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Similarity and scale in catchment storm response

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Similarity and scale in catchment storm response. / Wood, Eric F.; Sivapalan, Murugesu; Beven, Keith.
In: Reviews of Geophysics, Vol. 28, No. 1, 02.1990, p. 1-18.

Research output: Contribution to Journal/MagazineReview articlepeer-review

Harvard

Wood, EF, Sivapalan, M & Beven, K 1990, 'Similarity and scale in catchment storm response', Reviews of Geophysics, vol. 28, no. 1, pp. 1-18. https://doi.org/10.1029/RG028i001p00001

APA

Wood, E. F., Sivapalan, M., & Beven, K. (1990). Similarity and scale in catchment storm response. Reviews of Geophysics, 28(1), 1-18. https://doi.org/10.1029/RG028i001p00001

Vancouver

Wood EF, Sivapalan M, Beven K. Similarity and scale in catchment storm response. Reviews of Geophysics. 1990 Feb;28(1):1-18. doi: 10.1029/RG028i001p00001

Author

Wood, Eric F. ; Sivapalan, Murugesu ; Beven, Keith. / Similarity and scale in catchment storm response. In: Reviews of Geophysics. 1990 ; Vol. 28, No. 1. pp. 1-18.

Bibtex

@article{6dc0d81546284aadbea16712e526f8aa,
title = "Similarity and scale in catchment storm response",
abstract = "Until recently, very little progress had been made in understanding the relationship between small‐scale variability of topography, soil, and rainfalls and the storm response seen at the catchment scale. The work reviewed here represents the first attempt at a systematic theoretical framework for such understanding in the context of surface runoff generation by different processes. The parameterization of hydrological processes over a range of scales is examined, and the concept of the “representative elementary area” (REA) is introduced. The REA is a fundamental scale for catchment modeling at which continuum assumptions can be applied for the spatially variable controls and parameters, and spatial patterns no longer have to be considered explicitly. The investigation of scale leads into the concept of hydrologic similarity in which the effects of the environmental controls on runoff generation and flood frequency response be investigated independently of catchment scale. The paper reviews the authors' initial results and hopefully will motivate others to also investigate the issues of hydrologic scale and similarity.",
author = "Wood, {Eric F.} and Murugesu Sivapalan and Keith Beven",
year = "1990",
month = feb,
doi = "10.1029/RG028i001p00001",
language = "English",
volume = "28",
pages = "1--18",
journal = "Reviews of Geophysics",
issn = "8755-1209",
publisher = "American Geophysical Union",
number = "1",

}

RIS

TY - JOUR

T1 - Similarity and scale in catchment storm response

AU - Wood, Eric F.

AU - Sivapalan, Murugesu

AU - Beven, Keith

PY - 1990/2

Y1 - 1990/2

N2 - Until recently, very little progress had been made in understanding the relationship between small‐scale variability of topography, soil, and rainfalls and the storm response seen at the catchment scale. The work reviewed here represents the first attempt at a systematic theoretical framework for such understanding in the context of surface runoff generation by different processes. The parameterization of hydrological processes over a range of scales is examined, and the concept of the “representative elementary area” (REA) is introduced. The REA is a fundamental scale for catchment modeling at which continuum assumptions can be applied for the spatially variable controls and parameters, and spatial patterns no longer have to be considered explicitly. The investigation of scale leads into the concept of hydrologic similarity in which the effects of the environmental controls on runoff generation and flood frequency response be investigated independently of catchment scale. The paper reviews the authors' initial results and hopefully will motivate others to also investigate the issues of hydrologic scale and similarity.

AB - Until recently, very little progress had been made in understanding the relationship between small‐scale variability of topography, soil, and rainfalls and the storm response seen at the catchment scale. The work reviewed here represents the first attempt at a systematic theoretical framework for such understanding in the context of surface runoff generation by different processes. The parameterization of hydrological processes over a range of scales is examined, and the concept of the “representative elementary area” (REA) is introduced. The REA is a fundamental scale for catchment modeling at which continuum assumptions can be applied for the spatially variable controls and parameters, and spatial patterns no longer have to be considered explicitly. The investigation of scale leads into the concept of hydrologic similarity in which the effects of the environmental controls on runoff generation and flood frequency response be investigated independently of catchment scale. The paper reviews the authors' initial results and hopefully will motivate others to also investigate the issues of hydrologic scale and similarity.

UR - http://www.scopus.com/inward/record.url?scp=0025679827&partnerID=8YFLogxK

U2 - 10.1029/RG028i001p00001

DO - 10.1029/RG028i001p00001

M3 - Review article

AN - SCOPUS:0025679827

VL - 28

SP - 1

EP - 18

JO - Reviews of Geophysics

JF - Reviews of Geophysics

SN - 8755-1209

IS - 1

ER -