Articles | Volume 19, issue 8
https://doi.org/10.5194/hess-19-3541-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/hess-19-3541-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
11 Aug 2015
Research article |
| 11 Aug 2015
Impacts of beaver dams on hydrologic and temperature regimes in a mountain stream
M. Majerova
CORRESPONDING AUTHOR
Utah Water Research Laboratory, Department of Civil and Environmental Engineering, Utah State University, 8200 Old Main Hill, Logan, Utah, 84322-8200, USA
B. T. Neilson
CORRESPONDING AUTHOR
Utah Water Research Laboratory, Department of Civil and Environmental Engineering, Utah State University, 8200 Old Main Hill, Logan, Utah, 84322-8200, USA
N. M. Schmadel
Utah Water Research Laboratory, Department of Civil and Environmental Engineering, Utah State University, 8200 Old Main Hill, Logan, Utah, 84322-8200, USA
J. M. Wheaton
Department of Watershed Sciences, Utah State University, 8200 Old Main Hill, Logan, Utah 84322-8200, USA
C. J. Snow
Utah Water Research Laboratory, Department of Civil and Environmental Engineering, Utah State University, 8200 Old Main Hill, Logan, Utah, 84322-8200, USA
Related authors
Milada Majerova, Bethany T. Neilson, and Brett B. Roper
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2017-521, https://doi.org/10.5194/hess-2017-521, 2017
Manuscript not accepted for further review
Short summary
Short summary
In this study we quantitatively document the effect of beaver dams on stream ecosystems. Through predicted spatial distributions of hydraulic properties, we demonstrated that geomorphic units within beaver dam complexes exhibit highly unique thermal responses in part due to the variability in flow velocities and depths. Thus we link changes in physical template of the river to thermal variability associated with the development of beaver dam complexes.
Jessica R. Dzara, Bethany T. Neilson, and Sarah E. Null
Hydrol. Earth Syst. Sci., 23, 2965–2982, https://doi.org/10.5194/hess-23-2965-2019, https://doi.org/10.5194/hess-23-2965-2019, 2019
Short summary
Short summary
In Nevada's Walker River, stream temperatures nearly always exceed optimal temperature thresholds for adult trout. We used high-resolution measured data to verify simulated stream temperatures and estimate the spatial distribution of cold-water pockets for fish. Irrigation return canals, beaver dams, and groundwater seeps were river features with cold-water, and the average distance between pockets of cold-water in this river was 2.8 km.
Alan Kasprak, James Brasington, Konrad Hafen, Richard D. Williams, and Joseph M. Wheaton
Earth Surf. Dynam., 7, 247–274, https://doi.org/10.5194/esurf-7-247-2019, https://doi.org/10.5194/esurf-7-247-2019, 2019
Short summary
Short summary
We present a modelling framework for the prediction of gravel-bed braided river evolution. The model is unique in that it simplifies sediment transport through the use of empirically-derived relationships between channel form and flood-scale particle transport distances, or path lengths, which ultimately allow for longer duration model runs with reduced computational demand. We use field surveys on two braided rivers to validate the model at the event, annual, and decadal timescales.
Milada Majerova, Bethany T. Neilson, and Brett B. Roper
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2017-521, https://doi.org/10.5194/hess-2017-521, 2017
Manuscript not accepted for further review
Short summary
Short summary
In this study we quantitatively document the effect of beaver dams on stream ecosystems. Through predicted spatial distributions of hydraulic properties, we demonstrated that geomorphic units within beaver dam complexes exhibit highly unique thermal responses in part due to the variability in flow velocities and depths. Thus we link changes in physical template of the river to thermal variability associated with the development of beaver dam complexes.
Daniel J. Karran, Cherie J. Westbrook, Joseph M. Wheaton, Carol A. Johnston, and Angela Bedard-Haughn
Hydrol. Earth Syst. Sci., 21, 1039–1050, https://doi.org/10.5194/hess-21-1039-2017, https://doi.org/10.5194/hess-21-1039-2017, 2017
Short summary
Short summary
Beaver ponds are found in many landscapes and their transient nature makes it difficult to account for the surface water they store using traditional methods. We found that reliable estimates of surface water storage in beaver ponds can be made with simple measurements of pond depth and surface area. This makes it possible for hydrologists and environmental managers to include beaver ponds in models and land use planning decisions without the need for resource intensive topographic surveys.
R. M. Cory, K. H. Harrold, B.T. Neilson, and G. W. Kling
Biogeosciences, 12, 6669–6685, https://doi.org/10.5194/bg-12-6669-2015, https://doi.org/10.5194/bg-12-6669-2015, 2015
Short summary
Short summary
This study investigates how sunlight, dissolved organic matter (DOM) concentration and composition, and hydrology interact to control DOM degradation in headwater streams. In Imnavait Creek, a shallow, low-relief stream in the Arctic, DOM degradation by sunlight was limited by light under all conditions. Study results were used to synthesize controls on DOM degradation by sunlight for a river reach, expressed as a function of light attenuation and water residence times.
Related subject area
Subject: Ecohydrology | Techniques and Approaches: Theory development
The natural abundance of stable water isotopes method may overestimate deep-layer soil water use by trees
Contribution of cryosphere to runoff in the transition zone between the Tibetan Plateau and arid region based on environmental isotopes
Vegetation optimality explains the convergence of catchments on the Budyko curve
Differential response of plant transpiration to uptake of rainwater-recharged soil water for dominant tree species in the semiarid Loess Plateau
Isotopic offsets between bulk plant water and its sources are larger in cool and wet environments
Hydrology without dimensions
Long-term climate-influenced land cover change in discontinuous permafrost peatland complexes
Groundwater fauna in an urban area – natural or affected?
Age and origin of leaf wax n-alkanes in fluvial sediment–paleosol sequences and implications for paleoenvironmental reconstructions
Seasonal partitioning of precipitation between streamflow and evapotranspiration, inferred from end-member splitting analysis
The influence of litter crusts on soil properties and hydrological processes in a sandy ecosystem
Unexplained hydrogen isotope offsets complicate the identification and quantification of tree water sources in a riparian forest
A synthesis of three decades of hydrological research at Scotty Creek, NWT, Canada
Potential evaporation at eddy-covariance sites across the globe
Scaling properties reveal regulation of river flows in the Amazon through a “forest reservoir”
Water movement through plant roots – exact solutions of the water flow equation in roots with linear or exponential piecewise hydraulic properties
Large-scale vegetation responses to terrestrial moisture storage changes
Vegetation dynamics and climate seasonality jointly control the interannual catchment water balance in the Loess Plateau under the Budyko framework
Leaf-scale experiments reveal an important omission in the Penman–Monteith equation
The Budyko functions under non-steady-state conditions
Matching the Budyko functions with the complementary evaporation relationship: consequences for the drying power of the air and the Priestley–Taylor coefficient
Hydrological recovery in two large forested watersheds of southeastern China: the importance of watershed properties in determining hydrological responses to reforestation
The socioecohydrology of rainwater harvesting in India: understanding water storage and release dynamics across spatial scales
Nitrate sinks and sources as controls of spatio-temporal water quality dynamics in an agricultural headwater catchment
Estimation of crop water requirements: extending the one-step approach to dual crop coefficients
Technical Note: On the Matt–Shuttleworth approach to estimate crop water requirements
Horizontal soil water potential heterogeneity: simplifying approaches for crop water dynamics models
Hurricane impacts on a pair of coastal forested watersheds: implications of selective hurricane damage to forest structure and streamflow dynamics
Regional and local patterns in depth to water table, hydrochemistry and peat properties of bogs and their laggs in coastal British Columbia
Impacts of forest changes on hydrology: a case study of large watersheds in the upper reaches of Minjiang River watershed in China
A simple three-dimensional macroscopic root water uptake model based on the hydraulic architecture approach
Training hydrologists to be ecohydrologists and play a leading role in environmental problem solving
Thermodynamic constraints on effective energy and mass transfer and catchment function
Can we predict groundwater discharge from terrestrial ecosystems using existing eco-hydrological concepts?
Macroinvertebrate community responses to a dewatering disturbance gradient in a restored stream
Mechanisms of vegetation uprooting by flow in alluvial non-cohesive sediment
Forest decline caused by high soil water conditions in a permafrost region
Shaofei Wang, Xiaodong Gao, Min Yang, Gaopeng Huo, Xiaolin Song, Kadambot H. M. Siddique, Pute Wu, and Xining Zhao
Hydrol. Earth Syst. Sci., 27, 123–137, https://doi.org/10.5194/hess-27-123-2023, https://doi.org/10.5194/hess-27-123-2023, 2023
Short summary
Short summary
Water uptake depth of 11-year-old apple trees reached 300 cm in the blossom and young fruit stage and only 100 cm in the fruit swelling stage, while 17-year-old trees always consumed water from 0–320 cm soil layers. Overall, the natural abundance of stable water isotopes method overestimated the contribution of deep soil water, especially in the 320–500 cm soils. Our findings highlight that determining the occurrence of root water uptake in deep soils helps to quantify trees' water use strategy.
Juan Gui, Zongxing Li, Qi Feng, Qiao Cui, and Jian Xue
Hydrol. Earth Syst. Sci., 27, 97–122, https://doi.org/10.5194/hess-27-97-2023, https://doi.org/10.5194/hess-27-97-2023, 2023
Short summary
Short summary
As the transition zone between the Tibetan Plateau and the arid region, the Qilian Mountains are important ecological barriers and source regions of inland rivers in northwest China. In recent decades, drastic changes in the cryosphere have had a significant impact on the quantity and formation process of water resources in the Qilian Mountains. The mountain runoff of the Qilian Mountains mainly comes from the cryosphere belt, which contributes to approximately 80 % runoff.
Remko C. Nijzink and Stanislaus J. Schymanski
Hydrol. Earth Syst. Sci., 26, 6289–6309, https://doi.org/10.5194/hess-26-6289-2022, https://doi.org/10.5194/hess-26-6289-2022, 2022
Short summary
Short summary
Most catchments plot close to the empirical Budyko curve, which allows for estimating the long-term mean annual evaporation and runoff. We found that a model that optimizes vegetation properties in response to changes in precipitation leads it to converge to a single curve. In contrast, models that assume no changes in vegetation start to deviate from a single curve. This implies that vegetation has a stabilizing role, bringing catchments back to equilibrium after changes in climate.
Yakun Tang, Lina Wang, Yongqiang Yu, and Dongxu Lu
Hydrol. Earth Syst. Sci., 26, 4995–5013, https://doi.org/10.5194/hess-26-4995-2022, https://doi.org/10.5194/hess-26-4995-2022, 2022
Short summary
Short summary
Whether rainwater-recharged soil water (RRS) uptake can increase plant transpiration after rainfall pulses requires investigation. Our results indicate a differential response of plant transpiration to RRS uptake. Mixed afforestation enhances these water relationships and decreases soil water source competition in deep soil. Our results suggest that plant species or plantation types that can enhance RRS uptake and reduce water competition should be considered for use in water-limited regions.
Javier de la Casa, Adrià Barbeta, Asun Rodríguez-Uña, Lisa Wingate, Jérôme Ogée, and Teresa E. Gimeno
Hydrol. Earth Syst. Sci., 26, 4125–4146, https://doi.org/10.5194/hess-26-4125-2022, https://doi.org/10.5194/hess-26-4125-2022, 2022
Short summary
Short summary
Recently, studies have been reporting mismatches in the water isotopic composition of plants and soils. In this work, we reviewed worldwide isotopic composition data of field and laboratory studies to see if the mismatch is generalised, and we found it to be true. This contradicts theoretical expectations and may underlie an non-described phenomenon that should be forward investigated and implemented in ecohydrological models to avoid erroneous estimations of water sources used by vegetation.
Amilcare Porporato
Hydrol. Earth Syst. Sci., 26, 355–374, https://doi.org/10.5194/hess-26-355-2022, https://doi.org/10.5194/hess-26-355-2022, 2022
Short summary
Short summary
Applying dimensional analysis to the partitioning of water and soil on terrestrial landscapes reveals their dominant environmental controls. We discuss how the dryness index and the storage index affect the long-term rainfall partitioning, the key nonlinear control of the dryness index in global datasets of weathering rates, and the existence of new macroscopic relations among average variables in landscape evolution statistics with tantalizing analogies with turbulent fluctuations.
Olivia Carpino, Kristine Haynes, Ryan Connon, James Craig, Élise Devoie, and William Quinton
Hydrol. Earth Syst. Sci., 25, 3301–3317, https://doi.org/10.5194/hess-25-3301-2021, https://doi.org/10.5194/hess-25-3301-2021, 2021
Short summary
Short summary
This study demonstrates how climate warming in peatland-dominated regions of discontinuous permafrost is changing the form and function of the landscape. Key insights into the rates and patterns of such changes in the coming decades are provided through careful identification of land cover transitional stages and characterization of the hydrological and energy balance regimes for each stage.
Fabien Koch, Kathrin Menberg, Svenja Schweikert, Cornelia Spengler, Hans Jürgen Hahn, and Philipp Blum
Hydrol. Earth Syst. Sci., 25, 3053–3070, https://doi.org/10.5194/hess-25-3053-2021, https://doi.org/10.5194/hess-25-3053-2021, 2021
Short summary
Short summary
In this study, we address the question of whether groundwater fauna in an urban area is natural or affected in comparison to forested land. We find noticeable differences in the spatial distribution of groundwater species and abiotic parameters. An ecological assessment reveals that conditions in the urban area are mainly not good. Yet, there is no clear spatial pattern in terms of land use and anthropogenic impacts. These are significant findings for conservation and usage of urban groundwater.
Marcel Bliedtner, Hans von Suchodoletz, Imke Schäfer, Caroline Welte, Gary Salazar, Sönke Szidat, Mischa Haas, Nathalie Dubois, and Roland Zech
Hydrol. Earth Syst. Sci., 24, 2105–2120, https://doi.org/10.5194/hess-24-2105-2020, https://doi.org/10.5194/hess-24-2105-2020, 2020
Short summary
Short summary
This study investigates the age and origin of leaf wax n-alkanes from a fluvial sediment–paleosol sequence (FSPS) by compound-class 14C dating. Our results show varying age offsets between the formation and sedimentation of leaf wax n-alkanes from well-developed (paleo)soils and fluvial sediments that are mostly due to their complex origin in such sequences. Thus, dating the leaf wax n-alkanes is an important step for more robust leaf-wax-based paleoenvironmental reconstructions in FSPSs.
James W. Kirchner and Scott T. Allen
Hydrol. Earth Syst. Sci., 24, 17–39, https://doi.org/10.5194/hess-24-17-2020, https://doi.org/10.5194/hess-24-17-2020, 2020
Short summary
Short summary
Perhaps the oldest question in hydrology is
Where does water go when it rains?. Here we present a new way to measure how the terrestrial water cycle partitions precipitation into its two ultimate fates:
green waterthat is evaporated or transpired back to the atmosphere and
blue waterthat is discharged to stream channels. Our analysis may help in gauging the vulnerability of both water resources and terrestrial ecosystems to changes in rainfall patterns.
Yu Liu, Zeng Cui, Ze Huang, Hai-Tao Miao, and Gao-Lin Wu
Hydrol. Earth Syst. Sci., 23, 2481–2490, https://doi.org/10.5194/hess-23-2481-2019, https://doi.org/10.5194/hess-23-2481-2019, 2019
Short summary
Short summary
We focus on the positive effects of litter crusts on soil water holding capacity and water interception capacity compared with biocrusts. Litter crusts can significantly improve sandy water content and organic matter. Water-holding capacity increased with development of litter crusts in the sandy interface. Water infiltration rate is increased by sandy and litter crusts' interface properties. Litter crusts provided a better microhabitat conducive to plant growth in sandy lands.
Adrià Barbeta, Sam P. Jones, Laura Clavé, Lisa Wingate, Teresa E. Gimeno, Bastien Fréjaville, Steve Wohl, and Jérôme Ogée
Hydrol. Earth Syst. Sci., 23, 2129–2146, https://doi.org/10.5194/hess-23-2129-2019, https://doi.org/10.5194/hess-23-2129-2019, 2019
Short summary
Short summary
Plant water sources of a beech riparian forest were monitored using stable isotopes. Isotopic fractionation during root water uptake is usually neglected but may be more common than previously accepted. Xylem water was always more depleted in δ2H than all sources considered, suggesting isotopic discrimination during water uptake or within plant tissues. Thus, the identification and quantification of tree water sources was affected. Still, oxygen isotopes were a good tracer of plant source water.
William Quinton, Aaron Berg, Michael Braverman, Olivia Carpino, Laura Chasmer, Ryan Connon, James Craig, Élise Devoie, Masaki Hayashi, Kristine Haynes, David Olefeldt, Alain Pietroniro, Fereidoun Rezanezhad, Robert Schincariol, and Oliver Sonnentag
Hydrol. Earth Syst. Sci., 23, 2015–2039, https://doi.org/10.5194/hess-23-2015-2019, https://doi.org/10.5194/hess-23-2015-2019, 2019
Short summary
Short summary
This paper synthesizes nearly three decades of eco-hydrological field and modelling studies at Scotty Creek, Northwest Territories, Canada, highlighting the key insights into the major water flux and storage processes operating within and between the major land cover types of this wetland-dominated region of discontinuous permafrost. It also examines the rate and pattern of permafrost-thaw-induced land cover change and how such changes will affect the hydrology and water resources of the region.
Wouter H. Maes, Pierre Gentine, Niko E. C. Verhoest, and Diego G. Miralles
Hydrol. Earth Syst. Sci., 23, 925–948, https://doi.org/10.5194/hess-23-925-2019, https://doi.org/10.5194/hess-23-925-2019, 2019
Short summary
Short summary
Potential evaporation (Ep) is the amount of water an ecosystem would consume if it were not limited by water availability or other stress factors. In this study, we compared several methods to estimate Ep using a global dataset of 107 FLUXNET sites. A simple radiation-driven method calibrated per biome consistently outperformed more complex approaches and makes a suitable tool to investigate the impact of water use and demand, drought severity and biome productivity.
Juan Fernando Salazar, Juan Camilo Villegas, Angela María Rendón, Estiven Rodríguez, Isabel Hoyos, Daniel Mercado-Bettín, and Germán Poveda
Hydrol. Earth Syst. Sci., 22, 1735–1748, https://doi.org/10.5194/hess-22-1735-2018, https://doi.org/10.5194/hess-22-1735-2018, 2018
Short summary
Short summary
River flow regimes are being altered by global change. Understanding the mechanisms behind such alterations is crucial for hydrological prediction. We introduce a novel interpretation of river flow metrics (scaling) that allows any river basin to be classified as regulated or unregulated, and to identify transitions between these states. We propose the
forest reservoirhypothesis to explain how forest loss can force the Amazonian river basins from regulated to unregulated states.
Félicien Meunier, Valentin Couvreur, Xavier Draye, Mohsen Zarebanadkouki, Jan Vanderborght, and Mathieu Javaux
Hydrol. Earth Syst. Sci., 21, 6519–6540, https://doi.org/10.5194/hess-21-6519-2017, https://doi.org/10.5194/hess-21-6519-2017, 2017
Short summary
Short summary
To maintain its yield, a plant needs to transpire water that it acquires from the soil. A deep understanding of the mechanisms that lead to water uptake location and intensity is required to correctly simulate the water transfer in the soil to the atmosphere. This work presents novel and general solutions of the water flow equation in roots with varying hydraulic properties that deeply affect the uptake pattern and the transpiration rate and can be used in ecohydrological models.
Robert L. Andrew, Huade Guan, and Okke Batelaan
Hydrol. Earth Syst. Sci., 21, 4469–4478, https://doi.org/10.5194/hess-21-4469-2017, https://doi.org/10.5194/hess-21-4469-2017, 2017
Short summary
Short summary
In this study we statistically analyse the relationship between vegetation cover and components of total water storage. Splitting water storage into different components allows for a more comprehensive understanding of the temporal response of vegetation to changes in water storage. Generally, vegetation appears to be more sensitive to interannual changes in water storage than to shorter changes, though this varies in different land use types.
Tingting Ning, Zhi Li, and Wenzhao Liu
Hydrol. Earth Syst. Sci., 21, 1515–1526, https://doi.org/10.5194/hess-21-1515-2017, https://doi.org/10.5194/hess-21-1515-2017, 2017
Short summary
Short summary
The relationship between controlling parameters of annual catchment water balance and climate seasonality (S) and vegetation coverage (M) was discussed under the Budyko framework and an empirical equation was further developed so that the contributions from M to actual evapotranspiration (ET) could be determined more accurately. The results showed that the effects of landscape condition changes to ET variation will be estimated with a large error if the impacts of S are ignored.
Stanislaus J. Schymanski and Dani Or
Hydrol. Earth Syst. Sci., 21, 685–706, https://doi.org/10.5194/hess-21-685-2017, https://doi.org/10.5194/hess-21-685-2017, 2017
Short summary
Short summary
Most of the rain falling on land is returned to the atmosphere by plant leaves, which release water vapour (transpire) through tiny pores. To better understand this process, we used artificial leaves in a special wind tunnel and discovered major problems with an established approach (PM equation) widely used to quantify transpiration and its sensitivity to climate change. We present an improved set of equations, consistent with experiments and displaying more realistic climate sensitivity.
Roger Moussa and Jean-Paul Lhomme
Hydrol. Earth Syst. Sci., 20, 4867–4879, https://doi.org/10.5194/hess-20-4867-2016, https://doi.org/10.5194/hess-20-4867-2016, 2016
Short summary
Short summary
A new physically based formulation is proposed to extend the Budyko framework under non-steady-state conditions, taking into account the change in water storage. The new formulation, which introduces an additional parameter, represents a generic framework applicable to any Budyko function at various time steps. It is compared to other formulations from the literature and the analytical solution of Greve et al. (2016) appears to be a particular case.
Jean-Paul Lhomme and Roger Moussa
Hydrol. Earth Syst. Sci., 20, 4857–4865, https://doi.org/10.5194/hess-20-4857-2016, https://doi.org/10.5194/hess-20-4857-2016, 2016
Short summary
Short summary
The Budyko functions are matched with the complementary evaporation relationship. We show that there is a functional dependence between the Budyko functions and the drying power of the air. Examining the case where potential evaporation is calculated by means of a Priestley–Taylor type equation with a varying coefficient, we show that this coefficient should have a specified value as a function of the Budyko shape parameter and the aridity index.
Wenfei Liu, Xiaohua Wei, Qiang Li, Houbao Fan, Honglang Duan, Jianping Wu, Krysta Giles-Hansen, and Hao Zhang
Hydrol. Earth Syst. Sci., 20, 4747–4756, https://doi.org/10.5194/hess-20-4747-2016, https://doi.org/10.5194/hess-20-4747-2016, 2016
Short summary
Short summary
In recent decades, limited research has been conducted to examine the role of watershed properties in hydrological responses in large watersheds. Based on pair-wise comparisons, we conclude that reforestation decreased high flows but increased low flows in the watersheds studied. Hydrological recovery through reforestation is largely dependent on watershed properties when forest change and climate are similar and comparable. This finding has important implications for designing reforestation.
Kimberly J. Van Meter, Michael Steiff, Daniel L. McLaughlin, and Nandita B. Basu
Hydrol. Earth Syst. Sci., 20, 2629–2647, https://doi.org/10.5194/hess-20-2629-2016, https://doi.org/10.5194/hess-20-2629-2016, 2016
Short summary
Short summary
Although village-scale rainwater harvesting (RWH) structures have been used for millennia in India, many of these structures have fallen into disrepair due to increased dependence on groundwater. This dependence has contributed to declines in groundwater resources, and in turn to efforts to revive older RWH systems. In the present study, we use field data to quantify water fluxes in a cascade of irrigation tanks to better our understanding of the impact of RWH systems on the water balance in con
Tobias Schuetz, Chantal Gascuel-Odoux, Patrick Durand, and Markus Weiler
Hydrol. Earth Syst. Sci., 20, 843–857, https://doi.org/10.5194/hess-20-843-2016, https://doi.org/10.5194/hess-20-843-2016, 2016
Short summary
Short summary
We quantify the spatio-temporal impact of distinct nitrate sinks and sources on stream network nitrate dynamics in an agricultural headwater. By applying a data-driven modelling approach, we are able to fully distinguish between mixing and dilution processes, and biogeochemical in-stream removal processes along the stream network. In-stream nitrate removal is estimated by applying a novel transfer coefficient based on energy availability.
J. P. Lhomme, N. Boudhina, M. M. Masmoudi, and A. Chehbouni
Hydrol. Earth Syst. Sci., 19, 3287–3299, https://doi.org/10.5194/hess-19-3287-2015, https://doi.org/10.5194/hess-19-3287-2015, 2015
J. P. Lhomme, N. Boudhina, and M. M. Masmoudi
Hydrol. Earth Syst. Sci., 18, 4341–4348, https://doi.org/10.5194/hess-18-4341-2014, https://doi.org/10.5194/hess-18-4341-2014, 2014
V. Couvreur, J. Vanderborght, L. Beff, and M. Javaux
Hydrol. Earth Syst. Sci., 18, 1723–1743, https://doi.org/10.5194/hess-18-1723-2014, https://doi.org/10.5194/hess-18-1723-2014, 2014
A. D. Jayakaran, T. M. Williams, H. Ssegane, D. M. Amatya, B. Song, and C. C. Trettin
Hydrol. Earth Syst. Sci., 18, 1151–1164, https://doi.org/10.5194/hess-18-1151-2014, https://doi.org/10.5194/hess-18-1151-2014, 2014
S. A. Howie and H. J. van Meerveld
Hydrol. Earth Syst. Sci., 17, 3421–3435, https://doi.org/10.5194/hess-17-3421-2013, https://doi.org/10.5194/hess-17-3421-2013, 2013
X. Cui, S. Liu, and X. Wei
Hydrol. Earth Syst. Sci., 16, 4279–4290, https://doi.org/10.5194/hess-16-4279-2012, https://doi.org/10.5194/hess-16-4279-2012, 2012
V. Couvreur, J. Vanderborght, and M. Javaux
Hydrol. Earth Syst. Sci., 16, 2957–2971, https://doi.org/10.5194/hess-16-2957-2012, https://doi.org/10.5194/hess-16-2957-2012, 2012
M. E. McClain, L. Chícharo, N. Fohrer, M. Gaviño Novillo, W. Windhorst, and M. Zalewski
Hydrol. Earth Syst. Sci., 16, 1685–1696, https://doi.org/10.5194/hess-16-1685-2012, https://doi.org/10.5194/hess-16-1685-2012, 2012
C. Rasmussen
Hydrol. Earth Syst. Sci., 16, 725–739, https://doi.org/10.5194/hess-16-725-2012, https://doi.org/10.5194/hess-16-725-2012, 2012
A. P. O'Grady, J. L. Carter, and J. Bruce
Hydrol. Earth Syst. Sci., 15, 3731–3739, https://doi.org/10.5194/hess-15-3731-2011, https://doi.org/10.5194/hess-15-3731-2011, 2011
J. D. Muehlbauer, M. W. Doyle, and E. S. Bernhardt
Hydrol. Earth Syst. Sci., 15, 1771–1783, https://doi.org/10.5194/hess-15-1771-2011, https://doi.org/10.5194/hess-15-1771-2011, 2011
K. Edmaier, P. Burlando, and P. Perona
Hydrol. Earth Syst. Sci., 15, 1615–1627, https://doi.org/10.5194/hess-15-1615-2011, https://doi.org/10.5194/hess-15-1615-2011, 2011
H. Iwasaki, H. Saito, K. Kuwao, T. C. Maximov, and S. Hasegawa
Hydrol. Earth Syst. Sci., 14, 301–307, https://doi.org/10.5194/hess-14-301-2010, https://doi.org/10.5194/hess-14-301-2010, 2010
Cited articles
Albert, S. and Trimble, T.: Beavers are partners in riparian restoration on the Zuni Indian Reservation, Ecological Restoration, 18, 87–92, https://doi.org/10.3368/er.18.2.87, 2000.
Andersen, D. C., Shafroth, P. B., Pritekel, C. M., and O'Neill, M. W.: Managed flood effects on beaver pond habitat in a desert riverine ecosystem, Bill Williams River, Arizona USA, Wetlands, 31, 195–206, https://doi.org/10.1007/s13157-011-0154-y, 2011.
Barrett, K. R.: Ecological Engineering in Water Resources, Water Int., 24, 182–188, https://doi.org/10.1080/02508069908692160, 1999.
Beschta, L. R., Bilby, E. R., Brown, W. G., Holtby, L. B., and Hofstra, D. T.: Stream temperature and aquatic habitat: fishersies and forestry interactions, in: Streamside Management: Forestry and Fishery Interactions, edited by: Salo, E. O. and Cundy, T. W., University of Washington, Institute of Forest Resources, Seattle, WA, Contribution No. 57, 191–232, 1987.
Billman, E., Kreitzer, J., Creighton, J. C., Habit, E., McMillan, B., and Belk, M.: Habitat enhancement and native fish conservation: can enhancement of channel complexity promote the coexistence of native and introduced fishes?, Environ. Biol. Fish., 96, 555–566, https://doi.org/10.1007/s10641-012-0041-2, 2013.
Brentnall, S. J., Richards, K. J., Brindley, J., and Murphy, E.: Plankton patchiness and its effect on larger-scale productivity, J. Plankton Res., 25, 121–140, https://doi.org/10.1093/plankt/25.2.121, 2003.
Briggs, M. A., Lautz, L. K., and McKenzie, J. M.: A comparison of fibre-optic distributed temperature sensing to traditional methods of evaluating groundwater inflow to streams, Hydrol. Process., 26, 1277–1290, https://doi.org/10.1002/Hyp.8200, 2012.
Burns, D. A. and McDonnell, J. J.: Effects of a beaver pond on runoff processes: comparison of two headwater catchments, J. Hydrol., 205, 248–264, https://doi.org/10.1016/S0022-1694(98)00081-X, 1998.
Cardenas, M. B., Doering, M., Rivas, D. S., Galdeano, C., Neilson, B. T., and Robinson, C. T.: Analysis of the temperature dynamics of a proglacial river using time-lapse thermal imaging and energy balance modeling, J. Hydrol., 519, 1963–1973, https://doi.org/10.1016/j.jhydrol.2014.09.079, 2014.
Cey, E. E., Rudolph, D. L., Parkin, G. W., and Aravena, R.: Quantifying groundwater discharge to a small perennial stream in southern Ontario, Canada, J. Hydrol., 210, 21–37, https://doi.org/10.1016/S0022-1694(98)00172-3, 1998.
Cook, D. B.: Beaver–trout relations, J. Mammal., 21, 397–401, https://doi.org/10.2307/1374874, 1940.
Cooper, S. D., Barmuta, L., Sarnelle, O., Kratz, K., and Diehl, S.: Quantifying spatial heterogeneity in streams, J. N. Am. Benthol. Soc., 16, 174–188, 1997.
Evans, E., McGregor, G. R., and Petts, G. E.: River energy budgets with special reference to river bed processes, Hydrol. Process., 12, 575–595, 1998.
Fanelli, R. M. and Lautz, L. K.: Patterns of water, heat, and solute flux through streambeds around small dams, Ground Water, 46, 671–687, https://doi.org/10.1111/j.1745-6584.2008.00461.x, 2008.
Fuller, M. R. and Peckarsky, B. L.: Ecosystem engineering by beavers affects mayfly life histories, Freshwater Biol., 56, 969–979, https://doi.org/10.1111/j.1365-2427.2010.02548.x, 2011.
Gibson, P. P. and Olden, J. D.: Ecology, management, and conservation implications of North American beaver (Castor canadensis) in dryland streams, Aquat. Conserv., 24, 391–409, https://doi.org/10.1002/aqc.2432, 2014.
Gooseff, M. N. and McGlynn, B. L.: A stream tracer technique employing ionic tracers and specific conductance data applied to the Maimai catchment, New Zealand, Hydrol. Process., 19, 2491–2506, https://doi.org/10.1002/hyp.5685, 2005.
Grünbaum, D.: The logic of ecological patchiness, Interface Focus, 2, 150–155, https://doi.org/10.1098/rsfs.2011.0084, 2012.
Gurnell, A. M.: The hydrogeomorphological effects of beaver dam-building activity, Prog. Phys. Geog., 22, 167–189, 1998.
Harvey, J. W. and Wagner, B. J.: 1 – Quantifying hydrologic interactions between streams and their subsurface hyporheic zones, in: Streams and Ground Waters, edited by: Jones, J. B. and Mulholland, P. J., Academic Press, San Diego, California, A volume in Aquatic Ecology, 3–44, https://doi.org/10.1016/B978-012389845-6/50002-8, 2000.
Hill, A. R. and Duval, T. P.: Beaver dams along an agricultural stream in southern Ontario, Canada: their impact on riparian zone hydrology and nitrogen chemistry, Hydrol. Process., 23, 1324–1336, https://doi.org/10.1002/Hyp.7249, 2009.
Janzen, K. and Westbrook, C. J.: Hyporheic flows along a channelled peatland: influence of beaver dams, Can. Water Resour. J., 36, 331–347, https://doi.org/10.4296/cwrj3604846, 2011.
Johnson, S. L.: Factors influencing stream temperatures in small streams: substrate effects and a shading experiment, Can. J. Fish. Aquat. Sci., 61, 913–923, 2004.
Kemp, P. S., Worthington, T. A., Langford, T. E. L., Tree, A. R. J., and Gaywood, M. J.: Qualitative and quantitative effects of reintroduced beavers on stream fish, Fish Fish., 13, 158–181, https://doi.org/10.1111/j.1467-2979.2011.00421.x, 2012.
Kilpatrick, A. F. and Cobb, D. E.: Measurement of Discharge Using Tracers, Techniques of Water-Resources Investigations, Book 3, Chapter A16, 52 pp., US Geological Survey, Alexandria, VA, 1985.
Lautz, L. K. and Siegel, D. I.: Modeling surface and ground water mixing in the hyporheic zone using MODFLOW and MT3D, Adv. Water Resour., 29, 1618–1633, https://doi.org/10.1016/j.advwatres.2005.12.003, 2006.
Margolis, B. E., Castro, M. S., and Raesly, R. L.: The impact of beaver impoundments on the water chemistry of two Appalachian streams, Can. J. Fish. Aquat. Sci., 58, 2271–2283, https://doi.org/10.1139/cjfas-58-11-2271, 2001.
Merck, M. F. and Neilson, B. T.: Modeling in-pool temperature variability in a beaded arctic stream, Hydrol. Proc., 26, 3921–3933, https://doi.org/10.1002/hyp.8419, 2012.
McGraw, M.: Effect of Beaver Dams on Hyporheos Patterns, in: Ecology of streams and rivers, edited by: Hendricks, W., University of Michigan, Biological Station, University of Michigan, Ann Harbor, MI, 1987.
McRae, G. and Edwards, C. J.: Thermal characteristics of Wisconsin headwater streams occupied by beaver: implications for Brook Trout Habitat, Trans. Am. Fish. Soc., 123, 641–656, https://doi.org/10.1577/1548-8659(1994)123<0641:TCOWHS>2.3.CO;2, 1994.
Meentemeyer, R. K. and Butler, D. R.: Hydrogeomorphic effects of beaver dams in Glacier National Park, Montana, Phys. Geogr., 20, 436–446, https://doi.org/10.1080/02723646.1999.10642688, 1999.
Moore, R. D., Sutherland, P., Gomi, T., and Dhakal, A.: Thermal regime of a headwater stream within a clear-cut, coastal British Columbia, Canada, Hydrol. Process., 19, 2591–2608, https://doi.org/10.1002/hyp.5733, 2005.
Neilson, B. T., Stevens, D. K., Chapra, S. C., and Bandaragoda, C.: Data collection methodology for dynamic tmperature model testing and corroboration, Hydrol. Process., 23, 2902, https://doi.org/10.1002/hyp.7381, 2009.
Neilson, B. T., Chapra, S. C., Stevens, D. K., and Bandaragoda, C.: Two-zone transient storage modeling using temperature and solute data with multiobjective calibration: 1. Temperature, Water Resour. Res., 46, W12520, https://doi.org/10.1029/2009WR008756, 2010a.
Neilson, B. T., Stevens, D. K., Chapra, S. C., and Bandaragoda, C.: Two-zone transient storage modeling using temperature and solute data with multiobjective calibration: 2. Temperature and solute, Water Resour. Res., 46, W12521, https://doi.org/10.1029/2009WR008759, 2010b.
Nyssen, J., Pontzeele, J., and Billi, P.: Effect of beaver dams on the hydrology of small mountain streams: example from the Chevral in the Ourthe Orientale Basin, Ardennes, Belgium, J. Hydrol., 402, 92–102, https://doi.org/10.1016/j.jhydrol.2011.03.008, 2011.
Payn, R. A., Gooseff, M. N., McGlynn, B. L., Bencala, K. E., and Wondzell, S. M.: Channel water balance and exchange with subsurface flow along a mountain headwater stream in Montana, United States, Water Resour. Res., 45, W11427, https://doi.org/10.1029/2008wr007644, 2009.
Pollock, M. M., Pess, G. R., Beechie, T. J., and Montgomery, D. R.: The importance of beaver ponds to coho salmon production in the Stillaguamish River Basin, Washington, USA, N. Am. J. Fish. Manage., 24, 749–760, https://doi.org/10.1577/M03-156.1, 2004.
Pollock, M. M., Beechie, T. J., and Jordan, C. E.: Geomorphic changes upstream of beaver dams in Bridge Creek, an incised stream channel in the interior Columbia River Basin, eastern Oregon, Earth Surf. Proc. Land., 32, 1174–1185, https://doi.org/10.1002/esp.1553, 2007.
Rantz, S. E.: Measurement and Computation of Streamflow: Computation of Discharge, Water Supply Paper, Report 2175, US Geological Survey, Denver, 2, 285–631, 1982.
Rosell, F., Bozsér, O., Collen, P., and Parker, H.: Ecological impact of beavers Castor fiber and Castor canadensis and their ability to modify ecosystems, Mammal Rev., 35, 248–276, https://doi.org/10.1111/j.1365-2907.2005.00067.x, 2005.
Salyer, J. C.: Preliminary report on the beaver-trout investigation, American Game, 24, 6–15, 1935.
Schmadel, N. M., Neilson, B. T., and Stevens, D. K.: Approaches to estimate uncertainty in longitudinal channel water balances, J. Hydrol., 394, 357–369, https://doi.org/10.1016/j.jhydrol.2010.09.011, 2010.
Schmadel, N. M., Neilson, B. T., and Kasahara, T.: Deducing the spatial variability of exchange within a longitudinal channel water balance, Hydrol. Process., 28, 3088–3103, https://doi.org/10.1002/hyp.9854, 2014.
Shetter, D. S. and Whalls, M. J.: Effect of impoundment on water temperatures of Fuller Creek, Montmorency County, Michigan, J. Wildlife Manage., 19, 47–54, https://doi.org/10.2307/3797551, 1955.
Shields Jr., F., Cooper, C., and Knight, S.: Experiment in stream restoration, J. Hydraul. Eng.-ASCE, 121, 494–502, https://doi.org/10.1061/(ASCE)0733-9429(1995)121:6(494), 1995.
Sinokrot, B. A. and Stefan, H. G.: Stream temperature dynamics: measurements and modeling, Water Resour. Res., 29, 2299–2312, https://doi.org/10.1029/93WR00540, 1993.
Snow, C. J.: Impact of Beaver Ponds on Stream Temperature and on Solar Radiation Penetration in Water, PhD thesis, Utah State University, Logan, Utah, 2014.
Talabere, A. G.: Influence of water temperature and beaver ponds on Lahontan cutthroat trout in a high-desert stream, southeastern Oregon, Oregon State University, Corvallis, OR, 44 leaves, 2002.
Ward, A. S., Payn, R. A., Gooseff, M. N., McGlynn, B. L., Bencala, K. E., Kelleher, C. A., Wondezell, S. M., and Wagener, T.: Variations in surface water-ground water interactions along a headwater mountain stream: Comparison between transient storage and water balance analyses, Water Resour. Res., 49, 3359–3374, https://doi.org/10.1002/wrcr.20148, 2013.
Webb, B. and Zhang, Y.: Spatial and seasonal variability in the components of the river heat budget, Hydrol. Process., 11, 79–101, 1997.
Westbrook, C. J., Cooper, D. J., and Baker, B. W.: Beaver assisted river valley formation, River Res. Appl., 27, 247–256, https://doi.org/10.1002/Rra.1359, 2011.
Westhoff, M. C., Savenije, H. H. G., Luxemburg, W. M. J ., Stelling, G. S., van de Giesen, N. C., Selker, J. S., Pfister, L., and Uhlenbrook, S.: A distributed stream temperature model using high resolution temperature observations, Hydrol. Earth Syst. Sci., 11, 1469–1480, https://doi.org/10.5194/hess-11-1469-2007, 2007.
White, D. S.: Biological relationships to convective flow patterns within stream beds, Hydrobiologia, 196, 149–158, https://doi.org/10.1007/Bf00006106, 1990.
Younus, M., Hondzo, M., and Engel, B.: Stream temperature dynamics in upland agricultural watersheds, J. Environ. Eng., 126, 518–526, 2000.
Zellweger, G. W.: Testing and comparison of four ionic tracers to measure stream flow loss by multiple tracer injection, Hydrol. Process., 8, 155–165, https://doi.org/10.1002/hyp.3360080206, 1994.
Utah Division of Wildlife Resources: Utah Beaver Management Plan 2010–2020, DWR Publication 09-29, Utah Division of Wildlife Resources, Salt Lake City, Utah, 2010.
Short summary
This study quantifies the impacts of beaver on hydrologic and temperature regimes, as well as highlights the importance of understanding the spatial and temporal scales of those impacts.
Reach-scale discharge showed shift from losing to gaining. Temperature increased by 0.38°C (3.8%) and mean residence time by 230%. At the sub-reach scale, discharge gains and losses increased in variability. At the beaver dam scale, we observed increase in thermal heterogeneity with warmer and cooler niches.
This study quantifies the impacts of beaver on hydrologic and temperature regimes, as well as...
