TY - JOUR
T1 - The project for intercomparison of land-surface parameterization schemes (PILPS) phase 2(c) Red-Arkansas River basin experiment
T2 - 2. Spatial and temporal analysis of energy fluxes
AU - Liang, Xu
AU - Wood, Eric F.
AU - Lettenmaier, Dennis P.
AU - Lohmann, Dag
AU - Boone, Aaron
AU - Chang, Sam
AU - Chen, Fei
AU - Dai, Yongjiu
AU - Desborough, Carl
AU - Dickinson, Robert E.
AU - Duan, Qingyun
AU - Ek, Michael
AU - Gusev, Yeugeniy M.
AU - Habets, Florence
AU - Irannejad, Parviz
AU - Koster, Randy
AU - Mitchell, Kenneth E.
AU - Nasonova, Olga N.
AU - Noilhan, Joel
AU - Schaake, John
AU - Schlosser, Adam
AU - Shao, Yaping
AU - Shmakin, Andrey B.
AU - Verseghy, Diana
AU - Warrach, Kirsten
AU - Wetzel, Peter
AU - Xue, Yongkang
AU - Yang, Zong Liang
AU - Zeng, Qing Cun
PY - 1998/12
Y1 - 1998/12
N2 - The energy components of sixteen Soil-Vegetation Atmospheric Transfer (SVAT) schemes were analyzed and intercompared using 10 years of surface meteorological and radiative forcing data from the Red-Arkansas River basin in the Southern Great Plains of the United States. Comparisons of simulated surface energy fluxes among models showed that the net radiation and surface temperature generally had the best agreement among the schemes. On an average (annual and monthly) basis, the estimated latent heat fluxes agreed (to within approximate estimation errors) with the latent heat fluxes derived from a radiosonde-based atmospheric budget method for slightly more than half of the schemes. The sensible heat fluxes had larger differences among the schemes than did the latent heat fluxes, and the model-simulated ground heat fluxes had large variations among the schemes. The spatial patterns of the model-computed net radiation and surface temperature were generally similar among the schemes, and appear reasonable and consistent with observations of related variables, such as surface air temperature. The spatial mean patterns of latent and sensible heat fluxes were less similar than for net radiation, and the spatial patterns of the ground heat flux vary greatly among the 16 schemes. Generally, there is less similarity among the models in the temporal (interannual) variability of surface fluxes and temperature than there is in the mean fields, even for schemes with similar mean fields.
AB - The energy components of sixteen Soil-Vegetation Atmospheric Transfer (SVAT) schemes were analyzed and intercompared using 10 years of surface meteorological and radiative forcing data from the Red-Arkansas River basin in the Southern Great Plains of the United States. Comparisons of simulated surface energy fluxes among models showed that the net radiation and surface temperature generally had the best agreement among the schemes. On an average (annual and monthly) basis, the estimated latent heat fluxes agreed (to within approximate estimation errors) with the latent heat fluxes derived from a radiosonde-based atmospheric budget method for slightly more than half of the schemes. The sensible heat fluxes had larger differences among the schemes than did the latent heat fluxes, and the model-simulated ground heat fluxes had large variations among the schemes. The spatial patterns of the model-computed net radiation and surface temperature were generally similar among the schemes, and appear reasonable and consistent with observations of related variables, such as surface air temperature. The spatial mean patterns of latent and sensible heat fluxes were less similar than for net radiation, and the spatial patterns of the ground heat flux vary greatly among the 16 schemes. Generally, there is less similarity among the models in the temporal (interannual) variability of surface fluxes and temperature than there is in the mean fields, even for schemes with similar mean fields.
KW - Energy balance
KW - Land-surface models
KW - PILPS
KW - Red-Arkansas River basin
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U2 - 10.1016/S0921-8181(98)00045-9
DO - 10.1016/S0921-8181(98)00045-9
M3 - Article
AN - SCOPUS:0031770980
SN - 0921-8181
VL - 19
SP - 137
EP - 159
JO - Global and Planetary Change
JF - Global and Planetary Change
IS - 1-4
ER -