Testing simulations of intra‐ and inter‐annual variation in the plant production response to elevated CO2 against measurements from an 11‐year FACE experiment on grazed pasture. (17th November 2013)

• Record Type: Journal Article
• Authors: Li, Frank Yonghong; Newton, Paul C. D.; Lieffering, Mark
• Is Part Of: Global change biology. Volume 20:Number 1(2014:Jan.)
• Page Start: 228
• Page End: 239
• Publication Date: 2013-11-17
• Subjects: Climatic changes -- Environmental aspects -- Periodicals; Troposphere -- Environmental aspects -- Periodicals; Biodiversity conservation -- Periodicals; Eutrophication -- Periodicals; 551.5
• DOI: 10.1111/gcb.12358
• Languages: English
• ISSNs: 1354-1013

Abstract

<abstract abstract-type="main" id="gcb12358-abs-0001"> <title>Abstract</title> <p>Ecosystem models play a crucial role in understanding and evaluating the combined impacts of rising atmospheric CO<sub>2</sub> concentration and changing climate on terrestrial ecosystems. However, we are not aware of any studies where the capacity of models to simulate intra‐ and inter‐annual variation in responses to elevated CO<sub>2</sub> has been tested against long‐term experimental data. Here we tested how well the ecosystem model APSIM/AgPasture was able to simulate the results from a free air carbon dioxide enrichment (FACE) experiment on grazed pasture. At this FACE site, during 11 years of CO<sub>2</sub> enrichment, a wide range in annual plant production response to CO<sub>2</sub> (−6 to +28%) was observed. As well as running the full model, which includes three plant CO<sub>2</sub> response functions (plant photosynthesis, nitrogen (N) demand and stomatal conductance), we also tested the influence of these three functions on model predictions. Model/data comparisons showed that: (i) overall the model over‐predicted the mean annual plant production response to CO<sub>2</sub> (18.5% cf 13.1%) largely because years with small or negative responses to CO<sub>2</sub> were not well simulated; (ii) in general seasonal and inter‐annual variation in plant production responses to elevated CO<sub>2</sub> were well represented by the model; (iii) the observed CO<sub>2</sub> enhancement in overall mean legume content was well simulated but year‐to‐year variation in legume content was poorly captured by the model; (iv) the best fit of the model to the data required all three CO<sub>2</sub> response functions to be invoked; (v) using actual legume content and reduced N fixation rate under elevated CO<sub>2</sub> in the model provided the best fit to the experimental data. We conclude that in temperate grasslands the N dynamics (particularly the legume content and N fixation activity) play a critical role in pasture production responses to elevated CO<sub>2</sub>, and are processes for model improvement.</p> </abstract>