Feedback between drought and deforestation in the Amazon
By A. Staal, B. Flores, A. Aguiar, J. Bosmans, I. Fetzer, O. Tuinenburg. Environmental Research Letters, 2020
190 citations recorded by the source corpus.
Deforestation and drought are among the greatest environmental pressures on the Amazon rainforest, possibly destabilizing the forest-climate system. Deforestation in the Amazon reduces rainfall regionally, while this deforestation itself has been reported to be facilitated by droughts. Here we quantify the interactions between drought and deforestation spatially across the Amazon during the early 21st century. First, we relate observed fluctuations in deforestation rates to dry-season intensity; second, we determine the effect of conversion of forest to cropland on evapotranspiration; and third, we simulate the subsequent downwind reductions in rainfall due to decreased atmospheric water input. We find large variability in the response of deforestation to dry-season intensity, with a significant but small average increase in deforestation rates with a more intense dry season: with every mm of water deficit, deforestation tends to increase by 0.13% per year. Deforestation, in turn, has caused an estimated 4% of the recent observed drying, with the south-western part of the Amazon being most strongly affected. Combining both effects, we quantify a reinforcing drought-deforestation feedback that is currently small, but becomes gradually stronger with cumulative deforestation. Our results suggest that global climate change, not deforestation, is the main driver of recent drying in the Amazon. However, a feedback between drought and deforestation implies that increases in either of them will impede efforts to curb both.
Subfields: Global and Planetary Change, Soil Science
View Paper: https://www.semanticscholar.org/paper/44f24fb87e5ffc7d23bc5c7b678893c877f1fe13
Citations in the corpus
- Forest microclimates and climate change: Importance, drivers and future research agenda (2021, unknown): “In the tropics, the combined effects of logging, droughts and fires on canopy loss (i.e., deforestation and degradation) can locally increase air dryness (Staal et al. 2020) and daily maximum temperatures more than the warming associated with high emission scenarios (Senior et al. 2017).”