2005
DOI: 10.1111/j.1365-2486.2005.01048.x
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Constraining the Sheffield dynamic global vegetation model using stream‐flow measurements in the United Kingdom

Abstract: The biospheric water and carbon cycles are intimately coupled, so simulating carbon fluxes by vegetation also requires modelling of the water fluxes, with each component influencing the other. Observations of river streamflow integrate information at the catchment scale and are widely available over a long period; they therefore provide an important source of information for validating or calibrating vegetation models. In this paper, we analyse the performance of the Sheffield dynamic global vegetation model (… Show more

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Cited by 5 publications
(5 citation statements)
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“…The SDGVM was developed as a daily timestep, global biogeography and eco-physiology model Woodward & Lomas, 2004) to predict the primary biomes of Earth and their associated fluxes of C and water in response to global change. SDGVM has been described and extensively evaluated at site and global scales Cramer et al, 2001;Woodward & Lomas, 2004;Picard et al, 2005;Sitch et al, 2008;Beer et al, 2010;De Kauwe et al, 2013Friend et al, 2014;Walker et al, 2014b;Zaehle et al, 2014), so here we provide a brief description of the model and the process simulation methods relevant to this paper.…”
Section: Descriptionmentioning
confidence: 99%
“…The SDGVM was developed as a daily timestep, global biogeography and eco-physiology model Woodward & Lomas, 2004) to predict the primary biomes of Earth and their associated fluxes of C and water in response to global change. SDGVM has been described and extensively evaluated at site and global scales Cramer et al, 2001;Woodward & Lomas, 2004;Picard et al, 2005;Sitch et al, 2008;Beer et al, 2010;De Kauwe et al, 2013Friend et al, 2014;Walker et al, 2014b;Zaehle et al, 2014), so here we provide a brief description of the model and the process simulation methods relevant to this paper.…”
Section: Descriptionmentioning
confidence: 99%
“…However, such low spatial resolution data, for which each pixel may be made up of several land cover types, might be of limited utility for semi-arid forested areas that are mostly sparse and heterogeneous (Sprintsin et al 2007), therefore requiring detailed and careful validation by regionor site-specific measurements. LAI is a key parameter in land process models, terrestrial carbon modelling, dynamic vegetation models, large-scale carbon budgets and large scale climate models (Prince et al 2001, Picard et al 2005. Due to its central role in the dissipation of radiant energy input its erroneous assessment will affect the results of the models implemented.…”
Section: Introductionmentioning
confidence: 99%
“…A critical property of the emulator is that its execution is much faster than running the full model, and for this reason they have been widely used in statistics [18][19][20][21]. We focus our attention in Gaussian process (GP) emulators, which have been widely used in a number of fields (e.g., the climate and vegetation modelling communities have used emulators for some time [22][23][24][25]). In Earth Observation, GPs have been used as fast surrogates to computationally expensive models in [26] for sensitivity analysis.…”
Section: Introductionmentioning
confidence: 99%