2020
DOI: 10.1038/s41598-020-60938-y
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Protection of Permafrost Soils from Thawing by Increasing Herbivore Density

Abstract: climate change will cause a substantial future greenhouse gas release from warming and thawing permafrost-affected soils to the atmosphere enabling a positive feedback mechanism. Increasing the population density of big herbivores in northern high-latitude ecosystems will increase snow density and hence decrease the insulation strength of snow during winter. As a consequence, theoretically 80% of current permafrost-affected soils (<10 m) is projected to remain until 2100 even when assuming a strong warming usi… Show more

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Cited by 42 publications
(28 citation statements)
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“…By increasing the rate of decomposition, forest expansion causes net release of carbon from the ecosystem to the atmosphere (Zimov et al 2009, Hartley et al 2012). Mammalian herbivory prevents forest expansion (Olofsson et al 2009, Aune et al 2011, Olofsson and Post 2018), protects permafrost against melting, which could release large amounts of carbon to atmosphere (Beer et al 2020) and can increase the capacity of ecosystems to sequester carbon (Zimov et al 2009, Väisänen et al 2014). Moreover, the high surface albedo of the tundra cools down the planet (Cohen et al 2013, Cromsigt et al 2018), providing an appreciable ecosystem service.…”
Section: Discussionmentioning
confidence: 99%
“…By increasing the rate of decomposition, forest expansion causes net release of carbon from the ecosystem to the atmosphere (Zimov et al 2009, Hartley et al 2012). Mammalian herbivory prevents forest expansion (Olofsson et al 2009, Aune et al 2011, Olofsson and Post 2018), protects permafrost against melting, which could release large amounts of carbon to atmosphere (Beer et al 2020) and can increase the capacity of ecosystems to sequester carbon (Zimov et al 2009, Väisänen et al 2014). Moreover, the high surface albedo of the tundra cools down the planet (Cohen et al 2013, Cromsigt et al 2018), providing an appreciable ecosystem service.…”
Section: Discussionmentioning
confidence: 99%
“…By enhancing the atmospheric vapor pressure deficit (VPD) 13 , 14 , even in remote subarctic regions, increased evapotranspiration impacts in particular the tree’s water relation. Ongoing anthropogenic warming already has significant negative effects on Siberian forest ecosystems, leading to increased permafrost degradation and CO 2 emissions 15 . Along with temperature increases, increasing VPD 14 has been shown to result in low stomatal conductance 3 , thereby responding to water shortage in trees—even in regions affected by permafrost 3 .…”
Section: Introductionmentioning
confidence: 99%
“…Our study thus suggests that the buffering effect of large herbivores against vegetation changes extends from the tundra to forest understories as well. Increasing herbivore densities has been suggested as a way to protect permafrost in the boreal and tundra biomes from warming temperatures (Beer et al, 2020) , our study suggests that large herbivores could potentially be useful in protecting plant communities beyond permafrost areas as well.…”
Section: Discussionmentioning
confidence: 62%