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Forest response to rising CO2drives zonally asymmetric rainfall change over tropical land

  • Author(s): Kooperman, GJ
  • Chen, Y
  • Hoffman, FM
  • Koven, CD
  • Lindsay, K
  • Pritchard, MS
  • Swann, ALS
  • Randerson, JT
  • et al.
Abstract

© 2018 The Author(s). Understanding how anthropogenic CO2emissions will influence future precipitation is critical for sustainably managing ecosystems, particularly for drought-sensitive tropical forests. Although tropical precipitation change remains uncertain, nearly all models from the Coupled Model Intercomparison Project Phase 5 predict a strengthening zonal precipitation asymmetry by 2100, with relative increases over Asian and African tropical forests and decreases over South American forests. Here we show that the plant physiological response to increasing CO2is a primary mechanism responsible for this pattern. Applying a simulation design in the Community Earth System Model in which CO2increases are isolated over individual continents, we demonstrate that different circulation, moisture and stability changes arise over each continent due to declines in stomatal conductance and transpiration. The sum of local atmospheric responses over individual continents explains the pan-tropical precipitation asymmetry. Our analysis suggests that South American forests may be more vulnerable to rising CO2than Asian or African forests.

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