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3 results for “Proglacial forefield”
Suspended sediment load and bedload flux from the Glacier d'Otemma proglacial forefield (summers 2020 and 2021)
<p>The Glacier d’Otemma proglacial margin, located in the Swiss Alps at an altitude of about 2450 m a.s.l. (45.93423 N, 7.41160 E), is characterized by a ca. 1 km long by 200 m wide active braided forefield. In this setting we installed two gauging stations for the monitoring of both suspended sediment and bedload transport within the proglacial margin: GS1 at about 350 m from the glacier terminus and GS2 at the forefield outlet.</p> <p>Monitoring stations were equipped with water pressure sensors (CS451 from Cambell Scientific), turbidity probes (OBS300+ from Cambell Scientific) and geophones (3-components PE-6/B from Sensor Nederland connected to a DiGOS DATA-CUBE type 2 logger). Water discharge were determined following modalities described in Müller and Miesen (2022). Suspended loads were quantified using a conventional turbidity-suspended sediment concentration relationship, while bedload transport was derived seismically using the geophysical Fluvial model inversion (FMI) algorithm developed in Dietze et al. (2018). The dataset covers summers 2020 and 2021.</p> <p> Further details on data aquisition and post-processing techniques are available in Mancini et al. (2023).</p>
Temporal morphodynamic evolution of the Glacier d'Otemma proglacial forefield for melt seasons 2020 and 2021: data collection and post-processing
<p><span>The data included in this dataset concern the continuous geomorphic (orthomosaics, DEMs, inundation maps) and sedimentological (grain-size maps) evolution of the Glacier d’Otemma proglacial margin (Southern-Western Swiss Alps) located at an altitude of ca. 2450 m a.s.l. during summer 2020 and 2021. </span></p> <p><span>Data details and formats are available in the pdf document. Further information on data aquisition and post-processing techniques are available in Mancini et al. (2024).</span></p>
Simulations of proglacial forefield morphodynamics and sediment transport to changing boundary conditions
<p>This dataset includes the simulated sediment flux records, stream statistics (braiding index and bar proprieties), DEMs and inundation maps of a proglacial forefield under different boundary conditions. Further information are available in: </p> <p>Mancini, D., Nicholas, A.P., Roncoroni, M., Müller, T., Jenkin, M., Miesen, F., Dietze, M., Calvo, F. & Lane, S.N. (submitted). Simulations of proglacial forefield morphodynamics and their implications for the filtering of subglacial sediment export following glacier retreat. <em>Earth Surface Processes and Landforms</em>.</p> <p>General information:</p> <ul> <li>Domain size: 462 x 125 pixels</li> <li>Time step (sediment fluxes): 0.005 days</li> <li>Time tep (inundation maps, DEMs and stream stats): 0.2 days</li> </ul> <p>The model used to produce them is called eRiDynaS, and enquiries regarding its availability should be directed to a.p.nicholas@exeter.ac.uk.</p>
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