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Three-dimensional modelling of hillslope hydrology.

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Three-dimensional modelling of hillslope hydrology. / Binley, Andrew M.; Beven, Keith J.
In: Hydrological Processes, Vol. 6, No. 3, 1992, p. 347-359.

Research output: Contribution to Journal/Magazine › Journal article

Harvard

Binley, AM & Beven, KJ 1992, 'Three-dimensional modelling of hillslope hydrology.', Hydrological Processes, vol. 6, no. 3, pp. 347-359. https://doi.org/10.1002/hyp.3360060308

APA

Binley, A. M., & Beven, K. J. (1992). Three-dimensional modelling of hillslope hydrology. Hydrological Processes, 6(3), 347-359. https://doi.org/10.1002/hyp.3360060308

Vancouver

Binley AM, Beven KJ. Three-dimensional modelling of hillslope hydrology. Hydrological Processes. 1992;6(3):347-359. doi: 10.1002/hyp.3360060308

Author

Binley, Andrew M. ; Beven, Keith J. / Three-dimensional modelling of hillslope hydrology. In: Hydrological Processes. 1992 ; Vol. 6, No. 3. pp. 347-359.

Bibtex

@article{9b7e9757a2554b08a76d5bfea3d93839,
title = "Three-dimensional modelling of hillslope hydrology.",
abstract = "Physically-based models of catchment hydrology are computationally demanding. the cost of even small scale simulations of multidimensional subsurface flow problems is often considered too high and yet May, be important if one is to appreciate the complex flow pathways in heterogeneous catchments. This is likely to be the case for problems concerned with transport of chemical substances in soils, in particular those with some localized origin. Recent advances in computer hardware technology and numerical algorithms are beginning to make detailed simulations more feasible. We discuss here issues relating to using these new tools in modelling hillslope flow processes and document an example three-dimensional simulation of a heterogeneous Darcian headwater.",
keywords = "Distributed models • Finite element • Parallel computers",
author = "Binley, {Andrew M.} and Beven, {Keith J.}",
year = "1992",
doi = "10.1002/hyp.3360060308",
language = "English",
volume = "6",
pages = "347--359",
journal = "Hydrological Processes",
issn = "1099-1085",
publisher = "John Wiley and Sons Ltd",
number = "3",

}

RIS

TY - JOUR

T1 - Three-dimensional modelling of hillslope hydrology.

AU - Binley, Andrew M.

AU - Beven, Keith J.

PY - 1992

Y1 - 1992

N2 - Physically-based models of catchment hydrology are computationally demanding. the cost of even small scale simulations of multidimensional subsurface flow problems is often considered too high and yet May, be important if one is to appreciate the complex flow pathways in heterogeneous catchments. This is likely to be the case for problems concerned with transport of chemical substances in soils, in particular those with some localized origin. Recent advances in computer hardware technology and numerical algorithms are beginning to make detailed simulations more feasible. We discuss here issues relating to using these new tools in modelling hillslope flow processes and document an example three-dimensional simulation of a heterogeneous Darcian headwater.

AB - Physically-based models of catchment hydrology are computationally demanding. the cost of even small scale simulations of multidimensional subsurface flow problems is often considered too high and yet May, be important if one is to appreciate the complex flow pathways in heterogeneous catchments. This is likely to be the case for problems concerned with transport of chemical substances in soils, in particular those with some localized origin. Recent advances in computer hardware technology and numerical algorithms are beginning to make detailed simulations more feasible. We discuss here issues relating to using these new tools in modelling hillslope flow processes and document an example three-dimensional simulation of a heterogeneous Darcian headwater.

KW - Distributed models • Finite element • Parallel computers

U2 - 10.1002/hyp.3360060308

DO - 10.1002/hyp.3360060308

M3 - Journal article

VL - 6

SP - 347

EP - 359

JO - Hydrological Processes

JF - Hydrological Processes

SN - 1099-1085

IS - 3

ER -