2017
DOI: 10.1002/2017jg004008
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Simulation of the Unexpected Photosynthetic Seasonality in Amazonian Evergreen Forests by Using an Improved Diffuse Fraction‐Based Light Use Efficiency Model

Abstract: Understanding the mechanism of photosynthetic seasonality in Amazonian evergreen forests is critical for its formulation in global climate and carbon cycle models. However, the control of the unexpected photosynthetic seasonality is highly uncertain. Here we use eddy‐covariance data across a network of Amazonian research sites and a novel evapotranspiration (E) and two‐leaf‐photosynthesis‐coupled model to investigate links between photosynthetic seasonality and climate factors on monthly scales. It reproduces … Show more

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Cited by 16 publications
(28 citation statements)
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“…The water stress factor EF is calculated: EF=EPETPT where PET PT is the potential evaporation (Priestley & Taylor, ) and E is actual evapotranspiration calculated from the Air Relative Humidity‐Based Two‐Source E model (Yan et al, ) that simulates the surface energy balance, soil water balance, and environmental constraints on E with inputs of remotely sensed LAI, surface meteorological data, and maximum soil available water content. Maximum soil available water content was set to 2,000 mm for Amazonian rainforest (Yan et al, ).…”
Section: Methodsmentioning
confidence: 99%
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“…The water stress factor EF is calculated: EF=EPETPT where PET PT is the potential evaporation (Priestley & Taylor, ) and E is actual evapotranspiration calculated from the Air Relative Humidity‐Based Two‐Source E model (Yan et al, ) that simulates the surface energy balance, soil water balance, and environmental constraints on E with inputs of remotely sensed LAI, surface meteorological data, and maximum soil available water content. Maximum soil available water content was set to 2,000 mm for Amazonian rainforest (Yan et al, ).…”
Section: Methodsmentioning
confidence: 99%
“…According to the DTEC GPP model (equation ), PAR, EF, and LAI all could contribute to the decrease in GPP of Amazon rainforests during the 2015/2016 El Niño event relative to 2011–2014. As PAR is absorbed by plant through interaction of diffuse and direct PAR with sunlit and shaded leaves, its impact on GPP depends on LAI (Yan et al, ). We assumed potential GPP (GPP*) represented contributions of PAR and LAI to GPP, GPP*=()εmsu×APARsun+εmsh×APARshd where ε msu and ε msh are maximum LUE (g C/MJ) for sunlit and shaded leaves and APAR Sun and APAR shd are incident PAR absorbed by sunlit and shaded leaves, respectively (see equations and ).…”
Section: Methodsmentioning
confidence: 99%
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