Articles | Volume 24, issue 11
https://doi.org/10.5194/hess-24-5453-2020
© Author(s) 2020. 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-24-5453-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
20 Nov 2020
Research article |
| 20 Nov 2020
| 20 Nov 2020
Predicting probabilities of streamflow intermittency across a temperate mesoscale catchment
Nils Hinrich Kaplan
CORRESPONDING AUTHOR
Hydrology, Faculty of Environment and Natural Resources, University of Freiburg, 79098 Freiburg, Germany
Theresa Blume
Hydrology, Helmholtz Centre Potsdam, GFZ German Research Centre for
Geosciences, 14473 Potsdam, Germany
Markus Weiler
Hydrology, Faculty of Environment and Natural Resources, University of Freiburg, 79098 Freiburg, Germany
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Andreas Hänsler and Markus Weiler
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Axel Schaffitel, Tobias Schuetz, and Markus Weiler
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Robin Schwemmle, Dominic Demand, and Markus Weiler
Hydrol. Earth Syst. Sci., 25, 2187–2198, https://doi.org/10.5194/hess-25-2187-2021, https://doi.org/10.5194/hess-25-2187-2021, 2021
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Michael Rinderer, Jaane Krüger, Friederike Lang, Heike Puhlmann, and Markus Weiler
Biogeosciences, 18, 1009–1027, https://doi.org/10.5194/bg-18-1009-2021, https://doi.org/10.5194/bg-18-1009-2021, 2021
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We quantified the lateral and vertical subsurface flow (SSF) and P concentrations of three beech forest plots with contrasting soil properties during sprinkling experiments. Vertical SSF was 2 orders of magnitude larger than lateral SSF, and both consisted mainly of pre-event water. P concentrations in SSF were high during the first 1 to 2 h (nutrient flushing) but nearly constant thereafter. This suggests that P in the soil solution was replenished fast by mineral or organic sources.
Merle Koelbing, Tobias Schuetz, and Markus Weiler
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2021-24, https://doi.org/10.5194/hess-2021-24, 2021
Revised manuscript not accepted
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Based on a unique and comprehensive data set of urban micro-meteorological variables, which were observed with a mobile climate station, we developed a new method to transfer mesoscale reference potential evapotranspiration to the urban microscale in street canyons. Our findings can be transferred easily to existing urban hydrologic models to improve modelling results with a more precise estimate of potential evapotranspiration on street level.
Anne Hartmann, Markus Weiler, and Theresa Blume
Earth Syst. Sci. Data, 12, 3189–3204, https://doi.org/10.5194/essd-12-3189-2020, https://doi.org/10.5194/essd-12-3189-2020, 2020
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Our analysis of soil physical and hydraulic properties across two soil chronosequences of 10 millennia in the Swiss Alps provides important observation of the evolution of soil hydraulic behavior. A strong co-evolution of soil physical and hydraulic properties was revealed by the observed change of fast-draining coarse-textured soils to slow-draining soils with a high water-holding capacity in correlation with a distinct change in structural properties and organic matter content.
Daniel Beiter, Markus Weiler, and Theresa Blume
Hydrol. Earth Syst. Sci., 24, 5713–5744, https://doi.org/10.5194/hess-24-5713-2020, https://doi.org/10.5194/hess-24-5713-2020, 2020
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We investigated the interactions between streams and their adjacent hillslopes in terms of water flow. It could be revealed that soil structure has a strong influence on how hillslopes connect to the streams, while the groundwater table tells us a lot about when the two connect. This observation could be used to improve models that try to predict whether or not hillslopes are in a state where a rain event will be likely to produce a flood in the stream.
Maria Staudinger, Stefan Seeger, Barbara Herbstritt, Michael Stoelzle, Jan Seibert, Kerstin Stahl, and Markus Weiler
Earth Syst. Sci. Data, 12, 3057–3066, https://doi.org/10.5194/essd-12-3057-2020, https://doi.org/10.5194/essd-12-3057-2020, 2020
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The data set CH-IRP provides isotope composition in precipitation and streamflow from 23 Swiss catchments, being unique regarding its long-term multi-catchment coverage along an alpine–pre-alpine gradient. CH-IRP contains fortnightly time series of stable water isotopes from streamflow grab samples complemented by time series in precipitation. Sampling conditions, catchment and climate information, lab standards and errors are provided together with areal precipitation and catchment boundaries.
Conrad Jackisch, Samuel Knoblauch, Theresa Blume, Erwin Zehe, and Sibylle K. Hassler
Biogeosciences, 17, 5787–5808, https://doi.org/10.5194/bg-17-5787-2020, https://doi.org/10.5194/bg-17-5787-2020, 2020
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We developed software to calculate the root water uptake (RWU) of beech tree roots from soil moisture dynamics. We present our approach and compare RWU to measured sap flow in the tree stem. The study relates to two sites that are similar in topography and weather but with contrasting soils. While sap flow is very similar between the two sites, the RWU is different. This suggests that soil characteristics have substantial influence. Our easy-to-implement RWU estimate may help further studies.
Benjamin Fersch, Till Francke, Maik Heistermann, Martin Schrön, Veronika Döpper, Jannis Jakobi, Gabriele Baroni, Theresa Blume, Heye Bogena, Christian Budach, Tobias Gränzig, Michael Förster, Andreas Güntner, Harrie-Jan Hendricks Franssen, Mandy Kasner, Markus Köhli, Birgit Kleinschmit, Harald Kunstmann, Amol Patil, Daniel Rasche, Lena Scheiffele, Ulrich Schmidt, Sandra Szulc-Seyfried, Jannis Weimar, Steffen Zacharias, Marek Zreda, Bernd Heber, Ralf Kiese, Vladimir Mares, Hannes Mollenhauer, Ingo Völksch, and Sascha Oswald
Earth Syst. Sci. Data, 12, 2289–2309, https://doi.org/10.5194/essd-12-2289-2020, https://doi.org/10.5194/essd-12-2289-2020, 2020
Michael Stoelzle, Maria Staudinger, Kerstin Stahl, and Markus Weiler
Proc. IAHS, 383, 43–50, https://doi.org/10.5194/piahs-383-43-2020, https://doi.org/10.5194/piahs-383-43-2020, 2020
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The role of recharge and catchment storage is crucial to understand streamflow drought sensitivity. Here we introduce a model experiment with recharge stress tests as complement to climate scenarios to quantify the streamflow drought sensitivities of catchments in Switzerland. We identified a pre-drought period of 12 months as maximum storage-memory for the study catchments. From stress testing, we found up to 200 days longer summer streamflow droughts and minimum flow reductions of 50 %–80 %.
Cited articles
Akbar, S., Kathuria, A., and Maheshwari, B.: Combining imaging techniques with nonparametric modelling to predict seepage hotspots in irrigation channels, Irrig. Sci., 37, 11–23, https://doi.org/10.1007/s00271-018-0596-6, 2019.
Ali, G. A. and Roy, A. G.: Shopping for hydrologically representatice
connectivity metrics in a humid temperate forested catchment, Water Resour. Res., 46, W12544, https://doi.org/10.1029/2010WR009442, 2010.
Backhaus, K., Erichson, B., Plinke, W., and Weiber, R.: Multivariate
Analysemethoden – Eine anwendungsorientierte Einführung, 11th Edn.,
Springer, Heidelberg, 2006.
Beven, K. and Kirkby, M.: A physically based, variable contributing area model of basin hydrology, Hydrolog. Sci. Bull., 24, 43–69,
https://doi.org/10.1080/02626667909491834, 1979.
Bhamjee, R., Lindsay, J. B., and Cockburn, J.: Monitoring ephemeral headwater
streams: a paired-sensor approach, Hydrol. Process., 30, 888–898, https://doi.org/10.1002/hyp.10677, 2016.
Boulton, A. J., Rolls, R. J., Jaeger, K. L., and Datry, T.: Hydrological
Connectivity in Intermittent Rivers and Ephemeral Streams, 79–108,
https://doi.org/10.1016/B978-0-12-803835-2.00004-8, in: Intermittent Rivers and Ephemeral Streams, edited by: Datry, T., Bonada, N., and Boulton, A., Ecol. Manage., https://doi.org/10.1016/B978-0-12-803835-2.00004, 2017.
Bracken, L. J., Wainwright, J., Ali, G. A., Tetzlaff, D., Smith, M. W., Reaney, S. M., and Roy, A. G.: Concepts of hydrological connectivity: Research approaches, pathways and future agendas, Earth-Sci. Rev., 119, 17–34, 2013.
Buttle, J. M., Boon, S., Peters, D. L., Spence, C., van Meerveld, H. J., and
Whitfield, P. H.: An Overview of Temporary Stream Hydrology in Canada, Can. Water Resour. J., 37, 279–310, https://doi.org/10.4296/cwrj2011-903, 2012.
Cammeraat, L. H., Sevink, J., Hissler, C., Juilleret, J., Jansen, B., Kooijman, A. M., Pfister, L., and Verstraten, J. M.: Soils of the Luxembourg Lias Cuesta Landscape, in: The Luxembourg Gutland Landscape, edited by: Kooijman, A. M., Seijmonsbergen, A. C., and Cammeraat, L. H., Springer, Cham,, 107–130, https://doi.org/10.1007/978-3-319-65543-7_6, 2018.
Clausen, B. and Person, C. P.: Regional frequency analysis of annual maximum streamflow drought, J. Hydrol., 173, 111–130, 1995.
Conrad, O., Bechtel, B., Bock, M., Dietrich, H., Fischer, E., Gerlitz, L.,
Wehberg, J., Wichmann, V., and Boehner, J.: System for Automated Geoscientific Analyses (SAGA) v. 2.1.4. Geosci. Model Dev., 8, 1991–2007,
https://doi.org/10.5194/gmd-8-1991-2015, 2015.
Costigan, K. H., Jaeger, K. L., Goss, C. W., Fritz, K. M., and Goebel, P. C.:
Understanding controls on flow permanence in intermittent rivers aid ecological research: integrating meteorology geology and land cover, Ecohydrology, 9, 7, https://doi.org/10.1002/eco.1712, 2016.
Datry, D., Larned, S. T., and Tockner, K.: Intermittent Rivers: A Challenge for Freshwater Ecology, BioScience, 64, 229–235, https://doi.org/10.1093/biosci/bit027, 2014.
Datry, T., Bondana, N., and Boulton, A. J.: Chapter 1 – General introduction, in: Intermittent Rivers and Ephemeral Streams – Ecology and Management, edited by: Datry, T., Bondana, N., and Boulton, A. J., Academic Press, London, https://doi.org/10.1016/B978-0-12-803835-2.00001-2, 2017.
ESRI: Understanding curvature rasters, available at:
https://www.esri.com/arcgis-blog/products/product/imagery/understanding-curvature-rasters/, last access: 16 February 2020.
Famiglietti, J. S., Rudnicki, J. W., and Rodell, M.: Variability in surface
moisture content along a hillslope transect: Rattlesnake Hill, Texas, J. Hydrol., 210, 259–281, 1998.
Friedrich, K.: Digitale Reliefgliederungsverfahren zur Ableitung bodenkundlich relevanter Flaecheneinheiten, Frankfurter Geowissenschaftliche Arbeiten D 21, Frankfurt am Main, 1996.
Friedrich, K.: Multivariate distance methods for geomorphographic relief classification, in: Land Inforamtion Systems – Developments for planning the sustainable use of land resources, European Soil Bureau, Research Report 4, EUR 17729 EN, edited by: Heinecke, H., Eckelmann, W., Thomasson, A., Jones, J., Montanarella, L., and Buckley, B., Office for oficial publications of the European Communities, Ispra, 259–266, 1998.
Godsey, S. E. and Kirchner, J. W.: Dynamic, discontinuous stream networks:
hydrologically driven variations in active drainage density, flowing channels and stream order, Hydrol. Process., 28, 5791–5803, https://doi.org/10.1002/hyp.10310, 2014.
Goodrich, D. C., Kepner, W. G., Levick, L. R., and Wigington Jr., P. J.: Southwestern intermittent and ephemeral stream connectivity, J. Am. Water Resour. Assoc., 54, 400–422, https://doi.org/10.1111/1752-1688.12636, 2018.
Goulsbra, C. S., Lindsay, J. B., and Evans, M. G.: A new approach to the
application of electrical resistance sensors to measuring the onset of
ephemeral streamflow in wetland environments, Water Resour. Res., 45,
W09501, https://doi.org/10.1029/2009WR007789, 2009.
Guisan, A., Weiss, S. B., and Weiss, A. D.: GLM versus CCA spatial modelling of plant species distribution, Plant Ecol., 143, 107–122, 1999.
Habtezion, N., Nasab, M. T., and Chu, X.: How does DEM resolution affect
microtopographic characteristics, hydrologic connectivity, and modelling of
hydrologic processes?, Hydrol. Process., 30, 4870–4892, https://doi.org/10.1002/hyp.10967, 2016.
Hallema, D. W., Moussa, R., Sun, G., and McNulty, S.: Surface storm flow
prediction on hillslopes based on topography and hydrologic connectivity,
Ecol. Process., 5, 1–13, https://doi.org/10.1186/s13717-016-0057-1, 2016.
Hansen, W. F.: Identifying stream types and management implications, Forest
Ecol. Manage., 143, 39–46, 2001.
Hedman, E. R. and Osterkamp, W. R.: Streamflow Characteristics Related to
Channel Geometry of Streams in Western United States, USGS Water-Supply
Paper 2193, US Geological Survey, Washington, 1982.
Hellebrand, H., van den Bos, R., Hoffmann, L., Juilleret, J., and Pfister, L.: The potential of winter stormflow coefficients for hydrological regionalization purposes in poorly gauged basins of the middle Rhine region, Hydrolog. Sci. J., 53, 773–788, https://doi.org/10.1623/hysj.53.4.773, 2008.
Hewlett, J. D.: Principles of Forest Hydrology, University of Georgia Press, Athens, GA, USA, p. 192, ISBN9780820323800, 1982.
Jaeger, K. L. and Olden, J. D.: Electrical Resistance Sensor Arrays as a Means to Quantify Longitudinal Connectivity of Rivers, River Res. Appl., 28, 1843–1852, https://doi.org/10.1002/rra.1554, 2012.
Jaeger, K. L., Sutfin, N. A., Tooth, S., Mechaelides, K., and Singer, M.: Chapter 2.1 – Geomorphology and Sediment Regimes of Intermittent Rivers and
Ephemeral Streams, in: Intermittent Rivers and Ephemeral Streams – Ecology and Management, edited by: Datry, T., Bondana, N., and Boulton, A. J., Academic Press, London, https://doi.org/10.1016/B978-0-12-803835-2.00002-4, 2017.
Jaeger, K. L., Sando, R., McShane, R. R., Dunham, J. B., Hockman-Wert, D. P., Kaiser, K. E., Hafen, K., Risley, J. C., and Blasch, K. W.: Probability of Streamflow Permanence Model (PROSPER): A spatially continuous model of annual
streamflow permanence throughout the Pacific Northwest, J. Hydrol., 2, 100005, https://doi.org/10.1016/j.hydroa.2018.100005, 2019.
Jencso, K. G. and McGlynn, B. L.: Hierarchical controls on runoff generation:
Topographically driven hydrologic connectivity, geology, and vegetation, Water Resour. Res., 47, W11527, https://doi.org/10.1029/2011WR010666, 2011.
Jencso, K. G., McGlynn, B. L., Gooseff, M. N., Bencala, K. E., and Wondzell, S. M.: Hillslope hydrologic connectivity controls riparian groundwater turnover: Implications of catchment structure for riparian buffering and stream water sources, Water Resour. Res., 46, W10524, https://doi.org/10.1029/2009WR008818, 2010.
Jensen, C. K., McGuire, K. J., and Prince, P. S.: Headwater stream length dynamics across four physiographic provinces of the Appalachian Highlands,
Hydrol. Process., 31, 3350–3363, https://doi.org/10.1002/hyp.11259, 2017.
Jensen, C. K., McGuire, K. J., Shao, Y., and Dolloff, C. A.: Modeling wet headwater stream networks across multiole flow conditions in the Appalachian
Highlands, Earth Surf. Proc. Land., 43, 2762–2778, https://doi.org/10.1002/esp.4431, 2018.
Jensen, C. K., McGuire, K. J., McLaughlin, D. L., and Scott, D. T.: Quantifying spatiotemporal variation in headwater stream length using flow intermittency sensors, Environ. Monit. Assess., 191, 226, https://doi.org/10.1007/s10661-019-7373-8, 2019.
Kalyanapu, A. J., Burian, S. J., and McPherson, T. N.: Effect of land use-based surface roughness on hydrologic model output, J. Spat. Hydrol., 9, 51–71, 2009.
Kaplan, N. H., Sohrt, E., Blume, T., and Weiler, M.: Monitoring ephemeral,
intermittent and perennial streamflow: a dataset from 182 sites in the Attert catchment, Luxembourg, Earth Syst. Sci. Data, 11, 1363–1374, https://doi.org/10.5194/essd-11-1363-2019, 2019a.
Kaplan, N. H., Sohrt, E., Blume, T., and Weiler, M.: Time series of streamflow occurrence from 182 sites in ephemeral, intermittent and perennial streams in the Attert catchment, Luxembourg, GFZ Data Services, https://doi.org/10.5880/FIDGEO.2019.010, 2019b.
Keesstra, S., Nunes, J. P., Saco, P., Parsons, T., Poeppl, R., Masselink, R., and Cerdà, A.: The way forward: Can connectivity be useful to design better measuring and modelling schemes for water and sediment dynamics?, Sci. Total Environ., 644, 1557–1572, https://doi.org/10.1016/j.scitotenv.2018.06.342, 2018.
Lane, S. N., Reaney, S. M., and Heathwaite, A. L.: Representation of landscape hydrological connectivity using a topographically driven surface flow index, Water Resour. Res., 45, W08423, https://doi.org/10.1029/2008WR007336, 2009.
Le Gouvernement du Grand-Duché de Luxembourg – Administration du cadastre et de la topographie: Carte Topographique régionale touristique, R4 Steinfort, Redange, Luxembourg, 2009.
Le Gouvernement du Grand-Duché de Luxembourg: Layer: Umwelt, Biologie und Geologie; Gewässerschutz; Kläranlagen, available at:
http://map.geoportail.lu, last access: 10 December 2018.
Leigh, C., Boulton, A. J., Courtwright, J. L., Fritz, K., May, C. L., Walker, R. H., and Datry, T.: Ecological research and management of intermittent rivers: an historical review and future directions, Freshwater Biol., 61,
1181–1199, https://doi.org/10.1111/fwb.12646, 2015.
Lexartza-Artza, I. and Wainwright, J.: Hydrological connectivity: Linking
concepts with practical implications, Catena, 79, 146–152, https://doi.org/10.1016/j.catena.2009.07.001, 2009.
Martínez-Carreras, N., Krein, A., Gallart, F., Iffly, J.-F., Hissler, C.,
Pfister, L., Hoffmann, L., and Owens, P. N.: The Influence of Sediment Sources and Hydrologic Events on the Nutrient and Metal Content of Fine-Grained Sediments (Attert River Basin, Luxembourg), Water Air Soil Pollut., 223, 5685–5705, https://doi.org/10.1007/s11270-012-1307-1, 2012.
Matthews, W. J.: North American prairie streams as systems for ecological study, J. N. Am. Benthol. Soc., 7, 387–409, 1988.
Müller, B., Bernhardt, M., Jackisch, C., and Schulz, K.: Estimating spatially distributed soil texture using time series of thermal remote sensing – a case study in central Europe, Hydrol. Earth Syst. Sci., 20, 3765–3775, https://doi.org/10.5194/hess-20-3765-2016, 2016.
Nadeau, T.-L. and Rains, M. C.: Hydrological Connectivity Between Headwater
Streams and Downstream Waters: How Sience Can Inform Policy, J. Am. Water Resour. Assoc., 43, 118–133, 2007.
Olson, S. A. and Brouillette, M. C.: A logistic regression equation for
estimating the probability of a stream in Vermont having intermittent flow,
US Geological Survey Scientific Investigations Report 2006-5217, US Geological Survey, p. 15, available at: https://pubs.usgs.gov/sir/2006/5217/ (last acess: 16 November 2020),
2006.
Open Street Map Wiki: Key:Highway, available at:
https://wiki.openstreetmap.org/wiki/Key:highway, last access: 10 April 2020.
Ossa-Moreno, J., Keir, G., McIntyre, N., Cameletti, M., and Rivera, D.: Comparison of approaches to interpolating climate observations in steep terrain with low-density gauging networks, Hydrol. Earth Syst. Sci., 23, 4763–4781, https://doi.org/10.5194/hess-23-4763-2019, 2019.
Pfister, L., Wagner, C., Vansuypeene, E., Drogue, G., and Hoffmann, L.: Atlas climatique du grand-duché de Luxembourg, edited by: Ries, C., Musée National d'Histoire Naturelle, Société des naturalistes luxembourgeois, Centre de Recherche Public – Gabriel Lippmann, Administration des Services Techniques de l'Agriculture, Luxembourg, 2005.
Pfister, L., Martínez-Carreras, N., Hissler, C., Klaus, J., Carrer, G. E., Stewart, M. K., and McDonnell, J. J.: Bedrock geology controls on catchment storage, mixing, and release: A comparative analysis of 16 nested
catchments, Hydrol. Process., 31, 1828–1845, https://doi.org/10.1002/hyp.11134, 2017.
Pfister, L., Hissler, C., Iffly, J. F., Coenders, M., Teuling, R., Arens, A., and Cammeraat, L. H.: Contrasting Hydrologic Response in the Cuesta Landscapes of Luxembourg, in: The Luxembourg Gutland Landscape, edited by: Kooijman, A. M., Cammeraat, L. H., and Seijmonsbergen, A. C., Springer, Cham, 73–87, https://doi.org/10.1007/978-3-319-65543-7, 2018.
Philips, J. V. and Tadayon, S.: Selection of Mannings's Roughness Coefficient
for Natural and Constructed Vegetated and Non-Vegetated Channels, and
Vegetation Maintenance Plan Guidelines for Vegetated Channels in Central
Arizona, US Geological Survey Scientific Investigations Report 2006-5108,
US Geological Survey, p. 41, https://doi.org/10.3133/sir20065108, 2006.
Prancevic, J. P. and Kirchner, J. W.: Topographic Controls on the Extension and Retraction of Flowing Streams, Geophys. Res. Lett., 46, 2084–2092,
https://doi.org/10.1029/2018GL081799, 2019.
Riley, S. J., Degloria, S. D., and Elliot, R.: A Terrain Ruggedness Index that Quantifies Topographic Heterogeneity, Intermount. J. Sci., 5, 23–27, 1999.
Schaich, H., Karier, J., and Konold, W.: Rivers, Regulation and Restoration:
Land Use History of Floodplains in a Peri-Urban Landscape in Luxembourg,
1777–2000, Europ. Countrys, 4, 241–264, https://doi.org/10.2478/v10091-012-0007-6,
2011.
Service géologique de l'Etat: Carte géologique du Luxembourg,
Echelle 1:25 000/1:50 0000, Ancienne édition, 2018.
Shanafield, M. and Cook, P. G.: Transmission losses, infiltration and groundwater recharge through ephemeral and intermittent streambeds: A review
of applied methods, J. Hydrol., 511, 518–529, https://doi.org/10.1016/j.jhydrol.2014.01.068, 2014.
Skoulikidis, N. T., Sabater, S., Datry, T., Morais, M. M., Buffagni, A., Dörflinger, G., and Tockner, K.: Non-perennial Mediterranean rivers in Europe: status, pressures, and challenges for research and management, Sci. Total Environ., 577, 1–18, https://doi.org/10.1016/j.scitotenv.2016.10.147, 2017.
Sophocleous, M.: Interaction between groundwater and surface water: the state
of the science, Hydrogeol. J., 10, 52–67, https://doi.org/10.1007/s10040-001-0170-8, 2002.
Strahler, A. N.: Hypsometric (area-altitude) Analysis of Erosional Topography, Bull. Geol. Soc. Am., 63, 1117–1141, 1952.
Stromberg, J. C. and Merrit, D. M.: Riparian plant guilds of ephemeral,
intermittent and perennial rivers, Freshwater Biol., 61, 1259–1275,
https://doi.org/10.1111/fwb.12686, 2015.
Stubbington, R., England, J., Wood, P. J., and Sefton, C. E. M.: Temporary streams in temperate zones: recognizing, monitoring and restoring transitional aquatic-terrestrial ecosystems, WIREs Water, 4, 4, https://doi.org/10.1002/wat2.1223, 2017.
Svec, J. R., Kolka, R. K., and Stringer, J. W.: Defining perennial, intermittent, and ephemeral channels in Eastern Kentucky: Application to forestry best management practices, Forest Ecol. Manage., 214, 170–182,
https://doi.org/10.1016/j.foreco.2005.04.008, 2005.
Texas Forest Service: The Texas Water Source – updating Cass and Marion Co. Forest Landowners on Forestry and Water Issues, March 2009, available at: https://tfsdev.tamu.edu/uploadedFiles/TFSMain/Manage_Forest_and_Land/Water_Resources_and_BMPs/Stewardship(1)/TexasWaterSource-Mar2009-color-forwebsite.pdf (last access: 16 November 2020), 2009.
Van der Ploeg, T., Austin, P. C., and Steyerberg, E. W.: Modern modelling
techniques are data hungry: a simulation study for predicting dichotomous
endpoints, BMC Med. Res. Methodol., 14, 137, https://doi.org/10.1186/1471-2288-14-137, 2014.
Van Genuchten, M. T.: A Closed-form Equation for Predicting the Hydraulic
Conductivity of Unsaturated Soils, Soil Sci. Soc. Am. J., 44, 892, https://doi.org/10.2136/sssaj1980.03615995004400050002x, 1980.
Weiler, M. and McDonnell, J. J.: Conceptualizing lateral preferential flow and flow networks and simulating the effects on gauged and ungauged hillslopes, Water Resour. Res., 43, W03403, https://doi.org/10.1029/2006WR004867, 2007.
Wösten, J. H. M., Lilly, A., Nemes, A., and Le Bas, C.: Development and use of a database of hydraulic properties of European soils, Geoderma, 90, 169–185, 2001.
Wrede, S., Fenicia, F., Martínez-Carreras, N., Juilleret, J., Hissler, C., Krein, A., Savenjie, H. H. G., Uhlenbrook, S., Kavetski, D., and Pfister, L.: Towards more systematic perceptual model development: a case study using 3 Luxembourgish catchments, Hydrol. Process., 29, 2731–2750,
https://doi.org/10.1002/hyp.10393, 2014.
Zehe, E., Ehret, U., Pfister, L., Blume, T., Schröder, B., Westhoff, M.,
Jackisch, C., Schymanski, S. J., Weiler, M., Schulz, K., Allroggen, N., Tronicke, J., van Schaik, L., Dietrich, P., Scherer, U., Eccard, J., Wulfmeyer, V., and Kleidon, A.: HESS Opinions: From response units to functional units: a thermodynamic reinterpretation of the HRU concept to link spatial organization and functioning of intermediate scale catchments, Hydrol. Earth Syst. Sci., 18, 4635–4655, https://doi.org/10.5194/hess-18-4635-2014, 2014.
Ziegler, A. D. and Giambelluca, T. W.: Importance of rural roads as source areas for runoff in mountainous areas of northern Thailand, J. Hydrol., 196, 204–229, 1997.
Zimmer, M. A. and McGlynn, B. L.: Ephemeral and intermittent runoff generation processes in a low relief, highly weathered catchment, Water Resour. Res., 53, 7055–7077, https://doi.org/10.1002/2016WR019742, 2017.
Short summary
In recent decades the demand for detailed information of spatial and temporal dynamics of the stream network has grown in the fields of eco-hydrology and extreme flow prediction. We use temporal streamflow intermittency data obtained at various sites using innovative sensing technology as well as spatial predictors to predict and map probabilities of streamflow intermittency. This approach has the potential to provide intermittency maps for hydrological modelling and management practices.
In recent decades the demand for detailed information of spatial and temporal dynamics of the...
