Observational data and scale-dependent parameterizations: explorations using a virtual hydrological reality

被引:36
作者
Bashford, KE [1 ]
Beven, KJ [1 ]
Young, PC [1 ]
机构
[1] Univ Lancaster, Inst Environm & Nat Sci, Lancaster LA1 4YQ, England
关键词
data-based mechanistic; hydrological modelling; remote sensing; scale dependent;
D O I
10.1002/hyp.339
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The use of small-scale process descriptions at larger scales has been identified as a major problem in hydrological modelling. An alternative is to use measurements taken at a larger scale, such as remote sensing data, and to develop process descriptions at that scale. A hypothetical catchment area, or 'virtual hydrological reality' dataset has been generated to explore the value of different types of data in model structure and parameter identification. Though only an approximation to the natural responses of the catchment, this virtual reality can be used to explore the use of observational series that would not normally be available. A data-based mechanistic approach was used to model evapotranspiration from 1 km data, as though they were available from remote sensing. The resulting parameterization is of a similar form to an evaporative fraction model. It is an example of the type of parameterization that could be used to describe the land surface, without estimation of effective parameters from small-scale measurements, and avoiding overparameterization. Copyright (C) 2002 John Wiley Sons, Ltd.
引用
收藏
页码:293 / 312
页数:20
相关论文
共 42 条
[1]  
Allen P. B., 1991, HYDROLOGY LITTLE WAS
[2]   CONCEPTUAL ASPECTS OF A STATISTICAL-DYNAMIC APPROACH TO REPRESENT LANDSCAPE SUBGRID-SCALE HETEROGENEITIES IN ATMOSPHERIC MODELS [J].
AVISSAR, R .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D3) :2729-2742
[3]   A remote sensing surface energy balance algorithm for land (SEBAL) - 1. Formulation [J].
Bastiaanssen, WGM ;
Menenti, M ;
Feddes, RA ;
Holtslag, AAM .
JOURNAL OF HYDROLOGY, 1998, 212 (1-4) :198-212
[4]   PROPHECY, REALITY AND UNCERTAINTY IN DISTRIBUTED HYDROLOGICAL MODELING [J].
BEVEN, K .
ADVANCES IN WATER RESOURCES, 1993, 16 (01) :41-51
[5]   LINKING PARAMETERS ACROSS SCALES - SUBGRID PARAMETERIZATIONS AND SCALE-DEPENDENT HYDROLOGICAL MODELS [J].
BEVEN, K .
HYDROLOGICAL PROCESSES, 1995, 9 (5-6) :507-525
[6]  
Beven K.J., 1979, HYDROL SCI B, V24, P43, DOI [DOI 10.1080/02626667909491834, 10.1080/02626667909491834]
[7]  
BEVEN KJ, 2001, NONLINEAR NONSTATION, pCH4
[8]  
Bras R.L., 1990, HYDROLOGY INTRO HYDR
[9]   A canopy conductance and photosynthesis model for use in a GCM land surface scheme [J].
Cox, PM ;
Huntingford, C ;
Harding, RJ .
JOURNAL OF HYDROLOGY, 1998, 212 (1-4) :79-94
[10]   Comparison of the evaporative fraction and the Priestley-Taylor alpha for parameterizing daytime evaporation [J].
Crago, RD .
WATER RESOURCES RESEARCH, 1996, 32 (05) :1403-1409