Articles | Volume 25, issue 12
https://doi.org/10.5194/hess-25-6309-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-25-6309-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Use of water isotopes and chemistry to infer the type and degree of exchange between groundwater and lakes in an esker complex of northeastern Ontario, Canada
Department of Geography and Planning, Queen's University, Kingston,
K7L3N6, Canada
Scott F. Lamoureux
Department of Geography and Planning, Queen's University, Kingston,
K7L3N6, Canada
Brian F. Cumming
Department of Biology, Queen's University, Kingston, K7L3J9, Canada
School of Environmental Studies, Queen's University, Kingston, K7L3J9,
Canada
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Thomas Schneider von Deimling, Hanna Lee, Thomas Ingeman-Nielsen, Sebastian Westermann, Vladimir Romanovsky, Scott Lamoureux, Donald A. Walker, Sarah Chadburn, Erin Trochim, Lei Cai, Jan Nitzbon, Stephan Jacobi, and Moritz Langer
The Cryosphere, 15, 2451–2471, https://doi.org/10.5194/tc-15-2451-2021, https://doi.org/10.5194/tc-15-2451-2021, 2021
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Climate warming puts infrastructure built on permafrost at risk of failure. There is a growing need for appropriate model-based risk assessments. Here we present a modelling study and show an exemplary case of how a gravel road in a cold permafrost environment in Alaska might suffer from degrading permafrost under a scenario of intense climate warming. We use this case study to discuss the broader-scale applicability of our model for simulating future Arctic infrastructure failure.
Cody C. Routson, Darrell S. Kaufman, Nicholas P. McKay, Michael P. Erb, Stéphanie H. Arcusa, Kendrick J. Brown, Matthew E. Kirby, Jeremiah P. Marsicek, R. Scott Anderson, Gonzalo Jiménez-Moreno, Jessica R. Rodysill, Matthew S. Lachniet, Sherilyn C. Fritz, Joseph R. Bennett, Michelle F. Goman, Sarah E. Metcalfe, Jennifer M. Galloway, Gerrit Schoups, David B. Wahl, Jesse L. Morris, Francisca Staines-Urías, Andria Dawson, Bryan N. Shuman, Daniel G. Gavin, Jeffrey S. Munroe, and Brian F. Cumming
Earth Syst. Sci. Data, 13, 1613–1632, https://doi.org/10.5194/essd-13-1613-2021, https://doi.org/10.5194/essd-13-1613-2021, 2021
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We present a curated database of western North American Holocene paleoclimate records, which have been screened on length, resolution, and geochronology. The database gathers paleoclimate time series that reflect temperature, hydroclimate, or circulation features from terrestrial and marine sites, spanning a region from Mexico to Alaska. This publicly accessible collection will facilitate a broad range of paleoclimate inquiry.
Caroline Coch, Bennet Juhls, Scott F. Lamoureux, Melissa J. Lafrenière, Michael Fritz, Birgit Heim, and Hugues Lantuit
Biogeosciences, 16, 4535–4553, https://doi.org/10.5194/bg-16-4535-2019, https://doi.org/10.5194/bg-16-4535-2019, 2019
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Climate change affects Arctic ecosystems. This includes thawing of permafrost (ground below 0 °C) and an increase in rainfall. Both have substantial impacts on the chemical composition of river water. We compared the composition of small rivers in the low and high Arctic with the large Arctic rivers. In comparison, dissolved organic matter in the small rivers is more susceptible to degradation; thus, it could potentially increase carbon dioxide emissions. Rainfall events have a similar effect.
Jean E. Holloway, Ashley C. A. Rudy, Scott F. Lamoureux, and Paul M. Treitz
The Cryosphere, 11, 1403–1415, https://doi.org/10.5194/tc-11-1403-2017, https://doi.org/10.5194/tc-11-1403-2017, 2017
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Below ground pressurization occurs when there is more moisture in the soil pores than normal, and it can potentially result in landscape degradation. We mapped features that are caused by this overpressurization and generated susceptibility maps to find other areas on the landscape that could be susceptible in the future. The susceptibility maps identified areas that may be sensitive to pressurization and help improve our understanding of potentially hazardous permafrost degradation.
François Lapointe, Pierre Francus, Scott F. Lamoureux, Mathias Vuille, Jean-Philippe Jenny, Raymond S. Bradley, and Charly Massa
Clim. Past, 13, 411–420, https://doi.org/10.5194/cp-13-411-2017, https://doi.org/10.5194/cp-13-411-2017, 2017
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Using a unique annually-laminated record (varve) from the western Canadian High Arctic, we found a significant relationship between our varve record and instrumental and reconstructed Pacific Decadal Oscillations (PDOs). The negative (positive) PDO (North Pacific Index) phases increase precipitation as low sea-ice extent, warmer temperature and winds reach our region more efficiently. Our results imply that future negative PDO phases will likely impact the already rapidly warming Arctic.
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Subject: Catchment hydrology | Techniques and Approaches: Instruments and observation techniques
Exploring the provenance of information across Canadian hydrometric stations: implications for discharge estimation and uncertainty quantification
Using high-frequency solute synchronies to determine simple two-end-member mixing in catchments during storm events
Thermal regime of High Arctic tundra ponds, Nanuit Itillinga (Polar Bear Pass), Nunavut, Canada
Impacts of hydrofacies geometry designed from seismic refraction tomography on estimated hydrogeophysical variables
Seasonal dynamics and spatial patterns of soil moisture in a loess catchment
Effects of urbanization on the water cycle in the Shiyang River basin: based on a stable isotope method
Isotopic variations in surface waters and groundwaters of an extremely arid basin and their responses to climate change
Seasonal variation and influence factors of river water isotopes in the East Asian monsoon region: a case study in the Xiangjiang River basin spanning 13 hydrological years
El Niño–Southern Oscillation (ENSO)-driven hypersedimentation in the Poechos Reservoir, northern Peru
Isotope-derived young water fractions in streamflow across the tropical Andes mountains and Amazon floodplain
Adaptively monitoring streamflow using a stereo computer vision system
Technical Note: Combining undisturbed soil monoliths for hydrological indoor experiments
Hydrodynamics of a high Alpine catchment characterized by four natural tracers
Seasonal variation and release of soluble reactive phosphorus in an agricultural upland headwater in central Germany
Improving the understanding of N transport in a rural catchment under Atlantic climate conditions from the analysis of the concentration–discharge relationship derived from a high-frequency data set
Sources and mean transit times of stream water in an intermittent river system: the upper Wimmera River, southeast Australia
Bedrock depth influences spatial patterns of summer baseflow, temperature and flow disconnection for mountainous headwater streams
Agricultural intensification vs. climate change: what drives long-term changes in sediment load?
Evaporation from a large lowland reservoir – observed dynamics and drivers during a warm summer
Comment on “A comparison of catchment travel times and storage deduced from deuterium and tritium tracers using StorAge Selection functions” by Rodriguez et al. (2021)
Technical note: Introduction of a superconducting gravimeter as novel hydrological sensor for the Alpine research catchment Zugspitze
CABra: a novel large-sample dataset for Brazilian catchments
Benefits from high-density rain gauge observations for hydrological response analysis in a small alpine catchment
Hydrologic regimes drive nitrate export behavior in human-impacted watersheds
Intensive landscape-scale remediation improves water quality of an alluvial gully located in a Great Barrier Reef catchment
Environmental DNA simultaneously informs hydrological and biodiversity characterization of an Alpine catchment
Technical note: Evaluation of a low-cost evaporation protection method for portable water samplers
New flood frequency estimates for the largest river in Norway based on the combination of short and long time series
The pulse of a montane ecosystem: coupling between daily cycles in solar flux, snowmelt, transpiration, groundwater, and streamflow at Sagehen Creek and Independence Creek, Sierra Nevada, USA
Technical note: A time-integrated sediment trap to sample diatoms for hydrological tracing
Do stream water solute concentrations reflect when connectivity occurs in a small, pre-Alpine headwater catchment?
Soil moisture sensor network design for hydrological applications
Catchment-scale drought: capturing the whole drought cycle using multiple indicators
Field-based estimation and modelling of distributed groundwater recharge in a Mediterranean karst catchment, Wadi Natuf, West Bank
Surface water as a cause of land degradation from dryland salinity
Technical note: A microcontroller-based automatic rain sampler for stable isotope studies
Controls on spatial and temporal variability in streamflow and hydrochemistry in a glacierized catchment
Open-source Arduino-compatible data loggers designed for field research
Water-use dynamics of an alien-invaded riparian forest within the summer rainfall zone of South Africa
Technical note: Mapping surface-saturation dynamics with thermal infrared imagery
Value of uncertain streamflow observations for hydrological modelling
Why has catchment evaporation increased in the past 40 years? A data-based study in Austria
Technical note: GUARD – an automated fluid sampler preventing sample alteration by contamination, evaporation and gas exchange, suitable for remote areas and harsh conditions
Hydrological processes and permafrost regulate magnitude, source and chemical characteristics of dissolved organic carbon export in a peatland catchment of northeastern China
Exploring the influence of citizen involvement on the assimilation of crowdsourced observations: a modelling study based on the 2013 flood event in the Bacchiglione catchment (Italy)
Comment on “Can assimilation of crowdsourced data in hydrological modelling improve flood prediction?” by Mazzoleni et al. (2017)
Multiconfiguration electromagnetic induction survey for paleochannel internal structure imaging: a case study in the alluvial plain of the River Seine, France
Tree-, stand- and site-specific controls on landscape-scale patterns of transpiration
The potamochemical symphony: new progress in the high-frequency acquisition of stream chemical data
Impact of snow deposition on major and trace element concentrations and elementary fluxes in surface waters of the Western Siberian Lowland across a 1700 km latitudinal gradient
Shervan Gharari, Paul H. Whitfield, Alain Pietroniro, Jim Freer, Hongli Liu, and Martyn P. Clark
Hydrol. Earth Syst. Sci., 28, 4383–4405, https://doi.org/10.5194/hess-28-4383-2024, https://doi.org/10.5194/hess-28-4383-2024, 2024
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This study provides insight into the practices that are incorporated into discharge estimation across the national Canadian hydrometric network operated by the Water Survey of Canada (WSC). The procedures used to estimate and correct discharge values are not always understood by end-users. Factors such as ice cover and sedimentation limit accurate discharge estimation. Highlighting these challenges sheds light on difficulties in discharge estimation and the associated uncertainty.
Nicolai Brekenfeld, Solenn Cotel, Mikaël Faucheux, Paul Floury, Colin Fourtet, Jérôme Gaillardet, Sophie Guillon, Yannick Hamon, Hocine Henine, Patrice Petitjean, Anne-Catherine Pierson-Wickmann, Marie-Claire Pierret, and Ophélie Fovet
Hydrol. Earth Syst. Sci., 28, 4309–4329, https://doi.org/10.5194/hess-28-4309-2024, https://doi.org/10.5194/hess-28-4309-2024, 2024
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The proposed methodology consists of simultaneously analysing the concentration variation of solute pairs during a storm event by plotting the concentration variation of one solute against the variation of another solute. This can reveal whether two or more end-members contribute to streamflow during a storm event. Furthermore, the variation of the solute ratios during the events can indicate which catchment processes are dominant and which are negligible.
Kathy L. Young and Laura C. Brown
Hydrol. Earth Syst. Sci., 28, 3931–3945, https://doi.org/10.5194/hess-28-3931-2024, https://doi.org/10.5194/hess-28-3931-2024, 2024
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This work details the temperature and related variables of several High Arctic ponds in the Nanuit Itillinga (Polar Bear Pass) National Wildlife Area through nine seasons. The ponds show much variability in their temperature patterns over time and space. Ponds normally reached 10–15 °C for parts of the summer except in 2013, a cold summer season in which pond temperatures never exceeded 5 °C. This study contributes to the ongoing discussion of climate warming and its impact on Arctic landscapes.
Nolwenn Lesparre, Sylvain Pasquet, and Philippe Ackerer
Hydrol. Earth Syst. Sci., 28, 873–897, https://doi.org/10.5194/hess-28-873-2024, https://doi.org/10.5194/hess-28-873-2024, 2024
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Vertical maps of seismic velocity reflect variations of subsurface porosity. We use such images to design the geometry of subsurface compartments delimited by velocity thresholds. The obtained patterns are inserted into a hydrogeological model to test the influence of random geometries, velocity thresholds, and hydraulic parameters on data estimated from the model: the depth of the groundwater and magnetic resonance sounding is a geophysical method sensitive to subsurface water content.
Shaozhen Liu, Ilja van Meerveld, Yali Zhao, Yunqiang Wang, and James W. Kirchner
Hydrol. Earth Syst. Sci., 28, 205–216, https://doi.org/10.5194/hess-28-205-2024, https://doi.org/10.5194/hess-28-205-2024, 2024
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We study the seasonal and spatial patterns of soil moisture in 0–500 cm soil using 89 monitoring sites in a loess catchment with monsoonal climate. Soil moisture is highest during the months of least precipitation and vice versa. Soil moisture patterns at the hillslope scale are dominated by the aspect-controlled evapotranspiration variations (a local control), not by the hillslope convergence-controlled downslope flow (a nonlocal control), under both dry and wet conditions.
Rui Li, Guofeng Zhu, Siyu Lu, Liyuan Sang, Gaojia Meng, Longhu Chen, Yinying Jiao, and Qinqin Wang
Hydrol. Earth Syst. Sci., 27, 4437–4452, https://doi.org/10.5194/hess-27-4437-2023, https://doi.org/10.5194/hess-27-4437-2023, 2023
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In semi-arid regions, the problem of water shortages is becoming more and more serious with the acceleration of urbanization. Based on isotope data and hydrometeorological data, we analysed the impact of urbanization on the water cycle of the basin. The results showed that urbanization sped up the process of rainfall runoff. The MRT got shorter from upstream to downstream, and the landscape dams that were built during urbanization made the river evaporate even more.
Yu Zhang, Hongbing Tan, Peixin Cong, Dongping Shi, Wenbo Rao, and Xiying Zhang
Hydrol. Earth Syst. Sci., 27, 4019–4038, https://doi.org/10.5194/hess-27-4019-2023, https://doi.org/10.5194/hess-27-4019-2023, 2023
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Rapid climate warming creates barriers for us to investigate water resource states. Using stable and radioactive isotopes, we identified the seasonality and spatiality of the water cycle in the northeastern Tibetan Plateau. Climate warming/humidification accelerates the water cycle in alpine arid basins. Precipitation and meltwater infiltrate along preferential flow paths to facilitate rapid groundwater recharge. Total water resources may show an initially increasing and then decreasing trend.
Xiong Xiao, Xinping Zhang, Zhuoyong Xiao, Zhiguo Rao, Xinguang He, and Cicheng Zhang
Hydrol. Earth Syst. Sci., 27, 3783–3802, https://doi.org/10.5194/hess-27-3783-2023, https://doi.org/10.5194/hess-27-3783-2023, 2023
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With the aim of improving the understanding of seasonal variations in water stable isotopes and catchment hydrological processes, we compared the temporal variations of precipitation and river water isotopes with the hydrometeorological factors in the Xiangjiang River over 13 years. Results showed that the changes in river water isotopes can be variables that reflect the seasonal variations in local environments and extreme events and may show implications for paleoclimate reconstruction.
Anthony Foucher, Sergio Morera, Michael Sanchez, Jhon Orrillo, and Olivier Evrard
Hydrol. Earth Syst. Sci., 27, 3191–3204, https://doi.org/10.5194/hess-27-3191-2023, https://doi.org/10.5194/hess-27-3191-2023, 2023
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The current research investigated, as a representative study case, the sediment accumulated in the Poechos Reservoir (located on the west coast of northern Peru) for retrospectively reconstructing the impact on sediment dynamics (1978–2019) of extreme phases of the El Niño–Southern Oscillation, land cover changes after humid periods and agricultural expansion along the riverine system.
Emily I. Burt, Daxs Herson Coayla Rimachi, Adan Julian Ccahuana Quispe, Abra Atwood, and A. Joshua West
Hydrol. Earth Syst. Sci., 27, 2883–2898, https://doi.org/10.5194/hess-27-2883-2023, https://doi.org/10.5194/hess-27-2883-2023, 2023
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Mountains store and release water, serving as water towers for downstream regions and affecting global sediment and carbon fluxes. We use stream and rain chemistry to calculate how much streamflow comes from recent rainfall across seven sites in the Andes mountains and the nearby Amazon lowlands. We find that the type of rock and the intensity of rainfall control water retention and release, challenging assumptions that mountain topography exerts the primary effect on watershed hydrology.
Nicholas Reece Hutley, Ryan Beecroft, Daniel Wagenaar, Josh Soutar, Blake Edwards, Nathaniel Deering, Alistair Grinham, and Simon Albert
Hydrol. Earth Syst. Sci., 27, 2051–2073, https://doi.org/10.5194/hess-27-2051-2023, https://doi.org/10.5194/hess-27-2051-2023, 2023
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Measuring flows in streams allows us to manage crucial water resources. This work shows the automated application of a dual camera computer vision stream gauging (CVSG) system for measuring streams. Comparing between state-of-the-art technologies demonstrated that camera-based methods were capable of performing within the best available error margins. CVSG offers significant benefits towards improving stream data and providing a safe way for measuring floods while adapting to changes over time.
David Ramler and Peter Strauss
Hydrol. Earth Syst. Sci., 27, 1745–1754, https://doi.org/10.5194/hess-27-1745-2023, https://doi.org/10.5194/hess-27-1745-2023, 2023
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Undisturbed soil monoliths combine advantages of outdoor and indoor experiments; however, there are often size limitations. A promising approach is the combination of smaller blocks to form a single large monolith. We compared the runoff properties of monoliths cut in half and recombined with uncut blocks. The effect of the combination procedure was negligible compared to the inherent soil heterogeneity, and we conclude that advantages outweigh possible adverse effects.
Anthony Michelon, Natalie Ceperley, Harsh Beria, Joshua Larsen, Torsten Vennemann, and Bettina Schaefli
Hydrol. Earth Syst. Sci., 27, 1403–1430, https://doi.org/10.5194/hess-27-1403-2023, https://doi.org/10.5194/hess-27-1403-2023, 2023
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Streamflow generation processes in high-elevation catchments are largely influenced by snow accumulation and melt. For this work, we collected and analyzed more than 2800 water samples (temperature, electric conductivity, and stable isotopes of water) to characterize the hydrological processes in such a high Alpine environment. Our results underline the critical role of subsurface flow during all melt periods and the presence of snowmelt even during the winter periods.
Michael Rode, Jörg Tittel, Frido Reinstorf, Michael Schubert, Kay Knöller, Benjamin Gilfedder, Florian Merensky-Pöhlein, and Andreas Musolff
Hydrol. Earth Syst. Sci., 27, 1261–1277, https://doi.org/10.5194/hess-27-1261-2023, https://doi.org/10.5194/hess-27-1261-2023, 2023
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Agricultural catchments show elevated phosphorus (P) concentrations during summer low flow. In an agricultural stream, we found that phosphorus in groundwater was a major source of stream water phosphorus during low flow, and stream sediments derived from farmland are unlikely to have increased stream phosphorus concentrations during low water. We found no evidence that riparian wetlands contributed to soluble reactive (SR) P loads. Agricultural phosphorus was largely buffered in the soil zone.
María Luz Rodríguez-Blanco, María Teresa Taboada-Castro, and María Mercedes Taboada-Castro
Hydrol. Earth Syst. Sci., 27, 1243–1259, https://doi.org/10.5194/hess-27-1243-2023, https://doi.org/10.5194/hess-27-1243-2023, 2023
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We examine the N dynamics in an Atlantic headwater catchment in the NW Iberian Peninsula, using high-frequency measurements of NO3 and TKN (total Kjeldahl N) during runoff events. The divergence dynamics observed between N components exemplifies the complexity of and variability in NO3 and TKN processes, highlighting the need to understand dominant hydrological pathways for the development of N-specific management plans to ensure that control measures are most effective at the catchment scale.
Zibo Zhou, Ian Cartwright, and Uwe Morgenstern
Hydrol. Earth Syst. Sci., 26, 4497–4513, https://doi.org/10.5194/hess-26-4497-2022, https://doi.org/10.5194/hess-26-4497-2022, 2022
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Streams may receive water from different sources in their catchment. There is limited understanding of which water stores intermittent streams are connected to. Using geochemistry we show that the intermittent streams in southeast Australia are connected to younger smaller near-river water stores rather than regional groundwater. This makes these streams more vulnerable to the impacts of climate change and requires management of the riparian zone for their protection.
Martin A. Briggs, Phillip Goodling, Zachary C. Johnson, Karli M. Rogers, Nathaniel P. Hitt, Jennifer B. Fair, and Craig D. Snyder
Hydrol. Earth Syst. Sci., 26, 3989–4011, https://doi.org/10.5194/hess-26-3989-2022, https://doi.org/10.5194/hess-26-3989-2022, 2022
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The geologic structure of mountain watersheds may control how groundwater and streamwater exchange, influencing where streams dry. We measured bedrock depth at 191 locations along eight headwater streams paired with stream temperature records, baseflow separation and observations of channel dewatering. The data indicated a prevalence of shallow bedrock generally less than 3 m depth, and local variation in that depth can drive stream dewatering but also influence stream baseflow supply.
Shengping Wang, Borbala Szeles, Carmen Krammer, Elmar Schmaltz, Kepeng Song, Yifan Li, Zhiqiang Zhang, Günter Blöschl, and Peter Strauss
Hydrol. Earth Syst. Sci., 26, 3021–3036, https://doi.org/10.5194/hess-26-3021-2022, https://doi.org/10.5194/hess-26-3021-2022, 2022
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This study explored the quantitative contribution of agricultural intensification and climate change to the sediment load of a small agricultural watershed. Rather than a change in climatic conditions, changes in the land structure notably altered sediment concentrations under high-flow conditions, thereby contributing most to the increase in annual sediment loads. More consideration of land structure improvement is required when combating the transfer of soil from land to water.
Femke A. Jansen, Remko Uijlenhoet, Cor M. J. Jacobs, and Adriaan J. Teuling
Hydrol. Earth Syst. Sci., 26, 2875–2898, https://doi.org/10.5194/hess-26-2875-2022, https://doi.org/10.5194/hess-26-2875-2022, 2022
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We studied the controls on open water evaporation with a focus on Lake IJssel, the Netherlands, by analysing eddy covariance observations over two summer periods at two locations at the borders of the lake. Wind speed and the vertical vapour pressure gradient can explain most of the variation in observed evaporation, which is in agreement with Dalton's model. We argue that the distinct characteristics of inland waterbodies need to be taken into account when parameterizing their evaporation.
Michael Kilgour Stewart, Uwe Morgenstern, and Ian Cartwright
Hydrol. Earth Syst. Sci., 25, 6333–6338, https://doi.org/10.5194/hess-25-6333-2021, https://doi.org/10.5194/hess-25-6333-2021, 2021
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The combined use of deuterium and tritium to determine travel time distributions in streams is an important development in catchment hydrology (Rodriguez et al., 2021). This comment, however, argues that their results do not generally invalidate the truncation hypothesis of Stewart et al. (2010) (i.e. that stable isotopes underestimate travel times through catchments), as they imply, but asserts instead that the hypothesis still applies to many other catchments.
Christian Voigt, Karsten Schulz, Franziska Koch, Karl-Friedrich Wetzel, Ludger Timmen, Till Rehm, Hartmut Pflug, Nico Stolarczuk, Christoph Förste, and Frank Flechtner
Hydrol. Earth Syst. Sci., 25, 5047–5064, https://doi.org/10.5194/hess-25-5047-2021, https://doi.org/10.5194/hess-25-5047-2021, 2021
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A continuously operating superconducting gravimeter at the Zugspitze summit is introduced to support hydrological studies of the Partnach spring catchment known as the Zugspitze research catchment. The observed gravity residuals reflect total water storage variations at the observation site. Hydro-gravimetric analysis show a high correlation between gravity and the snow water equivalent, with a gravimetric footprint of up to 4 km radius enabling integral insights into this high alpine catchment.
André Almagro, Paulo Tarso S. Oliveira, Antônio Alves Meira Neto, Tirthankar Roy, and Peter Troch
Hydrol. Earth Syst. Sci., 25, 3105–3135, https://doi.org/10.5194/hess-25-3105-2021, https://doi.org/10.5194/hess-25-3105-2021, 2021
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We have collected and synthesized catchment attributes from multiple sources into an extensive dataset, the Catchment Attributes for Brazil (CABra). CABra contains streamflow and climate daily series for 735 catchments in the 1980–2010 period, aside from dozens of attributes of topography, climate, streamflow, groundwater, soil, geology, land cover, and hydrologic disturbance. The CABra intends to pave the way for a better understanding of catchments' behavior in Brazil and the world.
Anthony Michelon, Lionel Benoit, Harsh Beria, Natalie Ceperley, and Bettina Schaefli
Hydrol. Earth Syst. Sci., 25, 2301–2325, https://doi.org/10.5194/hess-25-2301-2021, https://doi.org/10.5194/hess-25-2301-2021, 2021
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Rainfall observation remains a challenge, particularly in mountain environments. Unlike most studies which are model based, this analysis of the rainfall–runoff response of a 13.4 km2 alpine catchment is purely data based and relies on measurements from a network of 12 low-cost rain gauges over 3 months. It assesses the importance of high-density rainfall observations in informing hydrological processes and helps in designing a permanent rain gauge network.
Galen Gorski and Margaret A. Zimmer
Hydrol. Earth Syst. Sci., 25, 1333–1345, https://doi.org/10.5194/hess-25-1333-2021, https://doi.org/10.5194/hess-25-1333-2021, 2021
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Understanding when, where, and how nitrate is exported from watersheds is the key to addressing the challenges that excess nutrients pose. We analyzed daily nitrate and streamflow data for five nested, agricultural watersheds that export high levels of nitrate over a 4-year time period. Nutrient export patterns varied seasonally during baseflow but were stationary during stormflow. Additionally, anthropogenic and geologic factors drove nutrient export during both baseflow and stormflow.
Nicholas J. C. Doriean, William W. Bennett, John R. Spencer, Alexandra Garzon-Garcia, Joanne M. Burton, Peter R. Teasdale, David T. Welsh, and Andrew P. Brooks
Hydrol. Earth Syst. Sci., 25, 867–883, https://doi.org/10.5194/hess-25-867-2021, https://doi.org/10.5194/hess-25-867-2021, 2021
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Gully erosion is a major contributor to suspended sediment and associated nutrient pollution (e.g. gullies generate approximately 40 % of the sediment pollution impacting the Great Barrier Reef). This study used a new method of monitoring to demonstrate how large-scale earthworks used to remediated large gullies (i.e. eroding landforms > 1 ha) can drastically improve the water quality of connected waterways and, thus, protect vulnerable ecosystems in downstream-receiving waters.
Elvira Mächler, Anham Salyani, Jean-Claude Walser, Annegret Larsen, Bettina Schaefli, Florian Altermatt, and Natalie Ceperley
Hydrol. Earth Syst. Sci., 25, 735–753, https://doi.org/10.5194/hess-25-735-2021, https://doi.org/10.5194/hess-25-735-2021, 2021
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In this study, we collected water from an Alpine catchment in Switzerland and compared the genetic information of eukaryotic organisms conveyed by eDNA with the hydrologic information conveyed by naturally occurring hydrologic tracers. At the intersection of two disciplines, our study provides complementary knowledge gains and identifies the next steps to be addressed for using eDNA to achieve complementary insights into Alpine water sources.
Jana von Freyberg, Julia L. A. Knapp, Andrea Rücker, Bjørn Studer, and James W. Kirchner
Hydrol. Earth Syst. Sci., 24, 5821–5834, https://doi.org/10.5194/hess-24-5821-2020, https://doi.org/10.5194/hess-24-5821-2020, 2020
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Automated water samplers are often used to collect precipitation and streamwater samples for subsequent isotope analysis, but the isotopic signal of these samples may be altered due to evaporative fractionation occurring during the storage inside the autosamplers in the field. In this article we present and evaluate a cost-efficient modification to the Teledyne ISCO automated water sampler that prevents isotopic enrichment through evaporative fractionation of the water samples.
Kolbjørn Engeland, Anna Aano, Ida Steffensen, Eivind Støren, and Øyvind Paasche
Hydrol. Earth Syst. Sci., 24, 5595–5619, https://doi.org/10.5194/hess-24-5595-2020, https://doi.org/10.5194/hess-24-5595-2020, 2020
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We combine systematic, historical, and paleo information to obtain flood information from the last 10 300 years for the Glomma River in Norway. We identify periods with increased flood activity (4000–2000 years ago and the recent 1000 years) that correspond broadly to periods with low summer temperatures and glacier growth. The design floods in Glomma were more than 20 % higher during the 18th century than today. We suggest that trends in flood variability are linked to snow in late spring.
James W. Kirchner, Sarah E. Godsey, Madeline Solomon, Randall Osterhuber, Joseph R. McConnell, and Daniele Penna
Hydrol. Earth Syst. Sci., 24, 5095–5123, https://doi.org/10.5194/hess-24-5095-2020, https://doi.org/10.5194/hess-24-5095-2020, 2020
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Streams and groundwaters often show daily cycles in response to snowmelt and evapotranspiration. These typically have a roughly 6 h time lag, which is often interpreted as a travel-time lag. Here we show that it is instead primarily a phase lag that arises because aquifers integrate their inputs over time. We further show how these cycles shift seasonally, mirroring the springtime retreat of snow cover to higher elevations and the seasonal advance and retreat of photosynthetic activity.
Jasper Foets, Carlos E. Wetzel, Núria Martínez-Carreras, Adriaan J. Teuling, Jean-François Iffly, and Laurent Pfister
Hydrol. Earth Syst. Sci., 24, 4709–4725, https://doi.org/10.5194/hess-24-4709-2020, https://doi.org/10.5194/hess-24-4709-2020, 2020
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Diatoms (microscopic algae) are regarded as useful tracers in catchment hydrology. However, diatom analysis is labour-intensive; therefore, only a limited number of samples can be analysed. To reduce this number, we explored the potential for a time-integrated mass-flux sampler to provide a representative sample of the diatom assemblage for a whole storm run-off event. Our results indicate that the Phillips sampler did indeed sample representative communities during two of the three events.
Leonie Kiewiet, Ilja van Meerveld, Manfred Stähli, and Jan Seibert
Hydrol. Earth Syst. Sci., 24, 3381–3398, https://doi.org/10.5194/hess-24-3381-2020, https://doi.org/10.5194/hess-24-3381-2020, 2020
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The sources of stream water are important, for instance, for predicting floods. The connectivity between streams and different (ground-)water sources can change during rain events, which affects the stream water composition. We investigated this for stream water sampled during four events and found that stream water came from different sources. The stream water composition changed gradually, and we showed that changes in solute concentrations could be partly linked to changes in connectivity.
Lu Zhuo, Qiang Dai, Binru Zhao, and Dawei Han
Hydrol. Earth Syst. Sci., 24, 2577–2591, https://doi.org/10.5194/hess-24-2577-2020, https://doi.org/10.5194/hess-24-2577-2020, 2020
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Soil moisture plays an important role in hydrological modelling. However, most existing in situ observation networks rarely provide sufficient coverage to capture soil moisture variations. Clearly, there is a need to develop a systematic approach, so that with the minimal number of sensors the soil moisture information could be captured accurately. In this study, a simple and low-data requirement method is proposed (WRF, PCA, CA), which can provide very efficient soil moisture estimations.
Abraham J. Gibson, Danielle C. Verdon-Kidd, Greg R. Hancock, and Garry Willgoose
Hydrol. Earth Syst. Sci., 24, 1985–2002, https://doi.org/10.5194/hess-24-1985-2020, https://doi.org/10.5194/hess-24-1985-2020, 2020
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To be better prepared for drought, we need to be able to characterize how they begin, translate to on-ground impacts and how they end. We created a 100-year drought record for an area on the east coast of Australia and compared this with soil moisture and vegetation data. Drought reduces vegetation and soil moisture, but recovery rates are different across different catchments. Our methods can be universally applied and show the need to develop area-specific data to inform drought management.
Clemens Messerschmid, Martin Sauter, and Jens Lange
Hydrol. Earth Syst. Sci., 24, 887–917, https://doi.org/10.5194/hess-24-887-2020, https://doi.org/10.5194/hess-24-887-2020, 2020
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Recharge assessment in the shared transboundary Western Aquifer Basin is highly relevant, scientifically as well as hydropolitically (in Israeli–Palestinian water negotiations). Our unique combination of field-measured soil characteristics and soil moisture time series with soil moisture saturation excess modelling provides a new basis for the spatial differentiation of formation-specific groundwater recharge (at any scale), applicable also in other previously ungauged basins around the world.
J. Nikolaus Callow, Matthew R. Hipsey, and Ryan I. J. Vogwill
Hydrol. Earth Syst. Sci., 24, 717–734, https://doi.org/10.5194/hess-24-717-2020, https://doi.org/10.5194/hess-24-717-2020, 2020
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Secondary dryland salinity is a global land degradation issue. Our understanding of causal processes is adapted from wet and hydrologically connected landscapes and concludes that low end-of-catchment runoff indicates land clearing alters water balance in favour of increased infiltration and rising groundwater that bring salts to the surface causing salinity. This study shows surface flows play an important role in causing valley floor recharge and dryland salinity in low-gradient landscapes.
Nils Michelsen, Gerrit Laube, Jan Friesen, Stephan M. Weise, Ali Bakhit Ali Bait Said, and Thomas Müller
Hydrol. Earth Syst. Sci., 23, 2637–2645, https://doi.org/10.5194/hess-23-2637-2019, https://doi.org/10.5194/hess-23-2637-2019, 2019
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Most commercial automatic rain samplers are costly and do not prevent evaporation from the collection bottles. Hence, we have developed a microcontroller-based collector enabling timer-actuated integral rain sampling. The simple, low-cost device is robust and effectively minimizes post-sampling evaporation. The excellent performance of the collector during an evaporation experiment in a lab oven suggests that even multi-week field deployments in warm climates are feasible.
Michael Engel, Daniele Penna, Giacomo Bertoldi, Gianluca Vignoli, Werner Tirler, and Francesco Comiti
Hydrol. Earth Syst. Sci., 23, 2041–2063, https://doi.org/10.5194/hess-23-2041-2019, https://doi.org/10.5194/hess-23-2041-2019, 2019
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Hydrometric and geochemical dynamics are controlled by interplay of meteorological conditions, topography and geological heterogeneity. Nivo-meteorological indicators (such as global solar radiation, temperature and decreasing snow depth) explain monthly conductivity and isotopic dynamics best. These insights are important for better understanding hydrochemical responses of glacierized catchments under a changing cryosphere.
Andrew D. Wickert, Chad T. Sandell, Bobby Schulz, and Gene-Hua Crystal Ng
Hydrol. Earth Syst. Sci., 23, 2065–2076, https://doi.org/10.5194/hess-23-2065-2019, https://doi.org/10.5194/hess-23-2065-2019, 2019
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Measuring Earth's changing environment is a critical part of natural science, but to date most of the equipment to do so is expensive, proprietary, and difficult to customize. We addressed this challenge by developing and deploying the ALog, a low-power, lightweight, Arduino-compatible data logger. We present our hardware schematics and layouts, as well as our customizable code library that operates the ALog and helps users to link it to off-the-shelf sensors.
Bruce C. Scott-Shaw and Colin S. Everson
Hydrol. Earth Syst. Sci., 23, 1553–1565, https://doi.org/10.5194/hess-23-1553-2019, https://doi.org/10.5194/hess-23-1553-2019, 2019
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The research undertaken for this study has allowed for an accurate direct comparison of indigenous and introduced tree water use. The measurements of trees growing in the understorey indicate significant water use in the subcanopy layer. The results showed that individual tree water use is largely inter-species specific. The introduced species remain active during the dry winter periods, resulting in their cumulative water use being significantly greater than that of the indigenous species.
Barbara Glaser, Marta Antonelli, Marco Chini, Laurent Pfister, and Julian Klaus
Hydrol. Earth Syst. Sci., 22, 5987–6003, https://doi.org/10.5194/hess-22-5987-2018, https://doi.org/10.5194/hess-22-5987-2018, 2018
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We demonstrate how thermal infrared images can be used for mapping the appearance and disappearance of water at the surface. The use of thermal infrared images allows for mapping this appearance and disappearance for various temporal and spatial resolutions, and the images can be understood intuitively. We explain the necessary steps in detail, from image acquisition to final processing, by relying on image examples and experience from an 18-month mapping campaign.
Simon Etter, Barbara Strobl, Jan Seibert, and H. J. Ilja van Meerveld
Hydrol. Earth Syst. Sci., 22, 5243–5257, https://doi.org/10.5194/hess-22-5243-2018, https://doi.org/10.5194/hess-22-5243-2018, 2018
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To evaluate the potential value of streamflow estimates for hydrological model calibration, we created synthetic streamflow datasets in various temporal resolutions based on the errors in streamflow estimates of 136 citizens. Our results show that streamflow estimates of untrained citizens are too inaccurate to be useful for model calibration. If, however, the errors can be reduced by training or filtering, the estimates become useful if also a sufficient number of estimates are available.
Doris Duethmann and Günter Blöschl
Hydrol. Earth Syst. Sci., 22, 5143–5158, https://doi.org/10.5194/hess-22-5143-2018, https://doi.org/10.5194/hess-22-5143-2018, 2018
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We analyze changes in catchment evaporation estimated from the water balances of 156 catchments in Austria over 1977–2014, as well as the possible causes of these changes. Our results show that catchment evaporation increased on average by 29 ± 14 mm yr−1 decade−1. We attribute this increase to changes in atmospheric demand (based on reference and pan evaporation), changes in vegetation (quantified by a satellite-based vegetation index), and changes in precipitation.
Arno Hartmann, Marc Luetscher, Ralf Wachter, Philipp Holz, Elisabeth Eiche, and Thomas Neumann
Hydrol. Earth Syst. Sci., 22, 4281–4293, https://doi.org/10.5194/hess-22-4281-2018, https://doi.org/10.5194/hess-22-4281-2018, 2018
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We have developed a new mobile automated water sampling device for environmental research and other applications where waters need to be tested for compliance with environmental/health regulations. It has two main advantages over similar devices: firstly, it injects water samples directly into airtight vials to prevent any change in sample properties through contamination, evaporation and gas exchange. Secondly, it can hold up to 160 sample vials, while other devices only hold up to 24 vials.
Yuedong Guo, Changchun Song, Wenwen Tan, Xianwei Wang, and Yongzheng Lu
Hydrol. Earth Syst. Sci., 22, 1081–1093, https://doi.org/10.5194/hess-22-1081-2018, https://doi.org/10.5194/hess-22-1081-2018, 2018
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The study examined dynamics of DOC export from a permafrost peatland catchment located in northeastern China. The findings indicated that the DOC export is a transport-limited process and the DOC load was significant for the net carbon balance in the studied catchment. The flowpath shift process is key to observed DOC concentration, resources and chemical characteristics in discharge. Permafrost degradation would likely elevate the proportion of microbe-originated DOC in baseflow.
Maurizio Mazzoleni, Vivian Juliette Cortes Arevalo, Uta Wehn, Leonardo Alfonso, Daniele Norbiato, Martina Monego, Michele Ferri, and Dimitri P. Solomatine
Hydrol. Earth Syst. Sci., 22, 391–416, https://doi.org/10.5194/hess-22-391-2018, https://doi.org/10.5194/hess-22-391-2018, 2018
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We investigate the usefulness of assimilating crowdsourced observations from a heterogeneous network of sensors for different scenarios of citizen involvement levels during the flood event occurred in the Bacchiglione catchment in May 2013. We achieve high model performance by integrating crowdsourced data, in particular from citizens motivated by their feeling of belonging to a community. Satisfactory model performance can still be obtained even for decreasing citizen involvement over time.
Daniele P. Viero
Hydrol. Earth Syst. Sci., 22, 171–177, https://doi.org/10.5194/hess-22-171-2018, https://doi.org/10.5194/hess-22-171-2018, 2018
Fayçal Rejiba, Cyril Schamper, Antoine Chevalier, Benoit Deleplancque, Gaghik Hovhannissian, Julien Thiesson, and Pierre Weill
Hydrol. Earth Syst. Sci., 22, 159–170, https://doi.org/10.5194/hess-22-159-2018, https://doi.org/10.5194/hess-22-159-2018, 2018
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The internal variability of paleomeanders strongly influence water fluxes in alluvial plains. This study presents the results of a hydrogeophysical investigation that provide a very detailed characterization of the geometry of a wide paleomeander. The presented case study, situated in the Seine River basin (France), represents a common sedimentary and geomorphological structure in alluvial plains worldwide.
Sibylle Kathrin Hassler, Markus Weiler, and Theresa Blume
Hydrol. Earth Syst. Sci., 22, 13–30, https://doi.org/10.5194/hess-22-13-2018, https://doi.org/10.5194/hess-22-13-2018, 2018
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We use sap velocity measurements from 61 trees on 132 days to gain knowledge about the controls of landscape-scale transpiration, distinguishing tree-, stand- and site-specific controls on sap velocity and sap flow patterns and examining their dynamics during the vegetation period. Our results show that these patterns are not exclusively determined by tree characteristics. Thus, including site characteristics such as geology and aspect could be beneficial for modelling or management purposes.
Paul Floury, Jérôme Gaillardet, Eric Gayer, Julien Bouchez, Gaëlle Tallec, Patrick Ansart, Frédéric Koch, Caroline Gorge, Arnaud Blanchouin, and Jean-Louis Roubaty
Hydrol. Earth Syst. Sci., 21, 6153–6165, https://doi.org/10.5194/hess-21-6153-2017, https://doi.org/10.5194/hess-21-6153-2017, 2017
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We present a new prototype
lab in the fieldnamed River Lab (RL) designed for water quality monitoring to perform a complete analysis at sub-hourly frequency of major dissolved species in river water. The article is an analytical paper to present the proof of concept, its performances and improvements. Our tests reveal a significant improvement of reproducibility compared to conventional analysis in the laboratory. First results are promising for understanding the critical zone.
Vladimir P. Shevchenko, Oleg S. Pokrovsky, Sergey N. Vorobyev, Ivan V. Krickov, Rinat M. Manasypov, Nadezhda V. Politova, Sergey G. Kopysov, Olga M. Dara, Yves Auda, Liudmila S. Shirokova, Larisa G. Kolesnichenko, Valery A. Zemtsov, and Sergey N. Kirpotin
Hydrol. Earth Syst. Sci., 21, 5725–5746, https://doi.org/10.5194/hess-21-5725-2017, https://doi.org/10.5194/hess-21-5725-2017, 2017
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We used a coupled hydrological–hydrochemical approach to assess the impact of snow on river and lake water chemistry across a permafrost gradient in very poorly studied Western Siberia Lowland (WSL), encompassing > 1.5 million km2. The riverine springtime fluxes of major and trace element in WSL rivers might be strongly overestimated due to previously unknown input from the snow deposition.
Cited articles
Ala-aho, P., Rossi, P. M., and Kløve, B.: Interaction of esker groundwater
with headwater lakes and streams, J. Hydrol., 500, 144–156,
https://doi.org/10.1016/j.jhydrol.2013.07.014, 2013.
Ala-aho, P., Rossi, P. M., Isokangas, E., and Kløve, B.: Fully integrated
surface–subsurface flow modelling of groundwater–lake interaction in an
esker aquifer: Model verification with stable isotopes and airborne thermal
imaging, J. Hydrol., 522, 391–406,
https://doi.org/10.1016/j.jhydrol.2014.12.054, 2015a.
Ala-aho, P., Rossi, P. M., and Kløve, B.: Estimation of temporal and spatial variations in groundwater recharge in unconfined sand aquifers using Scots pine inventories, Hydrol. Earth Syst. Sci., 19, 1961–1976, https://doi.org/10.5194/hess-19-1961-2015, 2015b.
Anderson, M. P. and Munter, J. A.: Seasonal reversals of groundwater flow
around lakes and the relevance to stagnation points and lake budgets, Water
Resour. Res., 17, 1139–1150, https://doi.org/10.1029/WR017i004p01139, 1981.
Arnoux, M., Barbecot, F., Gibert-Brunet, E., Gibson, J., Rosa, E., Noret, A.
and Monvoisin, G.: Geochemical and isotopic mass balances of kettle lakes in
southern Quebec (Canada) as tools to document variations in groundwater
quantity and quality, Environ. Earth Sci., 76, 106,
https://doi.org/10.1007/s12665-017-6410-6, 2017a.
Arnoux, M., Gibert-Brunet, E., Barbecot, F., Guillon, S., Gibson, J., and
Noret, A.: Interactions between groundwater and seasonally ice-covered
lakes: using water stable isotopes and radon-222 multi-layer mass balance
models, Hydrol. Process., 31, 2566–2581, https://doi.org/10.1002/hyp.11206, 2017b.
Bennett, D. M., Fritz, S. C., Holz, J. C., and Zlotnik, V. A.: Evaluating
climatic and non-climatic influences on ion chemistry in natural and
man-made lakes of Nebraska, USA, Hydrobiologia, 591, 103–115,
https://doi.org/10.1007/s10750-007-0798-z, 2007.
Bertrand, G., Siergieiev, D., Ala-Aho, P., and Rossi, P. M.: Environmental
tracers and indicators bringing together groundwater, surface water and
groundwater dependent ecosystems: importance of scale in choosing relevant
tools, Environ. Earth Sci., 7, 813–827,
https://doi.org/10.1007/s12665-013-3005-8, 2014.
Birks, S. J., Edwards, T. W. D., Gibson, J. J., Michel, F. A., Drimmie, R. J.,
MacTavish, D., Remenda, V. H., and Wassenaar, L. I.: Canadian Network for
Isotopes in Precipitation, University of Waterloo, Ontario, Canada,
available at: http://science.uwaterloo.ca/~twdedwar/cnip/cniphome.html, last access: 23 May 2015.
Born, S. M., Smith, S. A., and Stephenson, D. A.: Hydrogeology of
glacial-terrain lakes, with management and planning applications, J.
Hydrol., 43, 7–43, https://doi.org/10.1016/0022-1694(79)90163-X, 1979.
Bouchard, F., Turner, K. W., MacDonald, L. A., Deakin, C., White, H.,
Farquharson, N., Medeiros, A. S., Wolfe, B. B., Hall, R. I., Pienitz, R., and
Edwards, T. W. D.: Vulnerability of shallow subarctic lakes to evaporate and
desiccate when snowmelt runoff is low, Geophys. Res. Lett., 40, 6112–6117,
https://doi.org/10.1139/as-2016-0019, 2013.
Cloutier, V., Veillette, J., Roy, M., Bois, D., Gagnon, F., and de Corta, H.:
Atlas sur les eaux souterraines de la MRC d'Abitibi, Université du
Québec en Abitibi-Témiscamingue, Québec, Canada, 24 pp., 36
maps, 2007.
Cloutier, V., Blanchette, D., Dallaire, P.-L., Nadeau, S., Rosa, E., and Roy,
M.: Projet d'acquisition de connaissances sur les eaux souterraines de
l'Abitibi-Témiscamingue (partie 1) [Abitibi-Témiscamingue
groundwater knowledge acquisition project, Part 1], Rapport final [Final
Report], Amos: Groupe de recherche sur l'eau souterraine. Institut de
recherche en mines et en environnement. Université du Québec en
Abitibi-Témiscamingue, Québec, Canada, 151 pp., 2013.
Cochrane, L. B.: Technical report on the Aquarius Project, Timmins, Ontario,
Canada, St. Andrew Goldfields LTD, 129 pp., 2006.
Cohen, M. J., Creed, I. F., Alexander, L., Basu, N. B., Calhoun, A. J. K., Craft,
C., D'Amico, E., DeKeyser, E., Fowler, L., Golden, H. E., Jawitz, J. W.,
Kalla, P., Kirkman, L. K., Lane, C. R., Lang, M., Leibowitz, S. G., Lewis,
D. B., Marton, J., McLaughlin, D. L., Mushet, D. M., Raanan-Kiperwas, H.,
Rains, M. C., Smith, L., and Walls, S. C.: Do geographically isolated wetlands
influence landscape functions?, P. Natl. Acad. Sci. USA, 113, 1978–1986,
https://doi.org/10.1073/pnas.1512650113, 2016.
Craig, H. and Gordon, L. I.: Deuterium and Oxygen-18 Variations in the Ocean
and the Marine Atmosphere, in: Stable Isotopes in Oceanographic Studies and
Paleotemperatures, edited by: Tongiorgi, E., Laboratorio di geologia
nucleare, Pisa, Italy, 9–130, 1965.
Cummings, D. I., Gorrell, G., Guilbault, J.-P., Hunter, J. A., Logan, C.,
Ponomarenko, D., Pugin, A. J.-M., Pullan, S. E., Russell, H. A. J., and Sharpe,
D. R.: Sequence stratigraphy of a glaciated basin fill, with a focus on esker
sedimentation, Geol. Soc. Am. Bull., 123, 1478–1496,
https://doi.org/10.1130/B30273.1, 2011.
Darling, W. G., Bath, A. H., Gibson, J. J., and Rozanski, K.: Isotopes in Water,
in: Isotopes in Palaeoenvironmental Research, edited by: Leng, M. J.,
Springer, Dordrecht, the Netherlands, 1–66, 2005.
Dyke, A. S.: An outline of North American deglaciation with emphasis on
central and northern Canada, in: Quaternary glaciations – extent and
chronology, part II: North America, Developments in Quaternary Science 2b,
edited by: Ehlers, J. and Gibard, P. L., Elsevier, Amsterdam, the
Netherlands, 373–424, 2004.
Environment Canada: Historical climate data for Timmins, Ontario, available
at: http://climate.weather.gc.ca/historical_data/search_historic_data_e.html, last access: 6 June 2015.
Fleckenstein, J. H., Krause, S., Hannah, D. M., and Boano, F.:
Groundwater-surface water interactions: new methods and models to improve
understanding of processes and dynamics, Adv. Water Resour., 33, 1291–1295,
https://doi.org/10.1016/j.advwatres.2010.09.011, 2010.
Fritz, S. C., Ito, E., Yu, Z., Laird, K., and Engstrom, D. R.: Hydrologic
variation in the Northern Great Plains during the last two millennia,
Quaternary Res., 53, 175–184, https://doi.org/10.1006/qres.1999.2115, 2000.
Gazis, C. and Feng, X.: A stable isotope study of soil water: evidence for
mixing and preferential flow paths, Geoderma, 119, 97–111,
https://doi.org/10.1016/S0016-7061(03)00243-X, 2004.
Gibson, J. J.: A new conceptual model for predicting isotope enrichment of
lakes in seasonal climates, PAGES News, 10, 10–11,
https://doi.org/10.22498/pages.10.2.10, 2002.
Gibson, J. J. and Edwards, T. W. D.: Regional surface water balance and
evaporation–transpiration partitioning from a stable isotope survey of
lakes in northern Canada, Global Biogeochem. Cy., 16, 1–14,
https://doi.org/10.1029/2001GB001839, 2002.
Gibson, J. J., Edwards, T. W. D., Bursey, G. G., and Prowse, T. D.: Estimating
evaporation using stable isotopes: quantitative results and sensitivity
analysis for two catchments in northern Canada, Nord. Hydrol., 24, 79–94,
https://doi.org/10.2166/nh.1993.0015, 1993.
Gibson, J. J., Birks, S. J., and Edwards, T. W. D.: Global prediction of δA and δ2H-δ18O evaporation slopes for lakes
and soil water accounting for seasonality, Global Biogeochem. Cy., 22,
GB2031, https://doi.org/10.1029/2007GB002997, 2008.
Gonfiantini, R.: Environmental isotopes in lake studies, in: Handbook of
Environmental Isotope Geochemistry, Vol. 2, The Terrestrial Environment,
edited by: Fritz, B. P. and Fontes, J. C., Elsevier, Amsterdam, the
Netherlands, 113–168, 1986.
Gorham, E., Dean, W. E., and Sanger, J. E.: The chemical composition of lakes
in the north-central United States, Limnol. Oceanogr., 28, 287–301,
https://doi.org/10.4319/lo.1983.28.2.0287, 1983.
Granger, R. J. and Hedstrom, N.: Modelling hourly rates of evaporation from small lakes, Hydrol. Earth Syst. Sci., 15, 267–277, https://doi.org/10.5194/hess-15-267-2011, 2011.
Gurrieri, J. T. and Furniss, G.: Estimation of groundwater exchange in
alpine lakes using non-steady mass-balance methods, J. Hydrol., 297,
187–208, https://doi.org/10.1016/j.jhydrol.2004.04.021, 2004.
Horita, J. and Wesolowski, D.: Liquid-vapour fractionation of oxygen and
hydrogen isotopes of water from the freezing to the critical temperature,
Geochim. Cosmochim. Ac., 58, 3425–3437,
https://doi.org/10.1016/0016-7037(94)90096-5, 1994.
Isokangas, E., Rozanski, K., Rossi, P. M., Ronkanen, A.-K., and Kløve, B.: Quantifying groundwater dependence of a sub-polar lake cluster in Finland using an isotope mass balance approach, Hydrol. Earth Syst. Sci., 19, 1247–1262, https://doi.org/10.5194/hess-19-1247-2015, 2015.
Katz, B. G., Coplen, T. B., Bullen, T. D., and Davis, J. H.: Use of chemical and
isotopic tracers to characterize the interactions between ground water and
surface water in mantled karst, Ground Water, 35, 1014–1028,
https://doi.org/10.1111/j.1745-6584.1997.tb00174.x, 1997.
Kendall, C. and Caldwell, E. A.: Fundamentals of Isotope Geochemistry, in:
Isotope Tracers in Catchment Hydrology, edited by: Kendall, C. and McDonnell
J. J., Elsevier Science B.V., Amsterdam, the Netherlands, 51–86, 1998.
Kenoyer, G. J. and Anderson, M. P.: Groundwater's dynamic role in regulating
acidity and chemistry in a precipitation-dominated lake, J. Hydrol., 109,
287–306, https://doi.org/10.1016/0022-1694(89)90020-6, 1989.
Kløve, B., Ala-aho, P., Bertrand, G., Boukalova, Z., Ertürk, A.,
Goldscheider, N., Ilmonen, J., Karakaya, N., Kupfersberger, H., Kværner,
J., Lundberg, A., Mileusnic, M., Moszczynska, A., Muotka, T., Preda, E.,
Rossi, P., Siergieiev, D., Šimek, J., Wachniew, P., and Widerlund, A.:
Groundwater dependent ecosystems: Part I – Hydroecology, threats and status
of ecosystems, Environ. Sci. Policy, 14, 770–781,
https://doi.org/10.1016/j.envsci.2011.04.002, 2011.
Knoll, L. B., Hagenbuch, E. J., Stevens, M. H., Vanni, M. J., Renwick, W. H.,
Denlinger, J. C., Hale, R. S., and González, M. J.: Predicting
eutrophication status in reservoirs at large spatial scales using landscape
and morphometric variables, Inland Waters, 5, 203–214,
https://doi.org/10.5268/IW-5.3.812, 2015.
Kratz, T., Webster, K., Bowser, C., Magnuson, J., and Benson, B.: The
influence of landscape position on lakes in northern Wisconsin, Freshwater
Biol., 37, 209–217, https://doi.org/10.1046/j.1365-2427.1997.00149.x, 1997.
LaBaugh, J. W., Winter, T. C., Rosenberry, D. O., Schuster, P. F., Reddy, M. M.,
and Aitken, G. R.: Hydrological and chemical estimates of the water balance
of a closed-basin lake in north central Minnesota, Water Resour. Res., 33,
2799–2812, https://doi.org/10.1029/97WR02427, 1997.
Laird, K. R., Haig, H. A., Ma, S., Kingsbury, M. V., Brown, T. A., Lewis,
C. F. M., Oglesby, R. J., and Cumming, B. F.: Expanded spatial extent of the
Medieval Climate Anomaly revealed in lake-sediment records across the boreal
region in northwest Ontario, Glob. Change Biol., 18, 2869–2881,
https://doi.org/10.1111/j.1365-2486.2012.02740.x, 2012.
Lewandowski, J., Meinikmann, K., Nützmann, G. and Rosenberry, D. O.: Groundwater – the disregarded component in lake water and nutrient budgets.
Part 2: effects of groundwater on nutrients, Hydrol. Process., 29,
2922–2955, https://doi.org/10.1002/hyp.10384, 2015.
Louiseize, N. L., Lafrenière, M. J., and Hastings, M. J.: Stable isotopic
evidence of enhanced export of microbially derived NO3 following active
layer slope disturbance in the Canadian High Arctic, Biogeochemistry, 121,
565–580, https://doi.org/10.1007/s10533-014-0023-x, 2014.
Martin, S. L. and Soranno, P. A.: Lake landscape position: relationships to
hydrologic connectivity and landscape features, Limnol. Oceanogr., 51,
801–814, https://doi.org/10.4319/lo.2006.51.2.0801, 2006.
Martin, S. L., Soranno, P. A., Bremigan, M. T., and Cheruvelil, K. S.: Comparing
hydrogeomorphic approaches to lake classification, Environ. Manage.,
48, 957–974, https://doi.org/10.1007/s00267-011-9740-2, 2011.
Mulholland, P. J.: Large scale patterns of dissolved organic carbon
concentration, flux and sources, in: Aquatic Ecosystems: Interactivity of
Dissolved Organic Matter, edited by: Findlay, S. E. G. and Sinsabaugh, R. L.,
Elsevier Science, San Diego, California, USA, 139–160, 2003.
Natural Resources Canada: GeoGratis (version 2.1):
available at: http://geogratis.cgdi.gc.ca/, 30 August 2019.
Newton, R. M. and Driscoll, C. T.: Classification of ALSC lakes, in:
Adriondack Lakes Survey: An Interpretive Analysis of Fish Communities and
Water Chemistry, 1984-87, edited by: Baker, J. P., Gherini, S. A., Munson,
R. K., Christensen, S. W., Driscoll, C. T., Gallagher, J., Newton, R. M.,
Reckhow, K. H., and Schofield, C. L., Adriondack Lakes Survey Corporation, Ray
Brook, New York, USA, 270–291, 1990.
Okkonen, J. and Kløve, B.: A sequential modelling approach to assess
groundwater–surface water resources in a snow dominated region of Finland,
J. Hydrol., 411, 91–107, https://doi.org/10.1016/j.jhydrol.2011.09.038,
2011.
Ontario Ministry of Natural Resources and Forestry: Fish ON-Line,
available at: https://www.gisapplication.lrc.gov.on.ca/FishONLine/Index.html?site=FishONLine&viewer=FishONLine&locale=en-US,
last access: 23 October 2011.
Ontario Ministry of Northern Development and Mines: Soils of
Timmins-Noranda-Rouyn area: soil survey report No 46, available at:
http://www.geologyontario.mndm.gov.on.ca/, last access: 19 October 2013.
Quinlan, R., Paterson, A. M., Hall, R. I., Dillon, P. J., Wilkinson, A. N.,
Cumming, B. F., Douglas, M. S. V., and Smol, J. P.: A landscape approach to
examining spatial patterns of limnological variables and long-term
environmental change in a southern Canadian lake district, Freshwater Biol.,
48, 1676–1697, https://doi.org/10.1046/j.1365-2427.2003.01105.x, 2003.
Rautio, A. and Korkka-Niemi, K.: Characterization of groundwater–lake water
interactions at Pyhäjärvi, a lake in SW Finland, Boreal Environ.
Res., 16, 363–380, https://doi.org/10.1108/14777831211204958, 2011.
Rey, N., Rosa, E., Cloutier, V., and Lefebvre, R.: Using water stable
isotopes for tracing surface and groundwater flow systems in the
Barlow-Ojibway Clay Belt, Quebec, Canada, Can. Water Resour. J., 43,
173–194, https://doi.org/10.1080/07011784.2017.1403960, 2018.
Richard, J. A. and McClenaghan, M. B.: Quaternary geology of the Porquis
Junction area, Ontario Geological Survey, Map 2659, scale 1:50000, 2000.
Rosenberry, D. O., Lewandowski, J., Meinikmann, K., and Nützmann, G.:
Groundwater – the disregarded component in lake water and nutrient budgets.
Part 1: effects of groundwater on hydrology, Hydrol. Process., 29,
2895–2921, https://doi.org/10.1002/hyp.10403, 2015.
Rossi, P. M., Ala-aho, P., Ronkanen, A., and Kløve, B.: Groundwater-surface
water interaction between an esker aquifer and a drained fen, J. Hydrol.,
432–433, 52–60, https://doi.org/10.1016/j.jhydrol.2012.02.026, 2012.
Roy, M., Dell'Oste, F., Veillette, J. J., de Vernal, A., Hélie, J.-F., and
Parent, M.: Insights on the events surrounding the final drainage of Lake
Ojibway based on James Bay stratigraphic sequences, Quaternary Sci. Rev., 30, 682–692,
https://doi.org/10.1016/j.quascirev.2010.12.008, 2011.
Schuster, P. F., Reddy, M. M., LaBaugh, J. W., Parkhurst, R. S., Rosenberry,
D. O., Winter, T. C., Antweiler, R. C., and Dean, W. E.: Characterization of lake
water and ground water movement in the littoral zone of Williams Lake, a
closed-basin lake in north central Minnesota, Hydrol. Process., 17,
823–838, https://doi.org/10.1002/hyp.1211, 2003.
Sebestyen, S. D. and Schneider, R. L.: Dynamic temporal patterns of nearshore
seepage flux in a headwater Adirondack lake, J. Hydrol., 247, 137–150,
https://doi.org/10.1016/S0022-1694(01)00377-8, 2001.
Skrzypek, G., Mydłowski, A., Dogramaci, S., Hedley, P., Gibson, J., and Grierson, P.: Estimation of evaporative loss based on the stable isotope
composition of water using “Hydrocalculator”, J. Hydrol., 523, 781–789,
https://doi.org/10.1016/j.jhydrol.2015.02.010, 2015.
Smerdon, B. D., Devito, K. J., and Mendoza, C. A.: Interaction of groundwater
and shallow lakes on outwash sediments in the subhumid Boreal Plains region,
J. Hydrol., 314, 246–262, https://doi.org/10.1016/j.jhydrol.2005.04.001,
2005.
Smerdon, B. D., Devito, K. J., and Mendoza, C. A.: Simulations of fully coupled
lake-groundwater exchange in a subhumid climate with an integrated
hydrologic model, Water Resour. Res., 43, W01416,
https://doi.org/10.1029/2006WR005137, 2007.
Stauffer, R. E. and Wittchen, B. D.: Hydrogeochemistry of Maine seepage lakes
and related groundwaters, J. Hydrol., 138, 559–581,
https://doi.org/10.1016/0022-1694(92)90137-K, 1992.
Thorslund, J., Cohen, M. J., Jawitz, J. W., Destouni, G., Creed, I. F., Rains,
M. C., Badiou, P., and Jarsjö, J.: Solute Evidence for Hydrological
Connectivity of Geographically Isolated Wetlands, Land Degrad. Dev., 29,
3954–3962, https://doi.org/10.1002/ldr.3145, 2018.
Tóth, J.: A theoretical analysis of groundwater flow in small drainage
basins, J. Geophys. Res., 68, 4795–4812,
https://doi.org/10.1029/JZ068i016p04795, 1963.
Tondu, J. M., Turner, K. W., Wolfe, B. B., Hall, R. I., Edwards, T. W. D., and
McDonald, I.: Using water isotope tracers to develop the hydrological
component of a long-term aquatic ecosystem monitoring program for a northern
lake-rich landscape, Arct. Antarct. Alp. Res., 45, 594–614,
https://doi.org/10.1657/1938-4246-45.4.594, 2013.
Turner, J. V. and Townley, L. R.: Determination of groundwater flow-through
regimes of shallow lakes and wetlands from numerical analysis of stable
isotope and chloride tracer distribution patterns, J. Hydrol., 320, 451–483,
https://doi.org/10.1016/j.jhydrol.2005.07.050, 2006.
Turner, K. W., Wolfe, B. B., and Edwards, T. W. D.: Characterizing the role of
hydrological processes on lake water balances in the Old Crow Flats, Yukon
Territory, Canada, using water isotope tracers, J. Hydrol., 386, 103–117,
https://doi.org/10.1016/j.jhydrol.2010.03.012, 2010.
Turner, K. W., Edwards, T. W. D., and Wolfe, B. B.: Characterizing runoff
generation processes in a lake-rich thermokarst landscape (Old Crow Flats,
Yukon, Canada) using δ18O, δ2H and d-excess
measurements, Permafrost Periglac., 25, 53–59,
https://doi.org/10.1002/ppp.1802, 2014a.
Turner, K. W., Wolfe, B. B., Edwards, T. W. D., Lantz, T. C., Hall, R. I., and
Larocque, G.: Controls on water balance of shallow thermokarst lakes and
their relations with catchment characteristics: a multi-year,
landscape-scale assessment based on water isotope tracers and remote sensing
in Old Crow Flats, Yukon (Canada), Glob. Change Biol., 20, 1585–1603,
https://doi.org/10.1111/gcb.12465, 2014b.
Webster, K. E., Kratz, T. K., Bowser, C. J., Magnuson, J. J., and Rose, W. J.: The
influence of landscape position on lake chemical responses to drought in
northern Wisconsin, Limnol. Oceanogr., 41, 977–984,
https://doi.org/10.4319/lo.1996.41.5.0977, 1996.
Webster, K. E., Soranno, P. A., Baines, S. B., Kratz, T. K., Bowser, C. J.,
Dillon, P. J., Campbell, P., Fee, E. J., and Hecky, R. E.: Structuring features
of lake districts: landscape controls on lake chemical responses to drought,
Freshwater Biol., 43, 499–515,
https://doi.org/10.1046/j.1365-2427.2000.00571.x, 2000.
Winter, T. C.: Numerical simulation analysis of the interaction of lakes and
groundwater, United States Geological Survey Professional Papers, 1001,
https://doi.org/10.3133/pp1001, 1976.
Winter, T. C.: Classification of the hydrologic setting of lakes in the north
central United States, Water Resour. Res., 13, 753–767,
https://doi.org/10.1029/WR013i004p00753, 1977.
Winter, T. C.: Relation of streams, lakes, and wetlands to groundwater flow
systems, Hydrogeol. J., 7, 28–45, https://doi.org/10.1007/s100400050178,
1999.
Winter, T. C., Harvey, J. W., Franke, O. L., and Alley, W. W.: Ground water and
surface water: a single resource, in: U.S. Geological Survey Circular 1139,
U.S. Geological Survey, Denver, Colorado, USA, 1998.
Winter, T. C., Rosenberry, D. O., and LaBaugh, J. W.: Where does the ground
water in small watersheds come from?, Ground Water, 41, 989–1000,
https://doi.org/10.1111/j.1745-6584.2003.tb02440.x, 2003.
Wolfe, B. B., Karst-Riddoch, T. L., Hall, R. I., Edwards, T. W. D., English,
M. C., Palmini, R., McGowan, S., and Vardy, S. R.: Classification of hydrologic
regimes of northern floodplain basins (Peace-Athabasca Delta, Canada) from
analysis of stable isotopes (δ18O, δ2H) and water
chemistry, Hydrol. Process., 21, 151–168, https://doi.org/10.1002/hyp.6229,
2007.
Yi, Y., Brock, B. E., Falcone, M. D., Wolfe, B. B., and Edwards, T. W. D.: A
coupled isotope tracer method to characterize input water to lakes, J.
Hydrol., 350, 1–13, https://doi.org/10.1016/j.jhydrol.2007.11.008, 2008.
Short summary
The investigation of groundwater–lake-water interactions in highly permeable boreal terrain using several indicators showed that lowland lakes are embedded into the groundwater system and are thus relatively resilient to short-term hydroclimatic change, while upland lakes rely more on precipitation as their main water input, making them more sensitive to evaporative drawdown. This suggests that landscape position controls the vulnerability of lake-water levels to hydroclimatic change.
The investigation of groundwater–lake-water interactions in highly permeable boreal terrain...