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  Improving canopy processes in the Community Land Model version 4 (CLM4) using global flux fields empirically inferred from FLUXNET data

Bonan, G. B., Lawrence, P. J., Oleson, K. W., Levis, S., Jung, M., Reichstein, M., et al. (2011). Improving canopy processes in the Community Land Model version 4 (CLM4) using global flux fields empirically inferred from FLUXNET data. Journal of Geophysical Research - Biogeosciences, 116, G02014. doi:10.1029/2010jg001593.

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 Creators:
Bonan, G. B., Author
Lawrence, P. J., Author
Oleson, K. W., Author
Levis, S., Author
Jung, M.1, Author           
Reichstein, M.1, Author           
Lawrence, D. M., Author
Swenson, S. C., Author
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1Research Group Biogeochemical Model-data Integration, Dr. M. Reichstein, Max Planck Institute for Biogeochemistry, Max Planck Society, ou_1497760              

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Free keywords: temperature response functions surface parameterization sib2 stomatal conductance model leaf nitrogen distribution gross primary production net ecosystem exchange photosynthetic capacity deciduous forest limited photosynthesis integration scheme
 Abstract: The Community Land Model version 4 (CLM4) overestimates gross primary production (GPP) compared with data-driven estimates and other process models. We use global, spatially gridded GPP and latent heat flux upscaled from the FLUXNET network of eddy covariance towers to evaluate and improve canopy processes in CLM4. We investigate differences in GPP and latent heat flux arising from model parameterizations (termed model structural error) and from uncertainty in the photosynthetic parameter V-c max (termed model parameter uncertainty). Model structural errors entail radiative transfer, leaf photosynthesis and stomatal conductance, and canopy scaling of leaf processes. Model structural revisions reduce global GPP over the period 1982-2004 from 165 Pg C yr(-1) to 130 Pg C yr(-1), and global evapotranspiration decreases from 68,000 km(3) yr(-1) to 65,000 km(3) yr(-1), within the uncertainty of FLUXNET-based estimates. Colimitation of photosynthesis is a cause of the improvements, as are revisions to photosynthetic parameters and their temperature dependency. Improvements are seen in all regions and seasonally over the course of the year. Similar improvements occur in latent heat flux. Uncertainty in V-c max produces effects of comparable magnitude as model structural errors, but of offsetting sign. This suggests that model structural errors can be compensated by parameter adjustment, and this may explain the lack of consensus in values for V-c max used in terrestrial biosphere models. Our analyses show that despite inherent uncertainties global flux fields empirically inferred from FLUXNET data are a valuable tool to guide terrestrial biosphere model development and evaluation.

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Language(s): eng - English
 Dates: 2011
 Publication Status: Issued
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 Identifiers: DOI: 10.1029/2010jg001593
ISI: ://000290933300002
Other: BGC1509
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Title: Journal of Geophysical Research - Biogeosciences
Source Genre: Journal
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Pages: - Volume / Issue: 116 Sequence Number: - Start / End Page: G02014 Identifier: ISSN: 0148-0227