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Climate change-induced peatland drying in Southeast Asia Authors
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  • Nathan Dadap,
  • Alexander R Cobb,
  • Alison M Hoyt,
  • Charles F Harvey,
  • Andrew F Feldman,
  • Eun-Soon Im,
  • Alexandra G Konings
Nathan Dadap
Stanford University

Corresponding Author:[email protected]

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Alexander R Cobb
Singapore-MIT Alliance for Research and Technology
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Alison M Hoyt
Stanford University
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Charles F Harvey
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Andrew F Feldman
NASA Goddard Space Flight Center
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Eun-Soon Im
Hong Kong University of Science and Technology
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Alexandra G Konings
Stanford University
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When organic peat soils are sufficiently dry, they become flammable. In Southeast Asian peatlands, widespread deforestation and associated drainage create dry conditions that, when coupled with El Niño-driven drought, result in catastrophic fire events that release large amounts of carbon and deadly smoke to the atmosphere. While the effects of anthropogenic degradation on peat moisture and fire risk have been extensively demonstrated, climate change impacts to peat flammability are poorly understood. These impacts are likely to be mediated primarily through changes in soil moisture. Here, we used neural networks (trained on data from the NASA SMAP satellite) to model soil moisture as a function of climate, degradation, and location. The neural networks were forced with regional climate model projections for 1985-2005 and 2040-2060 climate under RCP8.5 forcing to predict changes in soil moisture. We find that reduced precipitation and increased evaporative demand will lead to median soil moisture decreases about half as strong as those observed during recent El Niño droughts. Such reductions may be expected to accelerate peat emissions. Our results also suggest that soil moisture in degraded areas with less tree cover may be more sensitive to climate change than in other land use types, motivating urgent peatland restoration. Climate change may play an important role in future soil moisture regimes and by extension, future peat fire in Southeast Asian peatlands.