Large-scale semi-arid afforestation can enhance precipitation and carbon sequestration potential

Abstract Afforestation is an important approach to mitigate global warming. Its complex interactions with the climate system, however, makes it controversial. Afforestation is expected to be effective in the tropics where biogeochemical and biogeophysical effects act in concert; however, its potenti...

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Autores principales: Gil Yosef, Robert Walko, Roni Avisar, Fedor Tatarinov, Eyal Rotenberg, Dan Yakir
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Lenguaje:EN
Publicado: Nature Portfolio 2018
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Acceso en línea:https://doaj.org/article/b93fbe67dae240efb92a90936f6393b6
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spelling oai:doaj.org-article:b93fbe67dae240efb92a90936f6393b62021-12-02T15:07:57ZLarge-scale semi-arid afforestation can enhance precipitation and carbon sequestration potential10.1038/s41598-018-19265-62045-2322https://doaj.org/article/b93fbe67dae240efb92a90936f6393b62018-01-01T00:00:00Zhttps://doi.org/10.1038/s41598-018-19265-6https://doaj.org/toc/2045-2322Abstract Afforestation is an important approach to mitigate global warming. Its complex interactions with the climate system, however, makes it controversial. Afforestation is expected to be effective in the tropics where biogeochemical and biogeophysical effects act in concert; however, its potential in the large semi-arid regions remains insufficiently explored. Here, we use a Global Climate Model to provide a process-based demonstration that implementing measured characteristics of a successful semi-arid afforestation system (2000 ha, ~300 mm mean annual precipitation) over large areas (~200 million ha) of similar precipitation levels in the Sahel and North Australia leads to the weakening and shifting of regional low-level jets, enhancing moisture penetration and precipitation (+0.8 ± 0.1 mm d−1 over the Sahel and +0.4 ± 0.1 mm d−1 over North Australia), influencing areas larger than the original afforestation. These effects are associated with increasing root depth and surface roughness and with decreasing albedo. This results in enhanced evapotranspiration, surface cooling and the modification of the latitudinal temperature gradient. It is estimated that the carbon sequestration potential of such large-scale semi-arid afforestation can be on the order of ~10% of the global carbon sink of the land biosphere and would overwhelm any biogeophysical warming effects within ~6 years.Gil YosefRobert WalkoRoni AvisarFedor TatarinovEyal RotenbergDan YakirNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 8, Iss 1, Pp 1-10 (2018)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Gil Yosef
Robert Walko
Roni Avisar
Fedor Tatarinov
Eyal Rotenberg
Dan Yakir
Large-scale semi-arid afforestation can enhance precipitation and carbon sequestration potential
description Abstract Afforestation is an important approach to mitigate global warming. Its complex interactions with the climate system, however, makes it controversial. Afforestation is expected to be effective in the tropics where biogeochemical and biogeophysical effects act in concert; however, its potential in the large semi-arid regions remains insufficiently explored. Here, we use a Global Climate Model to provide a process-based demonstration that implementing measured characteristics of a successful semi-arid afforestation system (2000 ha, ~300 mm mean annual precipitation) over large areas (~200 million ha) of similar precipitation levels in the Sahel and North Australia leads to the weakening and shifting of regional low-level jets, enhancing moisture penetration and precipitation (+0.8 ± 0.1 mm d−1 over the Sahel and +0.4 ± 0.1 mm d−1 over North Australia), influencing areas larger than the original afforestation. These effects are associated with increasing root depth and surface roughness and with decreasing albedo. This results in enhanced evapotranspiration, surface cooling and the modification of the latitudinal temperature gradient. It is estimated that the carbon sequestration potential of such large-scale semi-arid afforestation can be on the order of ~10% of the global carbon sink of the land biosphere and would overwhelm any biogeophysical warming effects within ~6 years.
format article
author Gil Yosef
Robert Walko
Roni Avisar
Fedor Tatarinov
Eyal Rotenberg
Dan Yakir
author_facet Gil Yosef
Robert Walko
Roni Avisar
Fedor Tatarinov
Eyal Rotenberg
Dan Yakir
author_sort Gil Yosef
title Large-scale semi-arid afforestation can enhance precipitation and carbon sequestration potential
title_short Large-scale semi-arid afforestation can enhance precipitation and carbon sequestration potential
title_full Large-scale semi-arid afforestation can enhance precipitation and carbon sequestration potential
title_fullStr Large-scale semi-arid afforestation can enhance precipitation and carbon sequestration potential
title_full_unstemmed Large-scale semi-arid afforestation can enhance precipitation and carbon sequestration potential
title_sort large-scale semi-arid afforestation can enhance precipitation and carbon sequestration potential
publisher Nature Portfolio
publishDate 2018
url https://doaj.org/article/b93fbe67dae240efb92a90936f6393b6
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