Rapid surface-water volume estimations in beaver ponds

Beaver ponds are surface-water features that are transient through space and time. Such qualities complicate the inclusion of beaver ponds in local and regional water balances, and in hydrological models, as reliable estimates of surface-water storage are difficult to acquire without time- and labou...

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Main Authors: D. J. Karran, C. J. Westbrook, J. M. Wheaton, C. A. Johnston, A. Bedard-Haughn
Format: Article
Language:English
Published: Copernicus Publications 2017-02-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/21/1039/2017/hess-21-1039-2017.pdf
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spelling doaj-8e364934b7cc4c4488e764ffe152bcb52020-11-24T21:03:12ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382017-02-012121039105010.5194/hess-21-1039-2017Rapid surface-water volume estimations in beaver pondsD. J. Karran0C. J. Westbrook1J. M. Wheaton2C. A. Johnston3A. Bedard-Haughn4Department of Geography and Planning, Centre for Hydrology, University of Saskatchewan, Saskatoon, SK S7N 5C8, CanadaDepartment of Geography and Planning, Centre for Hydrology, University of Saskatchewan, Saskatoon, SK S7N 5C8, CanadaDepartment of Watershed Sciences, Utah State University, Logan, UT 84322-5210, USADepartment of Natural Resource Management, South Dakota State University, Brookings, SD 57007, USADepartment of Soil Science, University of Saskatchewan, Saskatoon, SK S7N 5A8, CanadaBeaver ponds are surface-water features that are transient through space and time. Such qualities complicate the inclusion of beaver ponds in local and regional water balances, and in hydrological models, as reliable estimates of surface-water storage are difficult to acquire without time- and labour-intensive topographic surveys. A simpler approach to overcome this challenge is needed, given the abundance of the beaver ponds in North America, Eurasia, and southern South America. We investigated whether simple morphometric characteristics derived from readily available aerial imagery or quickly measured field attributes of beaver ponds can be used to approximate surface-water storage among the range of environmental settings in which beaver ponds are found. Studied were a total of 40 beaver ponds from four different sites in North and South America. The simplified volume–area–depth (V–A–h) approach, originally developed for prairie potholes, was tested. With only two measurements of pond depth and corresponding surface area, this method estimated surface-water storage in beaver ponds within 5 % on average. Beaver pond morphometry was characterized by a median basin coefficient of 0.91, and dam length and pond surface area were strongly correlated with beaver pond storage capacity, regardless of geographic setting. These attributes provide a means for coarsely estimating surface-water storage capacity in beaver ponds. Overall, this research demonstrates that reliable estimates of surface-water storage in beaver ponds only requires simple measurements derived from aerial imagery and/or brief visits to the field. Future research efforts should be directed at incorporating these simple methods into both broader beaver-related tools and catchment-scale hydrological models.http://www.hydrol-earth-syst-sci.net/21/1039/2017/hess-21-1039-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. J. Karran
C. J. Westbrook
J. M. Wheaton
C. A. Johnston
A. Bedard-Haughn
spellingShingle D. J. Karran
C. J. Westbrook
J. M. Wheaton
C. A. Johnston
A. Bedard-Haughn
Rapid surface-water volume estimations in beaver ponds
Hydrology and Earth System Sciences
author_facet D. J. Karran
C. J. Westbrook
J. M. Wheaton
C. A. Johnston
A. Bedard-Haughn
author_sort D. J. Karran
title Rapid surface-water volume estimations in beaver ponds
title_short Rapid surface-water volume estimations in beaver ponds
title_full Rapid surface-water volume estimations in beaver ponds
title_fullStr Rapid surface-water volume estimations in beaver ponds
title_full_unstemmed Rapid surface-water volume estimations in beaver ponds
title_sort rapid surface-water volume estimations in beaver ponds
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2017-02-01
description Beaver ponds are surface-water features that are transient through space and time. Such qualities complicate the inclusion of beaver ponds in local and regional water balances, and in hydrological models, as reliable estimates of surface-water storage are difficult to acquire without time- and labour-intensive topographic surveys. A simpler approach to overcome this challenge is needed, given the abundance of the beaver ponds in North America, Eurasia, and southern South America. We investigated whether simple morphometric characteristics derived from readily available aerial imagery or quickly measured field attributes of beaver ponds can be used to approximate surface-water storage among the range of environmental settings in which beaver ponds are found. Studied were a total of 40 beaver ponds from four different sites in North and South America. The simplified volume–area–depth (V–A–h) approach, originally developed for prairie potholes, was tested. With only two measurements of pond depth and corresponding surface area, this method estimated surface-water storage in beaver ponds within 5 % on average. Beaver pond morphometry was characterized by a median basin coefficient of 0.91, and dam length and pond surface area were strongly correlated with beaver pond storage capacity, regardless of geographic setting. These attributes provide a means for coarsely estimating surface-water storage capacity in beaver ponds. Overall, this research demonstrates that reliable estimates of surface-water storage in beaver ponds only requires simple measurements derived from aerial imagery and/or brief visits to the field. Future research efforts should be directed at incorporating these simple methods into both broader beaver-related tools and catchment-scale hydrological models.
url http://www.hydrol-earth-syst-sci.net/21/1039/2017/hess-21-1039-2017.pdf
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