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Deforestation-induced warming over tropical mountain regions regulated by elevation

Deforestation-induced warming over tropical mountain regions regulated by elevation
Deforestation-induced warming over tropical mountain regions regulated by elevation

Agriculture is expanding in tropical mountainous areas, yet its climatic effect is poorly understood. Here, we investigate how elevation regulates the biophysical climate impacts of deforestation over tropical mountainous areas by integrating satellite-observed forest cover changes into a high-resolution land–atmosphere coupled model. We show that recent forest conversion between 2000 and 2014 increased the regional warming by 0.022 ± 0.002 °C in the Southeast Asian Massif, 0.010 ± 0.007 °C in the Barisan Mountains (Maritime Southeast Asia), 0.042 ± 0.010 °C in the Serra da Espinhaço (South America) and 0.047 ± 0.008 °C in the Albertine Rift mountains (Africa) during the local dry season. The deforestation-driven local temperature anomaly can reach up to 2 °C where forest conversion is extensive. The warming from mountain deforestation depends on elevation, through the intertwined and opposing effects of increased albedo causing cooling and decreased evapotranspiration causing warming. As the elevation increases, the albedo effect increases in importance and the warming effect decreases, analogous to previously highlighted decreases of deforestation-induced warming with increasing latitude. As most new croplands are encroaching lands at low to moderate elevations, deforestation produces higher warming from suppressed evapotranspiration. Impacts of this additional warming on crop yields, land degradation and biodiversity of nearby intact ecosystems should be incorporated into future assessments.

1752-0894
23-29
Zeng, Zhenzhong
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Wang, Dashan
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Yang, Long
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Wu, Jie
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Ziegler, Alan D.
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Liu, Maofeng
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Ciais, Philippe
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Searchinger, Timothy D.
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Yang, Zong-liang
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Chen, Deliang
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Chen, Anping
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Li, Laurent Z. X.
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Piao, Shilong
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Taylor, David
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Cai, Xitian
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Pan, Ming
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Peng, Liqing
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Lin, Peirong
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Gower, Drew
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Feng, Yu
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Zheng, Chunmiao
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Guan, Kaiyu
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Lian, Xu
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Wang, Tao
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Wang, Lang
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Jeong, Su-jong
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Wei, Zhongwang
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Sheffield, Justin
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Caylor, Kelly
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Wood, Eric F.
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Zeng, Zhenzhong
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Wang, Dashan
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Yang, Long
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Wu, Jie
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Ziegler, Alan D.
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Liu, Maofeng
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Ciais, Philippe
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Searchinger, Timothy D.
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Yang, Zong-liang
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Chen, Deliang
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Chen, Anping
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Li, Laurent Z. X.
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Piao, Shilong
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Taylor, David
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Cai, Xitian
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Pan, Ming
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Peng, Liqing
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Lin, Peirong
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Gower, Drew
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Feng, Yu
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Zheng, Chunmiao
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Guan, Kaiyu
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Lian, Xu
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Wang, Tao
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Wang, Lang
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Jeong, Su-jong
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Wei, Zhongwang
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Sheffield, Justin
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Caylor, Kelly
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Wood, Eric F.
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Zeng, Zhenzhong, Wang, Dashan, Yang, Long, Wu, Jie, Ziegler, Alan D., Liu, Maofeng, Ciais, Philippe, Searchinger, Timothy D., Yang, Zong-liang, Chen, Deliang, Chen, Anping, Li, Laurent Z. X., Piao, Shilong, Taylor, David, Cai, Xitian, Pan, Ming, Peng, Liqing, Lin, Peirong, Gower, Drew, Feng, Yu, Zheng, Chunmiao, Guan, Kaiyu, Lian, Xu, Wang, Tao, Wang, Lang, Jeong, Su-jong, Wei, Zhongwang, Sheffield, Justin, Caylor, Kelly and Wood, Eric F. (2021) Deforestation-induced warming over tropical mountain regions regulated by elevation. Nature Geoscience, 14 (1), 23-29. (doi:10.1038/s41561-020-00666-0).

Record type: Article

Abstract

Agriculture is expanding in tropical mountainous areas, yet its climatic effect is poorly understood. Here, we investigate how elevation regulates the biophysical climate impacts of deforestation over tropical mountainous areas by integrating satellite-observed forest cover changes into a high-resolution land–atmosphere coupled model. We show that recent forest conversion between 2000 and 2014 increased the regional warming by 0.022 ± 0.002 °C in the Southeast Asian Massif, 0.010 ± 0.007 °C in the Barisan Mountains (Maritime Southeast Asia), 0.042 ± 0.010 °C in the Serra da Espinhaço (South America) and 0.047 ± 0.008 °C in the Albertine Rift mountains (Africa) during the local dry season. The deforestation-driven local temperature anomaly can reach up to 2 °C where forest conversion is extensive. The warming from mountain deforestation depends on elevation, through the intertwined and opposing effects of increased albedo causing cooling and decreased evapotranspiration causing warming. As the elevation increases, the albedo effect increases in importance and the warming effect decreases, analogous to previously highlighted decreases of deforestation-induced warming with increasing latitude. As most new croplands are encroaching lands at low to moderate elevations, deforestation produces higher warming from suppressed evapotranspiration. Impacts of this additional warming on crop yields, land degradation and biodiversity of nearby intact ecosystems should be incorporated into future assessments.

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More information

Accepted/In Press date: 11 November 2020
e-pub ahead of print date: 14 December 2020
Published date: 1 January 2021

Identifiers

Local EPrints ID: 448522
URI: http://eprints.soton.ac.uk/id/eprint/448522
ISSN: 1752-0894
PURE UUID: 42b580c6-b443-448c-bfa7-872236a2ea63
ORCID for Justin Sheffield: ORCID iD orcid.org/0000-0003-2400-0630

Catalogue record

Date deposited: 23 Apr 2021 16:36
Last modified: 17 Mar 2024 03:40

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Contributors

Author: Zhenzhong Zeng
Author: Dashan Wang
Author: Long Yang
Author: Jie Wu
Author: Alan D. Ziegler
Author: Maofeng Liu
Author: Philippe Ciais
Author: Timothy D. Searchinger
Author: Zong-liang Yang
Author: Deliang Chen
Author: Anping Chen
Author: Laurent Z. X. Li
Author: Shilong Piao
Author: David Taylor
Author: Xitian Cai
Author: Ming Pan
Author: Liqing Peng
Author: Peirong Lin
Author: Drew Gower
Author: Yu Feng
Author: Chunmiao Zheng
Author: Kaiyu Guan
Author: Xu Lian
Author: Tao Wang
Author: Lang Wang
Author: Su-jong Jeong
Author: Zhongwang Wei
Author: Kelly Caylor
Author: Eric F. Wood

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