Title: Ecohydrological Responses of Dense Canopies to Environmental Variability Part 2: Role of Acclimation Under Elevated CO2 Authors
|Drewry, Darren -|
|Kumar, Praveen -|
|Long, Stephen -|
|Liang, Xin-Zhong -|
|Sivapalan, Murugesu -|
Submitted to: Journal of Geophysical Research-Biogeosciences
Publication Type: Peer Reviewed Journal
Publication Acceptance Date: July 19, 2010
Publication Date: November 11, 2010
Repository URL: http://hdl.handle.net/10113/48763
Citation: Drewry, D.T., Kumar, P., Long, S., Bernacchi, C.J., Liang, X., Sivapalan, M. 2010. Ecohydrological responses of dense canopies to environmental variability Part 2: Role of acclimation under elevated CO2. Journal of Geophysical Research-Biogeosciences. doi:10.1029/2010JG001341. Interpretive Summary: This paper is the second of a two-part submission. The first paper, entitled “Ecohydrological Responses of Dense Canopies to Environmental Variability, Part 1: Interplay Between Vertical Structure and Photosynthetic Pathway”, developed and validated a plant canopy model to improve predictive ability of models to represent the dynamics that occur within a plant canopy. This second paper shows how the model is able to predict the responses of plants, namely corn and soybean, to future atmospheric conditions. The strength of the new plant canopy model, MLCan, is that it is highly mechanistic and slight changes in underlying plant metabolism are easily integrated into the model. In this paper, data from the Soybean Free Air CO2 Enrichment (SoyFACE) experiment is used first to parameterize the model based on measured relationships of plant physiology to rising CO2. The model is then compared with measurements from SoyFACE that represent the canopy-atmosphere interactions. The model is shown to faithfully mimic the observations for both maize and soybean over numerous years. This second paper validates MLCan for a wide range of conditions and provides an improved understanding of the physiological factors that lead to canopy-scale changes when plants are grown in elevated CO2. This paper, coupled with the first part, will help improve understanding of how corn and soybean respond to current and future environmental changes.
Technical Abstract: The ability to accurately predict land-atmosphere exchange of mass, energy, and momentum over the coming century requires the consideration of plant biochemical, ecophysiological and structural acclimation to modifications of the ambient environment. Amongst the most important environmental changes experienced by terrestrial vegetation over the last century has been the increase in ambient carbon dioxide (CO2) concentrations, with a projected doubling in CO2 from pre-industrial levels by the middle of this century. This change in atmospheric composition has been demonstrated to significantly alter a variety of leaf and plant properties across a range of species, with the potential to modify land-atmosphere interactions and their associated feedbacks. Free Air Carbon Enrichment (FACE) technology has provided significant insight into the functioning of vegetation in natural conditions under elevated CO2, but remains limited in its ability to quantify the exchange of CO2, water vapor and energy at the canopy scale. This paper addresses the roles of ecophysiological, biochemical and structural plant acclimation on canopy-scale exchange of CO2, water vapor and energy through the application of a multi-layer canopy-root-soil model (MLCan) capable of resolving changes induced by elevated CO2 through the canopy and soil systems. Previous validation of MLCan flux estimates were made for soybean and maize in the companion paper using a record of six growing seasons of eddy covariance data from the Bondville Ameriflux site. Observations of leaf-level photosynthesis, stomatal conductance and surface temperature collected at the SoyFACE experimental facility in central Illinois provide a basis for examining the ability of MLCan to capture vegetative responses to an enriched CO2 environment. Simulations of control (370 [ppm]) and elevated (550 [ppm]) CO2 environments allow for an examination of the vertical variation and canopy-scale responses of vegetation states and fluxes to elevated CO2. The unique metabolic pathways of the C3 soybean and C4 maize produce contrasting modes of response to elevated CO2 for each crop. To examine the relative roles of direct reduction in stomatal aperature, observed structural augmentation of leaf area, and biochemical down-regulation of Rubisco carboxylation capacity in soybean, a set of simulations were conducted in which one or more of these 2 acclimations are synthetically removed. A 10% increase in canopy leaf area is shown to offset the ecophysiologically driven reduction in latent energy flux by 40% on average at mid-day. Considering all observed acclimations for soybean, average mid-day LE (H) were decreased (increased) by 10.5 (18) [W m*2]. A lack of direct stimulation of photosynthesis for maize, and no observed structural or biochemical acclimation resulted in decreases (increases) in average mid-day LE (H) by 40-50 [W m*2]. An examination of canopy-scale responses at a range of CO2 concentrations projected to be seen over the coming century showed a general continuation in the direction of flux responses. Flux responses showed little sensitivity to assumptions of constant versus linear trends in structural and biochemical acclimation magnitudes over the 400 to 700 [ppm] concentration range examined here.