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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 113,
D09111,
doi:10.1029/2007JD009246,
2008
Integration of the variable infiltration capacity model soil hydrology scheme into the community land model
Aihui Wang
Department of Civil and Environmental Engineering, University of Washington, Seattle, Washington, USA
Kaiyuan Y. Li
Department of Civil and Environmental Engineering, University of Washington, Seattle, Washington, USA
Dennis P. Lettenmaier
Department of Civil and Environmental Engineering, University of Washington, Seattle, Washington, USA
Abstract
Enhancements to the soil hydrology scheme in the NCAR Community Land Model version 3 (CLM3) are described, which are intended
to improve the ability of CLM to represent land surface hydrologic processes. Specifically, the CLM3 soil hydrology scheme
has been replaced with the scheme used in the Variable Infiltration Capacity model (VIC). While the modified model incorporates
VIC soil hydrology, the original model structure in CLM3 is unchanged in most other respects, such as the representation of
vegetation and its controls on surface energy exchanges. The modified version of CLM3 makes direct use of VIC soil parameters
that have been developed for off-line regional, continental, and global simulations. The performance of the new model and
CLM3 are evaluated through a comparison with observations at three flux tower sites: ABRACOS, a pasture clearing in the Brazilian
rain forest, HAPEX-MOBILHY, a midlatitude agricultural site in France, and Valdai, a midlatitude grassland in Russia, as well
as two large river basins (Arkansas-Red and Colorado in the United States). Overall, the results show that the merged model
better reproduces observed soil hydrological variability, in particular, the seasonal evolution and amplitude of soil moisture,
as compared to CLM3. The river basin simulations show that in the merged model, total runoff is generally less than in CLM3
and better agrees with observations. Owing to the interaction of runoff and soil moisture, the simulation of total evapotranspiration
(or latent heat) is also improved in the merged model.
Received 2
August
2007;
accepted 13
February
2008;
published 10
May
2008.
Keywords: soil hydrology;
variable infiltration capacity model;
community land model.
Index Terms: 1860 Hydrology: Streamflow; 1866 Hydrology: Soil moisture; 1818 Hydrology: Evapotranspiration; 1847 Hydrology: Modeling; 1863 Hydrology: Snow and ice (0736, 0738, 0776, 1827).
Subscriber Access to Full Article (Nonsubscribers may purchase for $9.00, Includes print PDF, file size: 7994917 bytes)
Citation: Wang, A., K. Y. Li, and D. P. Lettenmaier
(2008),
Integration of the variable infiltration capacity model soil hydrology scheme into the community land model,
J. Geophys. Res.,
113,
D09111,
doi:10.1029/2007JD009246.
Copyright 2008 by the American Geophysical Union.
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