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The Project for Intercomparison of Land-surface Parameterization Schemes (PILPS) phase 2(c) Red–Arkansas River basin experiment:

Identifieur interne : 00C869 ( Main/Exploration ); précédent : 00C868; suivant : 00C870

The Project for Intercomparison of Land-surface Parameterization Schemes (PILPS) phase 2(c) Red–Arkansas River basin experiment:

Auteurs : Dag Lohmann [États-Unis] ; Dennis P. Lettenmaier [États-Unis] ; Xu Liang [États-Unis] ; Eric F. Wood [États-Unis] ; Aaron Boone [États-Unis] ; Sam Chang [États-Unis] ; Fei Chen [États-Unis] ; Yongjiu Dai [République populaire de Chine] ; Carl Desborough [Australie] ; Robert E. Dickinson [États-Unis] ; Qingyun Duan [États-Unis] ; Michael Ek [États-Unis] ; Yeugeniy M. Gusev [Russie] ; Florence Habets [France] ; Parviz Irannejad [Australie] ; Randy Koster [États-Unis] ; Kenneth E. Mitchell [États-Unis] ; Olga N. Nasonova [Russie] ; Joel Noilhan [France] ; John Schaake [États-Unis] ; Adam Schlosser [États-Unis] ; Yaping Shao [Australie] ; Andrey B. Shmakin [Russie] ; Diana Verseghy [Canada] ; Kirsten Warrach [Allemagne] ; Peter Wetzel [États-Unis] ; Yongkang Xue [États-Unis] ; Zong-Liang Yang [États-Unis] ; Qing-Cun Zeng [République populaire de Chine]

Source :

RBID : ISTEX:206B1F9B68C7C8001D235FEA2864B16A98F36E61

Descripteurs français

English descriptors

Abstract

Abstract: The water-balance components of 16 Soil–Vegetation Atmospheric Transfer (SVAT) schemes were evaluated by comparing predicted and observed streamflow, predicted evapotranspiration and evapotranspiration inferred from an atmospheric moisture budget analysis, and soil moisture storage changes for a seven-year period (1980–1986) using data from the Red–Arkansas River basins of the Southern Great Plains of the USA. The evaluations support the following suggestions: (a) The mean annual runoff of all models follows, at least generally, the strong climatic East–West gradient of precipitation, although most models predict too much runoff in the dry part of the basin. (b) The mean monthly storage change tends to be underestimated, even though all models capture reasonably well the seasonality of the evapotranspiration. (c) The wide range of conceptualizations used for generation of surface and subsurface runoff strongly affect runoff generation on seasonal, and shorter, time scales. Model responses to summer precipitation ranged from almost no summer runoff (one model) to the (more common) situation of persistent overprediction of summer runoff, especially in the driest part of the basin. (d) All models tended to underpredict evapotranspiration in summer and overpredict in winter. (e) Model-derived mean seasonal cycles of changes in soil moisture storage are qualitatively similar to those inferred from observations, but most models do not predict the decrease in April soil moisture storage and the increase in October that is inferred from observations.

Url:
DOI: 10.1016/S0921-8181(98)00046-0


Affiliations:


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<term>Academic press</term>
<term>Alsis</term>
<term>Annual precipitation</term>
<term>Annual runoff</term>
<term>Annual runoff ratio</term>
<term>Arkansas river</term>
<term>Arkansas river basin</term>
<term>Atmospheric budget</term>
<term>Atmospheric budget calculation</term>
<term>Atmospheric moisture budget analysis</term>
<term>Atmospheric physics</term>
<term>Atmospheric water balance</term>
<term>Baseflow</term>
<term>Basin</term>
<term>Basin area</term>
<term>Basin boundary</term>
<term>Basin outlet</term>
<term>Buck model</term>
<term>Budget analysis</term>
<term>Canopy storage</term>
<term>Catchment</term>
<term>Civil engineering</term>
<term>Climatology</term>
<term>Different models</term>
<term>Different sets</term>
<term>Drainage areas</term>
<term>Eastern part</term>
<term>Effective precipitation</term>
<term>Elsevier science</term>
<term>Evapotranspiration</term>
<term>Excess water</term>
<term>Free drainage</term>
<term>Global</term>
<term>Grid</term>
<term>Grid cell</term>
<term>Grid cells</term>
<term>Higher fractions</term>
<term>Hydrologic literature</term>
<term>Infiltration capacity</term>
<term>Intercomparison</term>
<term>Isba</term>
<term>Isba mosaic ncep place sewab sponsor ssib swap</term>
<term>July</term>
<term>Land surface</term>
<term>Land surface schemes</term>
<term>Latent heat</term>
<term>Less runoff</term>
<term>Liang</term>
<term>Little rock</term>
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<term>Mmryr</term>
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<term>Model results</term>
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<term>Ncep</term>
<term>Negative storage change</term>
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<term>Operations research</term>
<term>Other schemes</term>
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<term>Parameterization</term>
<term>Parameterization schemes</term>
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<term>Pilps</term>
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<term>Pilps phase activities</term>
<term>Pilps phase schemes</term>
<term>Planetary change</term>
<term>Precipitation</term>
<term>Princeton university</term>
<term>Reasonable results</term>
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<term>Runoff climatology</term>
<term>Runoff production</term>
<term>Runoff ratio</term>
<term>Runoff ratios</term>
<term>Runoff timing</term>
<term>Russian federation</term>
<term>Schemes underpredicted</term>
<term>Seasonal cycle</term>
<term>Seasonal cycles</term>
<term>Sewab</term>
<term>Slow components</term>
<term>Small storage changes</term>
<term>Soil column</term>
<term>Soil moisture</term>
<term>Soil moisture storage changes</term>
<term>Soil water</term>
<term>Spatial pattern</term>
<term>Spatial patterns</term>
<term>Spatial runoff distribution</term>
<term>Spatial variability</term>
<term>Ssib</term>
<term>Storage change</term>
<term>Streamflow</term>
<term>Streamflow data</term>
<term>Subsurface</term>
<term>Subsurface runoff</term>
<term>Summary intercomparisons</term>
<term>Summer period</term>
<term>Summer runoff</term>
<term>Surface runoff</term>
<term>Surface water balance</term>
<term>Swap</term>
<term>Technical report</term>
<term>Temporal analysis</term>
<term>Threshold behavior</term>
<term>Time invariance</term>
<term>Time scales</term>
<term>Total runoff</term>
<term>Unit hydrograph</term>
<term>Upper soil layer</term>
<term>Various terms</term>
<term>Water balance</term>
<term>Water balances</term>
<term>Water budget</term>
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<term>Wide range</term>
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<term>Academic press</term>
<term>Alsis</term>
<term>Annual precipitation</term>
<term>Annual runoff</term>
<term>Annual runoff ratio</term>
<term>Arkansas river</term>
<term>Arkansas river basin</term>
<term>Atmospheric budget</term>
<term>Atmospheric budget calculation</term>
<term>Atmospheric moisture budget analysis</term>
<term>Atmospheric physics</term>
<term>Atmospheric water balance</term>
<term>Baseflow</term>
<term>Basin</term>
<term>Basin area</term>
<term>Basin boundary</term>
<term>Basin outlet</term>
<term>Buck model</term>
<term>Budget analysis</term>
<term>Canopy storage</term>
<term>Catchment</term>
<term>Civil engineering</term>
<term>Climatology</term>
<term>Different models</term>
<term>Different sets</term>
<term>Drainage areas</term>
<term>Eastern part</term>
<term>Effective precipitation</term>
<term>Elsevier science</term>
<term>Evapotranspiration</term>
<term>Excess water</term>
<term>Free drainage</term>
<term>Global</term>
<term>Grid</term>
<term>Grid cell</term>
<term>Grid cells</term>
<term>Higher fractions</term>
<term>Hydrologic literature</term>
<term>Infiltration capacity</term>
<term>Intercomparison</term>
<term>Isba</term>
<term>Isba mosaic ncep place sewab sponsor ssib swap</term>
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<term>Land surface schemes</term>
<term>Latent heat</term>
<term>Less runoff</term>
<term>Liang</term>
<term>Little rock</term>
<term>Lohmann</term>
<term>Mmryr</term>
<term>Model output</term>
<term>Model results</term>
<term>Model simulations</term>
<term>Moisture fluxes</term>
<term>Monthly basin evapotranspiration</term>
<term>Monthly evapotranspiration</term>
<term>Much runoff</term>
<term>Nasar gsfc</term>
<term>Ncep</term>
<term>Negative storage change</term>
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<term>Operations research</term>
<term>Other schemes</term>
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<term>Runoff production</term>
<term>Runoff ratio</term>
<term>Runoff ratios</term>
<term>Runoff timing</term>
<term>Russian federation</term>
<term>Schemes underpredicted</term>
<term>Seasonal cycle</term>
<term>Seasonal cycles</term>
<term>Sewab</term>
<term>Slow components</term>
<term>Small storage changes</term>
<term>Soil column</term>
<term>Soil moisture</term>
<term>Soil moisture storage changes</term>
<term>Soil water</term>
<term>Spatial pattern</term>
<term>Spatial patterns</term>
<term>Spatial runoff distribution</term>
<term>Spatial variability</term>
<term>Ssib</term>
<term>Storage change</term>
<term>Streamflow</term>
<term>Streamflow data</term>
<term>Subsurface</term>
<term>Subsurface runoff</term>
<term>Summary intercomparisons</term>
<term>Summer period</term>
<term>Summer runoff</term>
<term>Surface runoff</term>
<term>Surface water balance</term>
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<term>Technical report</term>
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<term>Time invariance</term>
<term>Time scales</term>
<term>Total runoff</term>
<term>Unit hydrograph</term>
<term>Upper soil layer</term>
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<term>Water balances</term>
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<term>Génie civil</term>
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<front>
<div type="abstract" xml:lang="en">Abstract: The water-balance components of 16 Soil–Vegetation Atmospheric Transfer (SVAT) schemes were evaluated by comparing predicted and observed streamflow, predicted evapotranspiration and evapotranspiration inferred from an atmospheric moisture budget analysis, and soil moisture storage changes for a seven-year period (1980–1986) using data from the Red–Arkansas River basins of the Southern Great Plains of the USA. The evaluations support the following suggestions: (a) The mean annual runoff of all models follows, at least generally, the strong climatic East–West gradient of precipitation, although most models predict too much runoff in the dry part of the basin. (b) The mean monthly storage change tends to be underestimated, even though all models capture reasonably well the seasonality of the evapotranspiration. (c) The wide range of conceptualizations used for generation of surface and subsurface runoff strongly affect runoff generation on seasonal, and shorter, time scales. Model responses to summer precipitation ranged from almost no summer runoff (one model) to the (more common) situation of persistent overprediction of summer runoff, especially in the driest part of the basin. (d) All models tended to underpredict evapotranspiration in summer and overpredict in winter. (e) Model-derived mean seasonal cycles of changes in soil moisture storage are qualitatively similar to those inferred from observations, but most models do not predict the decrease in April soil moisture storage and the increase in October that is inferred from observations.</div>
</front>
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<li>Allemagne</li>
<li>Australie</li>
<li>Canada</li>
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<li>Russie</li>
<li>République populaire de Chine</li>
<li>États-Unis</li>
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<li>District fédéral central</li>
<li>Maryland</li>
<li>Massachusetts</li>
<li>Midi-Pyrénées</li>
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<li>Washington (État)</li>
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<li>Université de Washington</li>
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