Modelling gross primary production of a tropical semi-deciduous forest in the southern Amazon Basin
2014
Biudes, Marcelo Sacardi | Souza, Maísa Caldas | Machado, Nadja Gomes | de Morais Danelichen, Victor Hugo | Vourlitis, George Louis | de Souza Nogueira, José
Semi-deciduous forest in the Amazon Basin is sensitive to temporal variation in surface water availability that can limit seasonal rates of leaf and canopy gas exchange. We estimated the seasonal dynamics of gross primary production (GPP) over 3 years (2005–2008) using eddy covariance and assessed canopy spectral reflectance using MODIS imagery for a mature tropical semi-deciduous forest located near Sinop, Mato Grosso, Brazil. A light-use efficiency model, known as the Vegetation Photosynthesis Model (VPM), was used to estimate seasonal and inter-annual variations in GPP as a function of the enhanced vegetation index (EVI), the land surface water index (LSWI), and local meteorology. Our results indicate that the standard VPM was incapable of reproducing the seasonal variation in GPP, primarily because the model overestimated dry-season GPP. In the standard model, the scalar function that alters light-use efficiency (ε g) as a function of water availability (W ₛcₐₗₐᵣ) is calculated as a linear function of the LSWI derived from MODIS; however, the LSWI is negatively correlated with several measures of water availability including precipitation, soil water content, and relative humidity (RH). Thus, during the dry season, when rainfall, soil water content, and RH are low, LSWI, and therefore, W ₛcₐₗₐᵣ, are at a seasonal maximum. Using previous research, we derived new functions for W ₛcₐₗₐᵣ based on time series of RH and photosynthetic photon flux density (PPFD) that significantly improved the performance of the VPM. Whether these new functions perform equally well in water stressed and unstressed tropical forests needs to be determined, but presumably unstressed ecosystems would have high cloud cover and humidity, which would minimize variations in W ₛcₐₗₐᵣ and GPP to spatial and/or temporal variation in water availability.
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