LINKING PARAMETERS ACROSS SCALES - SUBGRID PARAMETERIZATIONS AND SCALE-DEPENDENT HYDROLOGICAL MODELS

被引:171
作者
BEVEN, K
机构
[1] Centre for Research on Environmental Systems and Statistics, Institute of Environmental and Biological Sciences, Lancaster University, Lancaster
关键词
SUBGRID PARAMETERIZATION; SCALE; DISAGGREGATION; DISTRIBUTION FUNCTIONS; SVAT; TOPMODEL; UNCERTAINTY; MACROSCALE MODELS;
D O I
10.1002/hyp.3360090504
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
It is argued that the aggregation approach towards macroscale hydrological modelling, in which it is assumed that a model applicable at small scales can be applied at larger scales using 'effective' parameter values, is an inadequate approach to the scale problem. It is also unlikely that any general scaling theory can be developed due to the dependence of hydrological systems on historical and geological perturbations. Thus a disaggregation approach to developing scale-dependent models is advocated in which a representation of the distribution of hydrological responses is used to reflect hydrological heterogeneity. An appropriate form of distribution may vary with both scale and environment. Such an approach is dependent on the data available to define and calibrate the chosen subgrid parameterization. A parameterization based on a minimum patch representation is suggested and the problems of identification at the larger scale discussed.
引用
收藏
页码:507 / 525
页数:19
相关论文
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  • [1] Avissar R., A statistical‐dynamical approach to parameterise subgrid‐scale land surface heterogeneity in climate models, Land Surface‐Atmospheric Interactions for Climate Modeling, pp. 155-178, (1991)
  • [2] Avissar R., Conceptual aspects of a statistical‐dynamic approach to represent landscape subgrid scale heterogeneities in atmospheric models, J. Geophys. Res., 97, 3 D, pp. 2729-2742, (1992)
  • [3] Barling R.D., Moore I.D., Grayson R.B., A quasi‐dynamic wetness index for characterising the spatial distribution of zones of surface saturation and soil water content, Wat. Resour. Res., 30, pp. 1029-1044, (1994)
  • [4] Beven K.J., Changing ideas in hydrology: the case of physically‐based models, J. Hydrol., 105, pp. 157-172, (1989)
  • [5] Beven K.J., Interflow, Unsaturated Flow in Hydrologic Modelling, Proc. NATO ARW, Arles, pp. 191-219, (1989)
  • [6] Beven K.J., Prophecy, reality and uncertainty in distributed hydrological modelling, Adv. Wat. Resour., 16, pp. 41-51, (1993)
  • [7] Beven K.J., Process, heterogeneity and scale in modelling soil moisture fluxes, Global Environmental Change and Land Surface Process in Hydrology: The Trials and Tribulations of Modelling and Measuring. Proc. NATO ARW. Tucson, Arizona, (1994)
  • [8] Beven K., Binley A.M., The future of distributed models: model calibration and uncertainty prediction, Hydrol. Process., 6, pp. 279-298, (1992)
  • [9] Beven K.J., Germann P., Macropores and water flow in soils, Wat. Resour. Res., 18, pp. 1311-1325, (1982)
  • [10] Beven K.J., Kirkby M.J., A physically based variable contributing area model of basin hydrology, Hydrol. Sci. Bull., 24, pp. 43-69, (1979)