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11 IMSC Session Program<br />

Climate variability and its effect on the terrestrial biosphere<br />

Monday - Poster Session 9<br />

Lindsay Collins and Clive Anderson<br />

University of Sheffield, UK<br />

Climate change is the most important environmental issue of the 21st century, with<br />

profound societal impacts. International strategies to mitigate climate change rely on<br />

predictions on the fluxes of greenhouse gases (especially carbon dioxide) between<br />

atmosphere, oceans and the terrestrial biosphere. Of these fluxes, that between the<br />

atmosphere and vegetation and soils is the most complex and the least well quantified.<br />

A central strategy for estimating and predicting terrestrial carbon dynamics<br />

encapsulates knowledge of ecological and soil processes in a computer model, known<br />

as dynamic global vegetation model (DGVM), and uses the model to synthesise data<br />

and process understanding to predict carbon fluxes. Climate variables are major<br />

drivers of DGVMs and potentially a major source of uncertainty in derived carbon<br />

flux estimates.<br />

Here we bring together carbon modelling and statistical methods to identify the<br />

sources of uncertainty in the DGVM carbon fluxes with respect to the climate and the<br />

weather. The Sheffield Dynamic Global Vegetation Model (SDGVM) is used in this<br />

study. Dynamic linear models are used to measure the variability in the climate across<br />

the UK according to the SDGVM driving data. Bayesian sensitivity analysis is then<br />

used in the framework of Gaussian process emulation to estimate the uncertainty in<br />

the UK carbon flux estimates with respect to the climate and weather variability.<br />

Abstracts 52

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