Streamflow monitoring at high temporal resolution based on non-contact instruments in the Galabre river (Southern pre-Alps, France)

We provide a dataset for calculating streamflow in a river of the Southern pre-Alps in France over the period October 2018 to May 2021. The river is called the Galabre and is a tributary of the Bès, which in turn is a tributary of the Bléone. The hydrometric station, so-called RIPLE, which incorporates non-contact instruments, was described in detail by Nord et al (2020). It was installed at a site subject to frequent bathymetric changes, 2.5 km downstream of a historic hydrometric station called « La Robine », at the "Galabre" site of the Draix-Bléone observatory (https://draixbleone.osug.fr/). The dataset combines high-frequency monitoring (every 10 minutes) of water level and surface water velocity using radar, ground-based bathymetric surveys, video sequences recorded by fixed camera with velocity fields obtained using the Fudaa-LSPIV software (https://forge.irstea.fr/projects/fudaa-lspiv), and the results of theoretical models of velocity field distribution in the river section. Nord, G., Michielin, Y., Biron, R., Esteves, M., Freche, G., Geay, T., et al. (2020). An autonomous low-power instrument platform for monitoring water and solid discharges in mesoscale rivers. Geoscientific Instrumentation, Methods and Data Systems, 9(1), 41–67. https://doi.org/10.5194/gi-9-41-2020
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- LSPIV.zip
- H-Awet_ratings.zip
- Table_results_LSPIV_Isovels_QCommander.csv
- Q_time_series.csv
- bathymetry_of_LSPIV_cross-sections.csv
- readme.txt
- Quality_codes.txt
- Hrad-Vrad_time_series.csv
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- Streamflow monitoring at high temporal resolution based on non-contact instruments in a river prone to bathymetric shifts This study presents a reliable methodology for monitoring streamflow in a dynamic river of the Alps prone to bathymetric changes using non-contact instruments. The method relies on water level and surface velocity radar monitoring, discharge measurements by Large-Scale Particle Image Velocimetry (LSPIV), and topographic surveys. A single proportional relation, resistant to bathymetric changes, is established between maximum surface velocity (Vs,max) and bulk velocity (Umean). Different methods are used to build this relation: (i) an empirical approach calibrated with the LSPIV measurements; (ii) the Isovel model; (iii) the Q-Commander software developed by the Sommer company. The applicability of the method is tested over a 2.5-year dataset. Compared to the empirical approach, both models, which require minimal input data, predict well the Vs,max-Umean relation. The location of the maximum surface velocity, which reveals to be resistant to bathymetric changes, is also well predicted by these models. Discharge is calculated at a time step of 10 min by multiplying the bulk velocity and the wetted area. The results are compared to the discharge series at the historical station located 2.5 km further upstream, which has a stage-discharge rating curve. Good agreement is observed when surface velocity is above 0.7 m/s, but accuracy decreases for lower velocities. A simplified uncertainty analysis estimates a 20% relative error on discharge calculated with the presented method.
- Fudaa software Software adapted to LSPIV (Large-Scale Particle Image Velocimetry) for surface velocity and discharge applications in open channel
- An autonomous low-power instrument platform for monitoring water and solid discharges in mesoscale rivers We present the development of the River Platform for Monitoring Erosion (RIPLE) designed for monitoring at high temporal frequency (∼10 min) of water discharge, solid fluxes (bedload and suspended load) and properties of fine particles (settling velocity) in mesoscale rivers, i.e. which drain mesoscale catchments (≈10–103 km2). This platform responds to a request to continuously measure these variables in rivers using a single, centralized device, and to do this in the most direct way possible. The platform integrates the following instruments: (i) for water discharge, water level radar, and surface velocity radar, digital cameras and an echo sounder; (ii) for fine sediment load, turbidimeters and automatic samplers including the SCAF (a sediment settling velocity characterization device); (iii) for bedload, a hydrophone; and (iv) for water quality, a conductivity probe and water sampling. As far as water discharge monitoring is concerned, priority has been given to non-intrusive instruments to improve the robustness of the system. All the instruments are driven by a data logger (Campbell® CR6), which locally stores the data and then uploads them to a remote server every hour during the day using a 3G modem. SMS (Short Message Service) alerts can be sent depending on scheduled conditions (e.g. low battery voltage, water level threshold, all samples of the automatic sampler collected). The platform has been designed to be as autonomous as possible: it is powered by a battery that is supplied by a solar panel. Limiting the power consumption of the platform was one of the main technical challenges because of the quantity of instruments integrated. A simple 100 W solar panel is sufficient to power the entire platform, even during winter or low insulation conditions. A user-friendly interface has been developed, enabling to visualize the data collected by the platform from an internet connection. It is also possible to remotely configure the platform within this interface, e.g. to modify water sampling thresholds or alert thresholds. Finally, the platform is relatively easy to move from one site to another, because its installation requires little civil engineering. To date, RIPLE has been tested on two rivers of the Alps in France: the Romanche river in Bourg d'Oisans from September 2016 to July 2018 and the Galabre river in La Robine sur Galabre since October 2018, demonstrating the proper functioning of the platform.
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