Articles | Volume 11, issue 4
https://doi.org/10.5194/essd-11-1567-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-11-1567-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Data description paper
| 
22 Oct 2019
Data description paper |
| 22 Oct 2019
| 22 Oct 2019
Co-located contemporaneous mapping of morphological, hydrological, chemical, and biological conditions in a 5th-order mountain stream network, Oregon, USA
O'Neill School of Public and Environmental Affairs, Indiana
University, Bloomington, Indiana, USA
Jay P. Zarnetske
Department of Earth and Environmental Sciences, Michigan State
University, East Lansing, Michigan, USA
Viktor Baranov
LMU Munich Biocenter, Department of Biology II, Großhaderner Str.
2, 82152 Planegg-Martinsried, Germany
Phillip J. Blaen
School of Geography, Earth & Environmental Sciences, University of
Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Birmingham Institute of Forest Research (BIFoR), University of
Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Yorkshire Water, Halifax Road, Bradford, BD6 2SZ, UK
Nicolai Brekenfeld
School of Geography, Earth & Environmental Sciences, University of
Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Rosalie Chu
Environmental Molecular Sciences Laboratory, Pacific Northwest
National Laboratory, Richland, WA, USA
Romain Derelle
Environmental Genomics Group, School of Biosciences, University
of Birmingham, Birmingham B15 2TT, UK
Jennifer Drummond
School of Geography, Earth & Environmental Sciences, University of
Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Integrative Freshwater Ecology Group, Centre for Advanced Studies of
Blanes (CEAB-CSIC), Blanes, Spain
Jan H. Fleckenstein
Dept. of Hydrogeology, Helmholtz Center for Environmental Research – UFZ, Permoserstraße 15, 04318 Leipzig, Germany
Bayreuth Center of Ecology and Environmental Research, University of
Bayreuth, 95440 Bayreuth, Germany
Vanessa Garayburu-Caruso
Earth and Biological Sciences Division, Pacific Northwest National
Laboratory, Richland, WA, USA
Emily Graham
Earth and Biological Sciences Division, Pacific Northwest National
Laboratory, Richland, WA, USA
David Hannah
School of Geography, Earth & Environmental Sciences, University of
Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Ciaran J. Harman
Department of Environmental Health and Engineering, Johns Hopkins
University, Baltimore, Maryland, USA
Skuyler Herzog
O'Neill School of Public and Environmental Affairs, Indiana
University, Bloomington, Indiana, USA
Jase Hixson
O'Neill School of Public and Environmental Affairs, Indiana
University, Bloomington, Indiana, USA
Julia L. A. Knapp
Department of Environmental Systems Science, ETH Zürich,
Zurich, Switzerland
Center for Applied Geoscience, University of Tübingen,
Tübingen, Germany
Stefan Krause
School of Geography, Earth & Environmental Sciences, University of
Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Marie J. Kurz
Dept. of Hydrogeology, Helmholtz Center for Environmental Research – UFZ, Permoserstraße 15, 04318 Leipzig, Germany
The Academy of Natural Sciences of Drexel University,
Philadelphia, Pennsylvania, USA
Jörg Lewandowski
Leibniz-Institute of Freshwater Ecology and Inland Fisheries,
Department Ecohydrology, Müggelseedamm 310, 12587 Berlin, Germany
Humboldt University Berlin, Geography Department, Rudower Chaussee
16, 12489 Berlin, Germany
Angang Li
Department of Civil and Environmental Engineering, Northwestern
University, Evanston, Illinois, USA
Eugènia Martí
Integrative Freshwater Ecology Group, Centre for Advanced Studies of
Blanes (CEAB-CSIC), Blanes, Spain
Melinda Miller
O'Neill School of Public and Environmental Affairs, Indiana
University, Bloomington, Indiana, USA
Alexander M. Milner
School of Geography, Earth & Environmental Sciences, University of
Birmingham, Edgbaston, Birmingham, B15 2TT, UK
Kerry Neil
O'Neill School of Public and Environmental Affairs, Indiana
University, Bloomington, Indiana, USA
Luisa Orsini
Environmental Genomics Group, School of Biosciences, University
of Birmingham, Birmingham B15 2TT, UK
Aaron I. Packman
Department of Civil and Environmental Engineering, Northwestern
University, Evanston, Illinois, USA
Stephen Plont
Department of Earth and Environmental Sciences, Michigan State
University, East Lansing, Michigan, USA
Department of Biological Sciences, Virginia Polytechnic Institute
and State University, Blacksburg, Virginia, USA
Lupita Renteria
Pacific Northwest National Laboratory, Richland, WA, USA
Kevin Roche
Department of Civil & Environmental Engineering & Earth
Sciences, University of Notre Dame, Notre Dame, IN, USA
Todd Royer
O'Neill School of Public and Environmental Affairs, Indiana
University, Bloomington, Indiana, USA
Noah M. Schmadel
O'Neill School of Public and Environmental Affairs, Indiana
University, Bloomington, Indiana, USA
Earth System Processes Division, U.S. Geological Survey, Reston,
Virginia, USA
Catalina Segura
Forest Engineering, Resources, and Management, Oregon State
University Corvallis, OR, USA
James Stegen
Earth and Biological Sciences Division, Pacific Northwest National
Laboratory, Richland, WA, USA
Jason Toyoda
Environmental Molecular Sciences Laboratory, Pacific Northwest
National Laboratory, Richland, WA, USA
Jacqueline Hager
Pacific Northwest National Laboratory, Richland, WA, USA
Nathan I. Wisnoski
Department of Biology, Indiana University, Bloomington, Indiana, USA
Steven M. Wondzell
USDA Forest Service, Pacific Northwest Research Station, Corvallis,
Oregon, USA
Related authors
No articles found.
Álvaro Pardo-Álvarez, Jan H. Fleckenstein, Kalliopi Koutantou, and Philip Brunner
EGUsphere, https://doi.org/10.5194/egusphere-2025-3521, https://doi.org/10.5194/egusphere-2025-3521, 2025
This preprint is open for discussion and under review for Geoscientific Model Development (GMD).
Short summary
Short summary
An upgraded version of a numerical solver is introduced to better capture the three-dimensional interactions between surface water and groundwater. Built using open-source software, it adds new features to handle the complexity of real environments, including the representation of subsurface geology and the simulation of diverse dynamic processes, such as solute transport and heat transfer, in both domains. A test case and a full description of the novel features are provided in this paper.
Julia L. A. Knapp, Wouter R. Berghuijs, Marius G. Floriancic, and James W. Kirchner
Hydrol. Earth Syst. Sci., 29, 3673–3685, https://doi.org/10.5194/hess-29-3673-2025, https://doi.org/10.5194/hess-29-3673-2025, 2025
Short summary
Short summary
This study explores how streams react to rain and how water travels through the landscape to reach them, two processes rarely studied together. Using detailed data from two temperate areas, we show that streams respond to rain much faster than rainwater travels to them. Wetter conditions lead to stronger runoff by releasing older stored water, while heavy rainfall moves newer rainwater to streams faster. These findings offer new insights into how water moves through the environment.
Xue Ping, Zhang Wen, Yang Xian, Menggui Jin, and Stefan Krause
EGUsphere, https://doi.org/10.5194/egusphere-2025-2631, https://doi.org/10.5194/egusphere-2025-2631, 2025
This preprint is open for discussion and under review for Hydrology and Earth System Sciences (HESS).
Short summary
Short summary
Bedform migration affects hyporheic exchange, its impact on surface-groundwater mixing and groundwater-borne contaminant removal in groundwater-fed streams remained unclear. This study numerically simulated how bedform migration influences mixing and mixing-induced nitrate reduction. In fine-to-medium sands, higher bedform migration celerities reshape mixing zones, enhance mixing flux and extent, but reduce nitrate removal rate and efficiency, thus impairing hyporheic purification capacity.
Pia Ebeling, Andreas Musolff, Rohini Kumar, Andreas Hartmann, and Jan H. Fleckenstein
Hydrol. Earth Syst. Sci., 29, 2925–2950, https://doi.org/10.5194/hess-29-2925-2025, https://doi.org/10.5194/hess-29-2925-2025, 2025
Short summary
Short summary
Groundwater is a crucial resource at risk due to droughts. To understand drought effects on groundwater levels in Germany, we grouped 6626 wells into six regional and two national patterns. Weather explained half of the level variations with varied response times. Shallow groundwater responds fast and is more vulnerable to short droughts (a few months). Dampened deep heads buffer short droughts but suffer from long droughts and recoveries. Two nationwide trend patterns were linked to human water use.
Sudhanshu Dixit, Sumit Sen, Tahmina Yasmin, Kieran Khamis, Debashish Sen, Wouter Buytaert, and David Hannah
EGUsphere, https://doi.org/10.5194/egusphere-2025-2081, https://doi.org/10.5194/egusphere-2025-2081, 2025
This preprint is open for discussion and under review for Natural Hazards and Earth System Sciences (NHESS).
Short summary
Short summary
Flash floods are becoming more frequent in mountainous regions due to heavier rainstorms. To protect people and property, we are working to better understand local hydrology and improve the efficiency of early warning systems for urban flooding in Lesser Himalayas. By combining community knowledge, low-cost technology, we can enhance understanding of flood dynamics and strengthen preparedness in mountains. This work is a step toward building resilience by bridging science and community insight.
Mortimer L. Bacher, Julian Klaus, Adam S. Ward, Jasmine Krause, Catalina Segura, and Clarissa Glaser
EGUsphere, https://doi.org/10.5194/egusphere-2025-1625, https://doi.org/10.5194/egusphere-2025-1625, 2025
Short summary
Short summary
Slug tracer experiments are biased toward faster flow paths, underscoring the need for tracers that reveal temporally longer timescales. We explore integrating solute tracers with naturally occurring radon to quantify flow paths of different timescales at the reach scale. Joint calibration of a transient storage model with both tracers better constrains model parameters, highlighting that this approach is critical for improving solute transport estimates in future studies.
Susan E. Quick, Giulio Curioni, Nicholas J. Harper, Stefan Krause, and A. Robert MacKenzie
Biogeosciences, 22, 1557–1581, https://doi.org/10.5194/bg-22-1557-2025, https://doi.org/10.5194/bg-22-1557-2025, 2025
Short summary
Short summary
To study the effects of rising CO2 levels on water usage of old-growth temperate oak forest, we monitored trees in an open-air elevated CO2 experiment for 5 years. We found 4 %–16 % leaf-on season reduction in daylight water usage for ~35% increase in atmospheric CO2. July-only reduction varied more widely. Tree water usage depended on tree size, i.e. stem size and projected canopy area, across all treatments. Experimental infrastructure increased the water usage of the trees in leaf-on season.
Maggi M. Laan, Stephanie G. Fulton, Vanessa A. Garayburu-Caruso, Morgan E. Barnes, Mikayla A. Borton, Xingyuan Chen, Yuliya Farris, Brieanne Forbes, Amy E. Goldman, Samantha Grieger, Robert O. Hall Jr., Matthew H. Kaufman, Xinming Lin, Erin L. M. Zionce, Sophia A. McKever, Allison Myers-Pigg, Opal Otenburg, Aaron C. Pelly, Huiying Ren, Lupita Renteria, Timothy D. Scheibe, Kyongho Son, Jerry Tagestad, Joshua M. Torgeson, and James C. Stegen
EGUsphere, https://doi.org/10.5194/egusphere-2025-1109, https://doi.org/10.5194/egusphere-2025-1109, 2025
Short summary
Short summary
Respiration is a process that combines carbon and oxygen to generate energy for living organisms. Within a river, respiration in sediments and water have variable contributions to respiration of the whole river system. Contrary to conventional wisdom, we found that water column respiration did not increase systematically moving from small streams to big rivers. Instead, it was locally influenced by temperature, nutrients and suspended solids.
James Stegen, Amy J. Burgin, Michelle H. Busch, Joshua B. Fisher, Joshua Ladau, Jenna Abrahamson, Lauren Kinsman-Costello, Li Li, Xingyuan Chen, Thibault Datry, Nate McDowell, Corianne Tatariw, Anna Braswell, Jillian M. Deines, Julia A. Guimond, Peter Regier, Kenton Rod, Edward K. P. Bam, Etienne Fluet-Chouinard, Inke Forbrich, Kristin L. Jaeger, Teri O'Meara, Tim Scheibe, Erin Seybold, Jon N. Sweetman, Jianqiu Zheng, Daniel C. Allen, Elizabeth Herndon, Beth A. Middleton, Scott Painter, Kevin Roche, Julianne Scamardo, Ross Vander Vorste, Kristin Boye, Ellen Wohl, Margaret Zimmer, Kelly Hondula, Maggi Laan, Anna Marshall, and Kaizad F. Patel
Biogeosciences, 22, 995–1034, https://doi.org/10.5194/bg-22-995-2025, https://doi.org/10.5194/bg-22-995-2025, 2025
Short summary
Short summary
The loss and gain of surface water (variable inundation) are common processes across Earth. Global change shifts variable inundation dynamics, highlighting a need for unified understanding that transcends individual variably inundated ecosystems (VIEs). We review the literature, highlight challenges, and emphasize opportunities to generate transferable knowledge by viewing VIEs through a common lens. We aim to inspire the emergence of a cross-VIE community based on a proposed continuum approach.
Daniel G. Kingston, Liam Cooper, David A. Lavers, and David M. Hannah
Nat. Hazards Earth Syst. Sci., 25, 675–682, https://doi.org/10.5194/nhess-25-675-2025, https://doi.org/10.5194/nhess-25-675-2025, 2025
Short summary
Short summary
Extreme rainfall comprises a major hydrohazard for New Zealand and is commonly associated with atmospheric rivers – narrow plumes of very high atmospheric moisture transport. Here, we focus on improved forecasting of these events by testing a forecasting tool previously applied to similar situations in western Europe. However, our results for New Zealand suggest the performance of this forecasting tool may vary depending on geographical setting.
Jonathan D. Mackay, Nicholas E. Barrand, David M. Hannah, Emily Potter, Nilton Montoya, and Wouter Buytaert
The Cryosphere, 19, 685–712, https://doi.org/10.5194/tc-19-685-2025, https://doi.org/10.5194/tc-19-685-2025, 2025
Short summary
Short summary
We combine two globally capable glacier evolution models to include processes that are typically neglected but thought to control tropical glacier retreat (e.g. sublimation). We apply the model to Peru's Vilcanota-Urubamba Basin. The model captures observed glacier mass changes,but struggles with surface albedo dynamics. Projections show glacier mass shrinking to 17 % or 6 % of 2000 levels by 2100 under moderate- and high-emission scenarios, respectively.
Robert E. Danczak, Amy E. Goldman, Mikayla A. Borton, Rosalie K. Chu, Jason G. Toyoda, Vanessa A. Garayburu-Caruso, Emily B. Graham, Joseph W. Morad, Lupita Renteria, Jacqueline R. Hager, Shai Arnon, Scott Brooks, Edo Bar-Zeev, Michael Jones, Nikki Jones, Jorg Lewandowski, Christof Meile, Birgit M. Muller, John Schalles, Hanna Schulz, Adam Ward, and James C. Stegen
EGUsphere, https://doi.org/10.1101/2024.01.10.575030, https://doi.org/10.1101/2024.01.10.575030, 2025
Short summary
Short summary
As dissolved organic matter (DOM) is transported from land to the ocean through rivers, it interacts with the environment and some is converted to CO2. We used high-resolution carbon analysis to show that DOM from seven rivers exhibited ecological patterns particular to the corresponding river. These results indicate that local processes play an outsized role in shaping DOM. By understanding these interactions across environments, we can predict DOM across spatial scales or under perturbations.
Morgan E. Barnes, Jesse Alan Roebuck Jr., Samantha Grieger, Paul J. Aronstein, Vanessa A. Garayburu-Caruso, Kathleen Munson, Robert P. Young, Kevin D. Bladon, John D. Bailey, Emily B. Graham, Lupita Renteria, Peggy A. O'Day, Timothy D. Scheibe, and Allison N. Myers-Pigg
EGUsphere, https://doi.org/10.5194/egusphere-2025-21, https://doi.org/10.5194/egusphere-2025-21, 2025
Short summary
Short summary
Wildfires impact nutrient cycles on land and in water. We used burning experiments to understand the types of phosphorous (P), an essential nutrient, that might be released to the environment after different types of fires. We found that the amount of P moving through the environment post-fire is dependent on the type of vegetation and degree of burning which may influence when and where this material is processed or stored.
Katherine A. Muller, Peishi Jiang, Glenn Hammond, Tasneem Ahmadullah, Hyun-Seob Song, Ravi Kukkadapu, Nicholas Ward, Madison Bowe, Rosalie K. Chu, Qian Zhao, Vanessa A. Garayburu-Caruso, Alan Roebuck, and Xingyuan Chen
Geosci. Model Dev., 17, 8955–8968, https://doi.org/10.5194/gmd-17-8955-2024, https://doi.org/10.5194/gmd-17-8955-2024, 2024
Short summary
Short summary
The new Lambda-PFLOTRAN workflow incorporates organic matter chemistry into reaction networks to simulate aerobic respiration and biogeochemistry. Lambda-PFLOTRAN is a Python-based workflow in a Jupyter notebook interface that digests raw organic matter chemistry data via Fourier transform ion cyclotron resonance mass spectrometry, develops a representative reaction network, and completes a biogeochemical simulation with the open-source, parallel-reactive-flow, and transport code PFLOTRAN.
Anna B. Turetcaia, Nicole G. Dix, Hannah Ramage, Matthew C. Ferner, and Emily B. Graham
EGUsphere, https://doi.org/10.31223/X50Q3S, https://doi.org/10.31223/X50Q3S, 2024
This preprint is open for discussion and under review for Biogeosciences (BG).
Short summary
Short summary
We investigate what physicochemical and urbanization factors are involved in estuarine resistance to precipitation events across scales and salinity gradient. We found that urban estuaries are more resistant to precipitation events. We also found that while water temperature, water column depth, turbidity, nitrogen, and chlorophyll-a are related to estuarine resistance on continental-scale, these trends interacted with estuarine salinity and differed on local-scale.
William Kew, Allison Myers-Pigg, Christine H. Chang, Sean M. Colby, Josie Eder, Malak M. Tfaily, Jeffrey Hawkes, Rosalie K. Chu, and James C. Stegen
Biogeosciences, 21, 4665–4679, https://doi.org/10.5194/bg-21-4665-2024, https://doi.org/10.5194/bg-21-4665-2024, 2024
Short summary
Short summary
Natural organic matter (NOM) is often studied via Fourier transform mass spectrometry (FTMS), which identifies organic molecules as mass spectra peaks. The intensity of peaks is data that is often discarded due to technical concerns. We review the theory behind these concerns and show they are supported empirically. However, simulations show that ecological analyses of NOM data that include FTMS peak intensities are often valid. This opens a path for robust use of FTMS peak intensities for NOM.
Edwin Saavedra Cifuentes, Alex Furman, Ravid Rosenzweig, and Aaron I. Packman
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2024-251, https://doi.org/10.5194/hess-2024-251, 2024
Revised manuscript under review for HESS
Short summary
Short summary
Our research addresses the operational challenge of SAT systems that clog with biomass. A model to optimize their operation is proposed and considers the dynamic interactions between microbial activity, water flow, and soil clogging. Simulations showed the duration of wet and dry periods that enhance water infiltration. A link between the biomass spatial distribution and the wet and dry cycles was discovered. These findings can provide practical insights for real-world SAT systems.
Yiming Li, Uwe Schneidewind, Zhang Wen, Stefan Krause, and Hui Liu
Hydrol. Earth Syst. Sci., 28, 1751–1769, https://doi.org/10.5194/hess-28-1751-2024, https://doi.org/10.5194/hess-28-1751-2024, 2024
Short summary
Short summary
Meandering rivers are an integral part of many landscapes around the world. Here we used a new modeling approach to look at how the slope of riverbanks influences water flow and solute transport from a meandering river channel through its bank and into/out of the connected groundwater compartment (aquifer). We found that the bank slope can be a significant factor to be considered, especially when bank slope angles are small, and riverbank and aquifer conditions only allow for slow water flow.
Danny Croghan, Pertti Ala-Aho, Jeffrey Welker, Kaisa-Riikka Mustonen, Kieran Khamis, David M. Hannah, Jussi Vuorenmaa, Bjørn Kløve, and Hannu Marttila
Hydrol. Earth Syst. Sci., 28, 1055–1070, https://doi.org/10.5194/hess-28-1055-2024, https://doi.org/10.5194/hess-28-1055-2024, 2024
Short summary
Short summary
The transport of dissolved organic carbon (DOC) from land into streams is changing due to climate change. We used a multi-year dataset of DOC and predictors of DOC in a subarctic stream to find out how transport of DOC varied between seasons and between years. We found that the way DOC is transported varied strongly seasonally, but year-to-year differences were less apparent. We conclude that the mechanisms of transport show a higher degree of interannual consistency than previously thought.
Ciaran J. Harman and Esther Xu Fei
Geosci. Model Dev., 17, 477–495, https://doi.org/10.5194/gmd-17-477-2024, https://doi.org/10.5194/gmd-17-477-2024, 2024
Short summary
Short summary
Over the last 10 years, scientists have developed StorAge Selection: a new way of modeling how material is transported through complex systems. Here, we present some new, easy-to-use, flexible, and very accurate code for implementing this method. We show that, in cases where we know exactly what the answer should be, our code gets the right answer. We also show that our code is closer than some other codes to the right answer in an important way: it conserves mass.
Stephanie G. Fulton, Morgan Barnes, Mikayla A. Borton, Xingyuan Chen, Yuliya Farris, Brieanne Forbes, Vanessa A. Garayburu-Caruso, Amy E. Goldman, Samantha Grieger, Robert Hall Jr., Matthew H. Kaufman, Xinming Lin, Erin McCann, Sophia A. McKever, Allison Myers-Pigg, Opal C. Otenburg, Aaron C. Pelly, Huiying Ren, Lupita Renteria, Timothy D. Scheibe, Kyongho Son, Jerry Tagestad, Joshua M. Torgeson, and James C. Stegen
EGUsphere, https://doi.org/10.5194/egusphere-2023-3038, https://doi.org/10.5194/egusphere-2023-3038, 2024
Preprint archived
Short summary
Short summary
This research examines oxygen use in rivers, which is central to the carbon cycle and water quality. The study focused on an environmentally diverse river basin in the western United States and found that oxygen use in river water was very slow and influenced by factors like water temperature and concentrations of nutrients and carbon in the water. Results suggest that in the study system, most of the oxygen use occurs via mechanisms directly or indirectly associated with riverbed sediments.
Emily B. Graham, Hyun-Seob Song, Samantha Grieger, Vanessa A. Garayburu-Caruso, James C. Stegen, Kevin D. Bladon, and Allison N. Myers-Pigg
Biogeosciences, 20, 3449–3457, https://doi.org/10.5194/bg-20-3449-2023, https://doi.org/10.5194/bg-20-3449-2023, 2023
Short summary
Short summary
Intensifying wildfires are increasing pyrogenic organic matter (PyOM) production and its impact on water quality. Recent work indicates that PyOM may have a greater impact on aquatic biogeochemistry than previously assumed, driven by higher bioavailability. We provide a full assessment of the potential bioavailability of PyOM across its chemical spectrum. We indicate that PyOM can be actively transformed within the river corridor and, therefore, may be a growing source of riverine C emissions.
Arianna Borriero, Rohini Kumar, Tam V. Nguyen, Jan H. Fleckenstein, and Stefanie R. Lutz
Hydrol. Earth Syst. Sci., 27, 2989–3004, https://doi.org/10.5194/hess-27-2989-2023, https://doi.org/10.5194/hess-27-2989-2023, 2023
Short summary
Short summary
We analyzed the uncertainty of the water transit time distribution (TTD) arising from model input (interpolated tracer data) and structure (StorAge Selection, SAS, functions). We found that uncertainty was mainly associated with temporal interpolation, choice of SAS function, nonspatial interpolation, and low-flow conditions. It is important to characterize the specific uncertainty sources and their combined effects on TTD, as this has relevant implications for both water quantity and quality.
James C. Stegen, Vanessa A. Garayburu-Caruso, Robert E. Danczak, Amy E. Goldman, Lupita Renteria, Joshua M. Torgeson, and Jacqueline Hager
Biogeosciences, 20, 2857–2867, https://doi.org/10.5194/bg-20-2857-2023, https://doi.org/10.5194/bg-20-2857-2023, 2023
Short summary
Short summary
Chemical reactions in river sediments influence how clean the water is and how much greenhouse gas comes out of a river. Our study investigates why some sediments have higher rates of chemical reactions than others. We find that to achieve high rates, sediments need to have two things: only a few different kinds of molecules, but a lot of them. This result spans about 80 rivers such that it could be a general rule, helpful for predicting the future of rivers and our planet.
Jonas Leon Schaper, Olaf A. Cirpka, Joerg Lewandowski, and Christiane Zarfl
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2023-141, https://doi.org/10.5194/hess-2023-141, 2023
Manuscript not accepted for further review
Short summary
Short summary
In this study, we present a model approach to quantify river water to riverbed sediment travel times as a continuous function of time using natural electrical conductivity fluctuations as a tracer. We show that apparent water travel times from surface waters through riverbed sediments can be highly dynamic, which may be caused by actual variations of porewater velocity following diurnal variations of head gradients or by a shift of the spatial arrangement of flow paths and their lengths.
Tahmina Yasmin, Kieran Khamis, Anthony Ross, Subir Sen, Anita Sharma, Debashish Sen, Sumit Sen, Wouter Buytaert, and David M. Hannah
Nat. Hazards Earth Syst. Sci., 23, 667–674, https://doi.org/10.5194/nhess-23-667-2023, https://doi.org/10.5194/nhess-23-667-2023, 2023
Short summary
Short summary
Floods continue to be a wicked problem that require developing early warning systems with plausible assumptions of risk behaviour, with more targeted conversations with the community at risk. Through this paper we advocate the use of a SMART approach to encourage bottom-up initiatives to develop inclusive and purposeful early warning systems that benefit the community at risk by engaging them at every step of the way along with including other stakeholders at multiple scales of operations.
Carolin Winter, Tam V. Nguyen, Andreas Musolff, Stefanie R. Lutz, Michael Rode, Rohini Kumar, and Jan H. Fleckenstein
Hydrol. Earth Syst. Sci., 27, 303–318, https://doi.org/10.5194/hess-27-303-2023, https://doi.org/10.5194/hess-27-303-2023, 2023
Short summary
Short summary
The increasing frequency of severe and prolonged droughts threatens our freshwater resources. While we understand drought impacts on water quantity, its effects on water quality remain largely unknown. Here, we studied the impact of the unprecedented 2018–2019 drought in Central Europe on nitrate export in a heterogeneous mesoscale catchment in Germany. We show that severe drought can reduce a catchment's capacity to retain nitrogen, intensifying the internal pollution and export of nitrate.
Thomas Hermans, Pascal Goderniaux, Damien Jougnot, Jan H. Fleckenstein, Philip Brunner, Frédéric Nguyen, Niklas Linde, Johan Alexander Huisman, Olivier Bour, Jorge Lopez Alvis, Richard Hoffmann, Andrea Palacios, Anne-Karin Cooke, Álvaro Pardo-Álvarez, Lara Blazevic, Behzad Pouladi, Peleg Haruzi, Alejandro Fernandez Visentini, Guilherme E. H. Nogueira, Joel Tirado-Conde, Majken C. Looms, Meruyert Kenshilikova, Philippe Davy, and Tanguy Le Borgne
Hydrol. Earth Syst. Sci., 27, 255–287, https://doi.org/10.5194/hess-27-255-2023, https://doi.org/10.5194/hess-27-255-2023, 2023
Short summary
Short summary
Although invisible, groundwater plays an essential role for society as a source of drinking water or for ecosystems but is also facing important challenges in terms of contamination. Characterizing groundwater reservoirs with their spatial heterogeneity and their temporal evolution is therefore crucial for their sustainable management. In this paper, we review some important challenges and recent innovations in imaging and modeling the 4D nature of the hydrogeological systems.
Jie Yang, Qiaoyu Wang, Ingo Heidbüchel, Chunhui Lu, Yueqing Xie, Andreas Musolff, and Jan H. Fleckenstein
Hydrol. Earth Syst. Sci., 26, 5051–5068, https://doi.org/10.5194/hess-26-5051-2022, https://doi.org/10.5194/hess-26-5051-2022, 2022
Short summary
Short summary
We assessed the effect of catchment topographic slopes on the nitrate export dynamics in terms of the nitrogen mass fluxes and concentration level using a coupled surface–subsurface model. We found that flatter landscapes tend to retain more nitrogen mass in the soil and export less nitrogen mass to the stream, explained by the reduced leaching and increased potential of degradation in flat landscapes. We emphasized that stream water quality is potentially less vulnerable in flatter landscapes.
José L. J. Ledesma, Anna Lupon, Eugènia Martí, and Susana Bernal
Hydrol. Earth Syst. Sci., 26, 4209–4232, https://doi.org/10.5194/hess-26-4209-2022, https://doi.org/10.5194/hess-26-4209-2022, 2022
Short summary
Short summary
We studied a small stream located in a Mediterranean forest. Our goal was to understand how stream flow and the presence of riparian forests, which grow in flat banks near the stream, influence the availability of food for aquatic microorganisms. High flows were associated with higher amounts of food because rainfall episodes transfer it from the surrounding sources, particularly riparian forests, to the stream. Understanding how ecosystems work is essential to better manage natural resources.
James C. Stegen, Sarah J. Fansler, Malak M. Tfaily, Vanessa A. Garayburu-Caruso, Amy E. Goldman, Robert E. Danczak, Rosalie K. Chu, Lupita Renteria, Jerry Tagestad, and Jason Toyoda
Biogeosciences, 19, 3099–3110, https://doi.org/10.5194/bg-19-3099-2022, https://doi.org/10.5194/bg-19-3099-2022, 2022
Short summary
Short summary
Rivers are vital to Earth, and in rivers, organic matter (OM) is an energy source for microbes that make greenhouse gas and remove contaminants. Predicting Earth’s future requires understanding how and why river OM is transformed. Our results help meet this need. We found that the processes influencing OM transformations diverge between river water and riverbed sediments. This can be used to build new models for predicting the future of rivers and, in turn, the Earth system.
Esther Xu Fei and Ciaran Joseph Harman
Hydrol. Earth Syst. Sci., 26, 1977–1991, https://doi.org/10.5194/hess-26-1977-2022, https://doi.org/10.5194/hess-26-1977-2022, 2022
Short summary
Short summary
Water in streams is a mixture of water from many sources. It is sometimes possible to identify the chemical fingerprint of each source and track the time-varying contribution of that source to the total flow rate. But what if you do not know the chemical fingerprint of each source? Can you simultaneously identify the sources (called end-members), and separate the water into contributions from each, using only samples of water from the stream? Here we suggest a method for doing just that.
Guilherme E. H. Nogueira, Christian Schmidt, Daniel Partington, Philip Brunner, and Jan H. Fleckenstein
Hydrol. Earth Syst. Sci., 26, 1883–1905, https://doi.org/10.5194/hess-26-1883-2022, https://doi.org/10.5194/hess-26-1883-2022, 2022
Short summary
Short summary
In near-stream aquifers, mixing between stream water and ambient groundwater can lead to dilution and the removal of substances that can be harmful to the water ecosystem at high concentrations. We used a numerical model to track the spatiotemporal evolution of different water sources and their mixing around a stream, which are rather difficult in the field. Results show that mixing mainly develops as narrow spots, varying In time and space, and is affected by magnitudes of discharge events.
Arial J. Shogren, Jay P. Zarnetske, Benjamin W. Abbott, Samuel Bratsman, Brian Brown, Michael P. Carey, Randy Fulweber, Heather E. Greaves, Emma Haines, Frances Iannucci, Joshua C. Koch, Alexander Medvedeff, Jonathan A. O'Donnell, Leika Patch, Brett A. Poulin, Tanner J. Williamson, and William B. Bowden
Earth Syst. Sci. Data, 14, 95–116, https://doi.org/10.5194/essd-14-95-2022, https://doi.org/10.5194/essd-14-95-2022, 2022
Short summary
Short summary
Rapidly sampling multiple points in an entire river network provides a high-resolution snapshot in time that can reveal where nutrients and carbon are being taken up and released. Here, we describe two such datasets of river network chemistry in six Arctic watersheds in northern Alaska. We describe how these repeated snapshots can be used as an indicator of ecosystem response to climate change and to improve predictions of future release of carbon, nutrient, and other solutes.
Joni Dehaspe, Fanny Sarrazin, Rohini Kumar, Jan H. Fleckenstein, and Andreas Musolff
Hydrol. Earth Syst. Sci., 25, 6437–6463, https://doi.org/10.5194/hess-25-6437-2021, https://doi.org/10.5194/hess-25-6437-2021, 2021
Short summary
Short summary
Increased nitrate concentrations in surface waters can compromise river ecosystem health. As riverine nitrate uptake is hard to measure, we explore how low-frequency nitrate concentration and discharge observations (that are widely available) can help to identify (in)efficient uptake in river networks. We find that channel geometry and water velocity rather than the biological uptake capacity dominate the nitrate-discharge pattern at the outlet. The former can be used to predict uptake.
Benedikt J. Werner, Oliver J. Lechtenfeld, Andreas Musolff, Gerrit H. de Rooij, Jie Yang, Ralf Gründling, Ulrike Werban, and Jan H. Fleckenstein
Hydrol. Earth Syst. Sci., 25, 6067–6086, https://doi.org/10.5194/hess-25-6067-2021, https://doi.org/10.5194/hess-25-6067-2021, 2021
Short summary
Short summary
Export of dissolved organic carbon (DOC) from riparian zones (RZs) is an important yet poorly understood component of the catchment carbon budget. This study chemically and spatially classifies DOC source zones within a RZ of a small catchment to assess DOC export patterns. Results highlight that DOC export from only a small fraction of the RZ with distinct DOC composition dominates overall DOC export. The application of a spatial, topographic proxy can be used to improve DOC export models.
Doris E. Wendt, John P. Bloomfield, Anne F. Van Loon, Margaret Garcia, Benedikt Heudorfer, Joshua Larsen, and David M. Hannah
Nat. Hazards Earth Syst. Sci., 21, 3113–3139, https://doi.org/10.5194/nhess-21-3113-2021, https://doi.org/10.5194/nhess-21-3113-2021, 2021
Short summary
Short summary
Managing water demand and supply during droughts is complex, as highly pressured human–water systems can overuse water sources to maintain water supply. We evaluated the impact of drought policies on water resources using a socio-hydrological model. For a range of hydrogeological conditions, we found that integrated drought policies reduce baseflow and groundwater droughts most if extra surface water is imported, reducing the pressure on water resources during droughts.
Katharina Blaurock, Burkhard Beudert, Benjamin S. Gilfedder, Jan H. Fleckenstein, Stefan Peiffer, and Luisa Hopp
Hydrol. Earth Syst. Sci., 25, 5133–5151, https://doi.org/10.5194/hess-25-5133-2021, https://doi.org/10.5194/hess-25-5133-2021, 2021
Short summary
Short summary
Dissolved organic carbon (DOC) is an important part of the global carbon cycle with regards to carbon storage, greenhouse gas emissions and drinking water treatment. In this study, we compared DOC export of a small, forested catchment during precipitation events after dry and wet preconditions. We found that the DOC export from areas that are usually important for DOC export was inhibited after long drought periods.
Aditi Sengupta, Sarah J. Fansler, Rosalie K. Chu, Robert E. Danczak, Vanessa A. Garayburu-Caruso, Lupita Renteria, Hyun-Seob Song, Jason Toyoda, Jacqueline Hager, and James C. Stegen
Biogeosciences, 18, 4773–4789, https://doi.org/10.5194/bg-18-4773-2021, https://doi.org/10.5194/bg-18-4773-2021, 2021
Short summary
Short summary
Conceptual models link microbes with the environment but are untested. We test a recent model using riverbed sediments. We exposed sediments to disturbances, going dry and becoming wet again. As the length of dry conditions got longer, there was a sudden shift in the ecology of microbes, chemistry of organic matter, and rates of microbial metabolism. We propose a new model based on feedbacks initiated by disturbance that cascade across biological, chemical, and functional aspects of the system.
Liwen Wu, Jesus D. Gomez-Velez, Stefan Krause, Anders Wörman, Tanu Singh, Gunnar Nützmann, and Jörg Lewandowski
Hydrol. Earth Syst. Sci., 25, 1905–1921, https://doi.org/10.5194/hess-25-1905-2021, https://doi.org/10.5194/hess-25-1905-2021, 2021
Short summary
Short summary
With a physically based model that couples flow and heat transport in hyporheic zones, the present study provides the first insights into the dynamics of hyporheic responses to the impacts of daily groundwater withdrawal and river temperature fluctuations, allowing for a better understanding of transient hyporheic exchange processes and hence an improved pumping operational scheme.
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
Short summary
Short summary
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.
James W. Kirchner and Julia L. A. Knapp
Hydrol. Earth Syst. Sci., 24, 5539–5558, https://doi.org/10.5194/hess-24-5539-2020, https://doi.org/10.5194/hess-24-5539-2020, 2020
Short summary
Short summary
Ensemble hydrograph separation is a powerful new tool for measuring the age distribution of streamwater. However, the calculations are complex and may be difficult for researchers to implement on their own. Here we present scripts that perform these calculations in either MATLAB or R so that researchers do not need to write their own codes. We explain how these scripts work and how to use them. We demonstrate several potential applications using a synthetic catchment data set.
Doris E. Wendt, Anne F. Van Loon, John P. Bloomfield, and David M. Hannah
Hydrol. Earth Syst. Sci., 24, 4853–4868, https://doi.org/10.5194/hess-24-4853-2020, https://doi.org/10.5194/hess-24-4853-2020, 2020
Short summary
Short summary
Groundwater use changes the availability of groundwater, especially during droughts. This study investigates the impact of groundwater use on groundwater droughts. A methodological framework is presented that was developed and applied to the UK. We identified an asymmetric impact of groundwater use on droughts, which highlights the relation between short-term and long-term strategies for sustainable groundwater use.
Angel Monsalve, Catalina Segura, Nicole Hucke, and Scott Katz
Earth Surf. Dynam., 8, 825–839, https://doi.org/10.5194/esurf-8-825-2020, https://doi.org/10.5194/esurf-8-825-2020, 2020
Short summary
Short summary
Part of the inaccuracies when estimating bed load transport in
gravel-bed rivers is because we are not considering the wide distributions of shear stress in these systems. We modified a subsurface-based bed load transport equation to include these distributions. By doing so, our approach accurately predicts bed load transport rates when the pavement layer is still present, while the original one predicts zero transport. For high flows, our method had similar performance to the original equation.
Nicolas Massei, Daniel G. Kingston, David M. Hannah, Jean-Philippe Vidal, Bastien Dieppois, Manuel Fossa, Andreas Hartmann, David A. Lavers, and Benoit Laignel
Proc. IAHS, 383, 141–149, https://doi.org/10.5194/piahs-383-141-2020, https://doi.org/10.5194/piahs-383-141-2020, 2020
Short summary
Short summary
This paper presents recent thoughts by members of EURO-FRIEND Water project 3 “Large-scale-variations in hydrological characteristics” about research needed to characterize and understand large-scale hydrology under global changes. Emphasis is put on the necessary efforts to better understand 1 – the impact of low-frequency climate variability on hydrological trends and extremes, 2 – the role of basin properties on modulating the climate signal producing hydrological responses on the basin scale.
Bentje Brauns, Daniela Cuba, John P. Bloomfield, David M. Hannah, Christopher Jackson, Ben P. Marchant, Benedikt Heudorfer, Anne F. Van Loon, Hélène Bessière, Bo Thunholm, and Gerhard Schubert
Proc. IAHS, 383, 297–305, https://doi.org/10.5194/piahs-383-297-2020, https://doi.org/10.5194/piahs-383-297-2020, 2020
Short summary
Short summary
In Europe, ca. 65% of drinking water is groundwater. Its replenishment depends on rainfall, but droughts may cause groundwater levels to fall below normal. These
groundwater droughtscan limit supply, making it crucial to understand their regional connection. The Groundwater Drought Initiative (GDI) assesses spatial patterns in historic—recent groundwater droughts across Europe for the first time. Using an example dataset, we describe the background to the GDI and its methodological approach.
Cited articles
Abbott, B. W., Gruau, G., Zarnetske, J. P., Moatar, F., Barbe, L., Thomas,
Z., Fovet, O., Kolbe, T., Gu, S., Pierson-Wickmann, A. C., Davy, P., and
Pinay, G.: Unexpected spatial stability of water chemistry in headwater
stream networks, Ecol. Lett., 21, 296–308, https://doi.org/10.1111/ele.12897, 2018.
Anderson, J. K., Wondzell, S. M., Gooseff, M. N., and Haggerty, R.: Patterns
in stream longitudinal profiles and implications for hyporheic exchange flow
at the H. J. Andrews Experimental Forest, Oregon, USA, Hydrol. Process.,
19, 2931–2949, 2005.
Andersen, T.: in: Chironomidae of the Holarctic Region: Keys and Diagnoses: Larvae, edited by: Andersen, T., Cranston, P. S., and Epler, J. H., Scandinavian Society of Entomologym, 2013.
Arndt, S., Jørgensen, B. B., LaRowe, D. E., Middelburg, J. J., Pancost, R. D., and Regnier, P.: Quantifying the degradation of organic matter in marine sediments: A review and synthesis, Earth-Sci. Rev., 123, 53–86, https://doi.org/10.1016/j.earscirev.2013.02.008, 2013.
Belanger, C., Desrosiers, B., and Lee, K.: Microbial extracellular enzyme
activity in marine sediments: extreme pH to terminate reaction and sample
storage, Aquat. Microb. Ecol., 13, 187–196, 1997.
Bernhardt, E. S., Blaszczak, J. R., Ficken, C. D., Fork, M. L., Kaiser, K.
E., and Seybold, E. C.: Control Points in Ecosystems: Moving Beyond the Hot
Spot Hot Moment Concept, Ecosystems, 20, 665–682,
https://doi.org/10.1007/s10021-016-0103-y, 2017.
Boano, F., Harvey, J. W., Marion, A., Packman, A. I., Revelli, R., Ridolfi,
L., and Worman, A.: Hyporheic flow and transport processes: Mechanisms,
models, and biogeochemical implications, Rev. Geophys., 52, 603–679,
https://doi.org/10.1002/2012RG000417, 2014.
Boulton, A. J., Findlay, S., Marmonier, P., Stanley, E. H., and Valett, H.
M.: The functional significance of the hyporheic zone in streams and rivers,
Annu. Rev. Ecol. Syst., 29, 59–81, 1998.
Boye, K., Noël, V., Tfaily, M. M., Bone, S. E., Williams, K. H., Bargar,
J. R., and Fendorf, S.: Thermodynamically controlled preservation of organic
carbon in floodplains, Nat. Geosci., 10, 415–419, https://doi.org/10.1038/ngeo2940,
2017.
Brunke, M. and Gonser, T.: The ecological significance of exchange processes
between rivers and groundwater, Freshw. Biol., 37, 1–33, 1997.
Caporaso, J. G., Lauber, C. L., Walters, W. A., Berg-Lyons, D., Huntley, J., Fierer, N., Owens, S. M., Betley, J., Fraser, L., Bauer, M., Gormley, N.,
Gilbert, J. A., Smith, G., and Knight, R.: Ultra-high-throughput microbial community analysis on the Illumina HiSeq and MiSeq platforms, ISME J., 6, 1621–1624, https://doi.org/10.1038/ismej.2012.8, 2012.
Coble, P. G.: Characterization of marine and terrestrial DOM in seawater
using excitation-emission matrix spectroscopy, Mar. Chem., 51, 325–346,
https://doi.org/10.1016/0304-4203(95)00062-3, 1996.
Corson-Rikert, H. A., Wondzell, S. M., Haggerty, R., and Santelmann, M. V:
Carbon dynamics in the hyporheic zone of a headwater mountain streamin the
Cascade Mountains, Oregon, Water Resour. Res., 52, 7556–7576,
https://doi.org/10.1029/2008WR006912.M, 2016.
Cory, R. M. and Kaplan, L. A.: Biological lability of streamwater
fluorescent dissolved organic matter, Limnol. Oceanogr., 57, 1347–1360,
https://doi.org/10.4319/lo.2012.57.5.1347, 2012.
Cory, R. M. and McKnight, D. M.: Fluorescence spectroscopy reveals
ubiquitous presence of oxidized and reduced quinones in dissolved organic
matter, Environ. Sci. Technol., 39, 8142–8149, https://doi.org/10.1021/es0506962,
2005.
Cory, R. M., Miller, M. P., McKnight, D. M., Guerard, J. J., and Miller, P.
L.: Effect of instrument-specific response on the analysis of fulvic acid
fluorescence spectra, Limnol. Oceanogr.-Meth., 8, 67–78,
https://doi.org/10.4319/lom.2010.8.67, 2010.
Crevecoeur, S., Vincent, W. F., Comte, J., and Lovejoy, C.: Bacterial community structure across environmental gradients in permafrost thaw ponds: methanotroph-rich ecosystems, Front. Microbiol., 6, 192, https://doi.org/10.3389/fmicb.2015.00192, 2015.
Crossman, J., Bradley, C., Milner, A., and Pinay, G.: Influence Of
Environmental Instability Of Groundwater-Fed Streams On Hyporheic Fauna, On
A Glacial Floodplain, Denali National Park, ALASKA, River Res. Appl., 29,
548–559, https://doi.org/10.1002/rra.1619, 2012.
Deligne, N. I., Mckay, D., Conrey, R. M., Grant, G. E., Johnson, E. R.,
O'Connor, J., and Sweeney, K.: Field-trip guide to mafic volcanism of the
Cascade Range in Central Oregon – A volcanic, tectonic, hydrologic, and
geomorphic journey, Sci. Investig. Rep., 110, https://doi.org/10.3133/sir20175022H,
2017.
Dent, C. L. and Grimm, N. B.: Spatial heterogeneity of stream water nutrient
concentrations over successional time, Ecology, 80, 2283–2298,
https://doi.org/10.1890/0012-9658(1999)080[2283:SHOSWN]2.0.CO;2, 1999.
Dittmar, T., Koch, B., Hertkorn, N., and Kattner, G.: A simple and efficient
method for the solid-phase extraction of dissolved organic matter (SPE-DOM)
from seawater, Limnol. Oceanogr.-Meth., 6, 230–235,
https://doi.org/10.4319/lom.2008.6.230, 2008.
Dupas, R., Minaudo, C., and Abbott, B. W.: Stability of spatial patterns in
water chemistry across temperate ecoregions, Environ. Res. Lett., 14,
074015, https://doi.org/10.1088/1748-9326/ab24f4, 2019.
Dyrness, C. T.: Hydrologic properties of soils on three small watersheds in
the western Cascades of Oregon, USDA For. SERV RES NOTE PNW-111,
17 pp., 1969.
Graham, E. B., Tfaily, M. M., Crump, A. R., Goldman, A. E., Bramer, L. M.,
Arntzen, E., Romero, E., Resch, C. T., Kennedy, D. W., and Stegen, J. C.:
Carbon Inputs From Riparian Vegetation Limit Oxidation of Physically Bound
Organic Carbon Via Biochemical and Thermodynamic Processes, J. Geophys. Res.-Biogeo., 122, 3188–3205, https://doi.org/10.1002/2017JG003967, 2017.
Hale, R. L. and Godsey, S. E.: Dynamic stream network intermittence explains
emergent dissolved organic carbon chemostasis in headwaters, Hydrol.
Process., 33, 1926–1936, https://doi.org/10.1002/hyp.13455, 2019.
Harvey, J. W. and Gooseff, M. N.: River corridor science: Hydrologic
exchange and ecological consequences from bedforms to basins, Water Resour.
Res., 51, 6893–6922, https://doi.org/10.1002/2015WR017617, 2015.
Helms, J. R., Stubbins, A., Ritchie, J. D., Minor, E. C., Kieher, D. J., and
Mopper, K.: Absorption spectral slopes and slope ratios as indicators of
molecular weight, source, and photobleaching of chromophoric dissolved
organic matter, Limnol. Oceanogr., 53, 955–969,
https://doi.org/10.1186/s12913-017-2639-8, 2008.
Hvorslev, M. J.: Time lag and soil permeability in ground-water observations.
Bulletin No. 36, Waterways Exper. Sta., Corps of Engineers, U.S. Army,
Vicksburg, Mississippi, 50 pp., 1951.
Isaak, D. J., Peterson, E. E., Ver Hoef, J. M., Wenger, S. J., Falke, J. A.,
Torgersen, C. E., Sowder, C., Steel, E. A., Fortin, M.-J., Jordan, C. E.,
Ruesch, A. S., Som, N., and Monestiez, P.: Applications of spatial
statistical network models to stream data, WIREs Water,
1, 277–294, https://doi.org/10.1002/wat2.1023, 2014.
Jefferson, A., Grant, G. E., and Lewis, S. L.: A River Runs Underneath It:
Geological Control of Spring and Channel Systems and Management
Implications, Cascade Range, Oregon, in: Advancing the Fundamental Sciences
Proceedings of the Forest Service: Proceedings of the Forest Service
National Earth Sciences Conference, 1, 18–22, 2004.
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.
Kaufmann, P. R., Herlihy, A. T., Mitch, M. E., Messer, J. J., and Overton, W.
S.: Stream chemistry in the eastern United States: 1. Synoptic survey
design, acid-base status, and regional patterns, Water Resour. Res., 27,
611–627, https://doi.org/10.1029/90WR02767, 1991.
Kim, S., Kramer, R. W., and Hatcher, P. G.: Graphical Method for Analysis of
Ultrahigh-Resolution Broadband Mass Spectra of Natural Organic Matter, the
Van Krevelen Diagram, Anal. Chem., 75, 5336–5344,
https://doi.org/10.1021/ac034415p, 2003.
Krause, S., Hannah, D. M., Fleckenstein, J. H., Heppell, C. M., Kaeser, D.
H., Pickup, R., Pinay, G., Robertson, A. L., and Wood, P. J.:
Inter-disciplinary perspectives on processes in the hyporheic zone,
Ecohydrology, 4, 481–499, 2011.
Krause, S., Lewandowski, J., Grimm, N. B., Hannah, D. M., Pinay, G.,
McDonald, K., Martí, E., Argerich, A., Pfister, L., Klaus, J., Battin,
T., Larned, S. T., Schelker, J., Fleckenstein, J., Schmidt, C., Rivett, M.
O., Watts, G., Sabater, F., Sorolla, A., and Turk, V.: Ecohydrological
interfaces as hot spots of ecosystem processes, Water Resour. Res., 53,
6359–6376, https://doi.org/10.1002/2016WR019516, 2017.
Kujawinski, E. B. and Behn, M. D.: Automated analysis of electrospray
ionization fourier transform ion cyclotron resonance mass spectra of natural
organic matter, Anal. Chem., 78, 4363–4373, https://doi.org/10.1021/ac0600306,
2006.
Langton, P. H.: A key to pupal exuaviae of West Palaearctic
Chironomidae, Langton, 1991.
La Rowe, D. E. and Van Cappellen, P.: Degradation of natural organic matter: A thermodynamic analysis, Geochim. Cosmochim. Acta, 75, 2030–2042, https://doi.org/10.1016/j.gca.2011.01.020, 2011.
Lee-Cullin, J. A., Zarnetske, J. P., Ruhala, S. S., and Plont, S.: Toward
measuring biogeochemistry within the stream-groundwater interface at the
network scale: An initial assessment of two spatial sampling strategies,
Limnol. Oceanogr.-Meth., 16, 722–733, https://doi.org/10.1002/lom3.10277, 2018.
Likens, G. E. and Buso, D. C.: Variation in streamwater chemistry throughout
the Hubbard Brook Valley, Biogeochemistry, 78, 1–30,
https://doi.org/10.1007/s10533-005-2024-2, 2006.
Lowe, W. H., Likens, G. E., and Power, M. E.: Linking Scales in Stream
Ecology, Bioscience, 56, 591–597,
https://doi.org/10.1641/0006-3568(2006)56[591:LSISE]2.0.CO;2, 2006.
Malicky, H.: Atlas der europäischen Köcherfliegen, vol. 24,
Dr. W. Junk Publishing Company, 1983.
Mason, S. J. K., McGlynn, B. L., and Poole, G. C.: Hydrologic response to
channel reconfiguration on Silver Bow Creek, Montana, J. Hydrol., 438–439,
125–136, 2012.
McDonnell, J. J., Sivapalan, M., Vache, K., Dunn, S., Grant, G. E.,
Haggerty, R., Hinz, C., Hooper, R. P., Kirchner, J., and Roderick, M. L.:
Moving beyond heterogeneity and process complexity: A new vision for
watershed hydrology, Water Resour. Res., 43, W07301, https://doi.org/10.1029/2006WR005467, 2007.
McGuire, K. J., Torgersen, C. E., Likens, G. E., Buso, D. C., Lowe, W. H.,
and Bailey, S. W.: Network analysis reveals multiscale controls on
streamwater chemistry, P. Natl. Acad. Sci. USA, 111, 7030–7035,
https://doi.org/10.1073/pnas.1404820111, 2014.
McKnight, D. M., Boyer, E. W., Westerhoff, P. K., Doran, P. T., Kulbe, T.,
and Andersen, D. T.: Spectrofluorometric characterization of dissolved
organic matter for indication of precursor organic material and aromaticity,
Limnol. Oceanogr., 46, 38–48, https://doi.org/10.4319/lo.2001.46.1.0038, 2001.
Merritt, R. W. and Cummins, K. W. (Eds.): An introduction to the aquatic
insects of North America, Kendall Hunt Publishing, 1996.
Minor, E. C., Steinbring, C. J., Longnecker, K., and Kujawinski, E. B.:
Characterization of dissolved organic matter in Lake Superior and its
watershed using ultrahigh resolution mass spectrometry, Org. Geochem., 43,
1–11, https://doi.org/10.1016/j.orggeochem.2011.11.007, 2012.
Nickolas, L. B., Segura, C., and Brooks, J. R.: The influence of lithology on
surface water sources, Hydrol. Process., 31, 1913–1925,
https://doi.org/10.1002/hyp.11156, 2017.
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.
Schwanghart, W. and Kuhn, N. J.: TopoToolbox: A set of Matlab functions for
topographic analysis, Environ. Model. Softw., 25, 770–781,
https://doi.org/10.1016/j.envsoft.2009.12.002, 2010.
Schwanghart, W. and Scherler, D.: Short Communication: TopoToolbox 2 – MATLAB-based software for topographic analysis and modeling in Earth surface sciences, Earth Surf. Dynam., 2, 1–7, https://doi.org/10.5194/esurf-2-1-2014, 2014.
Seibert, J. and McGlynn, B. L.: A new triangular multiple flow direction
algorithm for computing upslope areas from gridded digital elevation models,
Water Resour. Res., 43, 1–8, https://doi.org/10.1029/2006WR005128, 2007.
Sinsabaugh, R. L., Findlay, S., Franchini, P., and Fischer, D.: Enzymatic
analysis of riverine bacterioplankton production, Limnol. Oceanogr., 42,
29–38, https://doi.org/10.4319/lo.1997.42.1.0029, 1997.
Spencer, R. G. M., Aiken, G. R., Butler, K. D., Dornblaser, M. M., Striegl,
R. G., and Hernes, P. J.: Utilizing chromophoric dissolved organic matter
measurements to derive export and reactivity of dissolved organic carbon
exported to the Arctic Ocean: A case study of the Yukon River, Alaska,
Geophys. Res. Lett., 36, L06401, https://doi.org/10.1029/2008GL036831, 2009.
Spies, T.: LiDAR Data (August 2008) for the Andrews Experimental Forest and
Willamette National Forest Study Areas, HJA Data Identifier GI010, Long-term
Ecol. Res., For. Sci. Data Bank, Corvalliss, Oreg. (Database), available at: http://andlter.forestry.oregonstate.edu/data/abstract.aspx?dbcode=GI010 (last access: 17 July 2018), 2016.
Stedmon, C. A. and Bro, R.: Characterizing dissolved organic matter
fluorescence with parallel factor analysis: A tutorial, Limnol. Oceanogr.-Meth., 6, 572–579, https://doi.org/10.4319/lom.2008.6.572, 2008.
Stegen, J. C., Johnson, T., Fredrickson, J. K., Wilkins, M. J., Konopka, A.
E., Nelson, W. C., Arntzen, E. V., Chrisler, W. B., Chu, R. K., Fansler, S.
J., Graham, E. B., Kennedy, D. W., Resch, C. T., Tfaily, M., and Zachara, J.:
Influences of organic carbon speciation on hyporheic corridor
biogeochemistry and microbial ecology, Nat. Commun., 9, 1034,
https://doi.org/10.1038/s41467-018-03572-7, 2018.
Swanson, F. J. and James, M. E.: Geology and geomorphology of the H.J.
Andrews Experimental Forest, western Cascades, Oregon, Portland, OR, 1975.
Swanson, F. J. and Jones, J. A.: Geomorphology and hydrology of the HJ
Andrews experimental forest, Blue River, Oregon, F. Guid. to Geol. Process.
Cascadia, 36, 289–314, 2002.
Temnerud, J. and Bishop, K.: Spatial variation of streamwater chemistry in
two Swedish boreal catchments: Implications for environmental assessment,
Environ. Sci. Technol., 39, 1463–1469, https://doi.org/10.1021/es040045q, 2005.
Tfaily, M. M., Chu, R. K., Tolić, N., Roscioli, K. M., Anderton, C. R.,
Paša-Tolić, L., Robinson, E. W., and Hess, N. J.: Advanced solvent
based methods for molecular characterization of soil organic matter by
high-resolution mass spectrometry, Anal. Chem., 87, 5206–5215,
https://doi.org/10.1021/acs.analchem.5b00116, 2015.
Tfaily, M. M., Chu, R. K., Toyoda, J., Tolić, N., Robinson, E. W.,
Paša-Tolić, L., and Hess, N. J.: Sequential extraction protocol for
organic matter from soils and sediments using high resolution mass
spectrometry, Anal. Chim. Acta, 972, 54–61, https://doi.org/10.1016/j.aca.2017.03.031,
2017.
Tonina, D. and Buffington, J. M.: Hyporheic exchange in mountain rivers I:
mechanics and environmental effects, Geogr. Compass, 3, 1063–1086,
https://doi.org/10.1111/j.1749-8198.2009.00226.x, 2009.
Wallace, J. B., Hutchens Jr., J. J., and Grubaugh, J. W.: Transport and storage of FPOM, in: Methods in Stream
Ecolgoy, edited by: Hauer, F. R. and Lamberti, G. A., 2nd edn., Elsevier, New York, 249–271 2006.
Ward, A. S.: The evolution and state of interdisciplinary hyporheic
research, WIREs Water, 3, 83–103,
https://doi.org/10.1002/wat2.1120, 2015.
Ward, A. S.: ESSD 2019 – Data Collection, HydroShare, https://doi.org/10.4211/hs.f4484e0703f743c696c2e1f209abb842, 2019.
Ward, A. S. and Packman, A. I.: Advancing our predictive understanding of
river corridor exchange, WIREs Water, 6, e1327, 17 pp., https://doi.org/10.1002/wat2.1327 2019.
Ward, A. S., Gooseff, M. N., Voltz, T. J., Fitzgerald, M., Singha, K., and
Zarnetske, J. P.: How does rapidly changing discharge during storm events
affect transient storage and channel water balance in a headwater mountain
stream?, Water Resour. Res., 49, 5473–5486, https://doi.org/10.1002/wrcr.20434,
2013a.
Ward, A. S., Payn, R. A., Gooseff, M. N., McGlynn, B. L., Bencala, K. E.,
Kelleher, C. A., Wondzell, S. M., and Wagener, T.: Variations in surface
water-ground water interactions along a headwater mountain stream:
Comparisons between transient storage and water balance analyses, Water
Resour. Res., 49, 3359–3374, https://doi.org/10.1002/wrcr.20148, 2013b.
Ward, A. S., Schmadel, N. M., and Wondzell, S. M.: Simulation of dynamic
expansion, contraction, and connectivity in a mountain stream network, Adv.
Water Resour., 114, 64–82, https://doi.org/10.1016/j.advwatres.2018.01.018, 2018.
Ward, A. S., Wondzell, S. M., Schmadel, N. M., Herzog, S., Zarnetske, J. P., Baranov, V., Blaen, P. J., Brekenfeld, N., Chu, R., Derelle, R., Drummond, J., Fleckenstein, J., Garayburu-Caruso, V., Graham, E., Hannah, D., Harman, C., Hixson, J., Knapp, J. L. A., Krause, S., Kurz, M. J., Lewandowski, J., Li, A., Marti, E., Miller, M., Milner, A. M., Neil, K., Orsini, L., Packman, A. I., Plont, S., Renteria, L., Roche, K., Royer, T., Segura, C., Stegen, J., Toyoda, J., Wells, J., and Wisnoski, N. I.: Spatial and temporal variation in river corridor exchange across a 5th order mountain stream network, Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2019-108, in review, 2019.
Weishaar, J. L., Aiken, G. R., Bergamaschi, B. A., Fram, M. S., Fujii, R., and Mopper, K.: Evaluation of specific ultraviolet absorbance as an indicator of the chemical composition and reactivity of dissolved organic carbon, Environ. Sci. Technol., 37, 4702–4708, https://doi.org/10.1021/es030360x, 2003.
Wolock, D. M., Fan, J., and Lawrence, G. B.: Effects of basin size on
low-flow stream chemistry and subsurface contact time in the Neversink River
watershed, New York, Hydrol. Process., 11, 1273–1286,
https://doi.org/10.1002/(SICI)1099-1085(199707)11:9<1273::AID-HYP557>3.0.CO;2-S, 1997.
Zimmer, M. A., Bailey, S. W., Mcguire, K. J., and Bullen, T. D.: Fine scale
variations of surface water chemistry in an ephemeral to perennial drainage
network, Hydrol. Process., 27, 3438–3451, https://doi.org/10.1002/hyp.9449, 2013.
Short summary
Studies of river corridor exchange commonly focus on characterization of the physical, chemical, or biological system. As a result, complimentary systems and context are often lacking, which may limit interpretation. Here, we present a characterization of all three systems at 62 sites in a 5th-order river basin, including samples of surface water, hyporheic water, and sediment. These data will allow assessment of interacting processes in the river corridor.
Studies of river corridor exchange commonly focus on characterization of the physical, chemical,...
Altmetrics
Final-revised paper
Preprint