation metrics or support model-based climate-biosphere studies.

Identifiants

pubmed: 34525747
pii: S0048-9697(21)04726-4
doi: 10.1016/j.scitotenv.2021.149651
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

149651

Informations de copyright

Copyright © 2021 Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

Yang Li (Y)

Environmental Science Graduate Program, The Ohio State University, Columbus, OH 43210, USA; School of Environment and Natural Resources, The Ohio State University, Columbus, OH 43210, USA. Electronic address: li.10015@osu.edu.

Yanlan Liu (Y)

School of Environment and Natural Resources, The Ohio State University, Columbus, OH 43210, USA; School of Earth Sciences, The Ohio State University, Columbus, OH 43210, USA.

Gil Bohrer (G)

Environmental Science Graduate Program, The Ohio State University, Columbus, OH 43210, USA; Department of Civil, Environmental and Geodetic Engineering, The Ohio State University, Columbus, OH 43210, USA.

Yongyang Cai (Y)

Department of Agricultural, Environmental, and Development Economics, The Ohio State University, Columbus, OH 43210, USA.

Aaron Wilson (A)

Byrd Polar and Climate Research Center, The Ohio State University, Columbus, OH 43210, USA; Department of Extension, The Ohio State University, Columbus, OH 43210, USA.

Tongxi Hu (T)

Environmental Science Graduate Program, The Ohio State University, Columbus, OH 43210, USA; School of Environment and Natural Resources, The Ohio State University, Columbus, OH 43210, USA.

Zhihao Wang (Z)

Department of Geographical Sciences, University of Maryland, College Park, MD 20742, USA.

Kaiguang Zhao (K)

Environmental Science Graduate Program, The Ohio State University, Columbus, OH 43210, USA; School of Environment and Natural Resources, The Ohio State University, Columbus, OH 43210, USA. Electronic address: zhao.1423@osu.edu.

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