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Klösch, Mario; Pessenlehner, Sebastian; Gmeiner, Philipp; Habersack, Helmut (2024): Time series of bed shear stress in the cross section of the seeding locations of bedload tracers in an alpine section of the Drava River between 11 May 2018 and 11 June 2018 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.969742, In: Klösch, M et al. (2024): Data set from a bedload tracer field study in an alpine section of the Drava River in 2017 and 2018 [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.969734

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Published: 2024-08-20DOI registered: 2024-09-18

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Abstract:
This is a data set related to a bedload tracer field study in an alpine section of the Drava River between 11 May 2017 and 11 June 2018. A time series of bed shear stress is provided for the seeding site of the tracers in the time span of the entire tracer study. The shear stress was calculated from water depths that were modelled with a one-dimensional hydrodynamic-numerical model and based on a channel slope obtained from the analysis of cross-sections. The shear stress can also be calculated for cross-sections downstream of the seeding location by using the functions available in the corresponding publication.
Keyword(s):
Active VHF transmitters; Bedload tracers; Bedload velocity; Drava River; Gravel-bed River; Gravel mobility; Tracer slowdown
Related to:
Klösch, Mario; Pessenlehner, Sebastian; Gmeiner, Philipp; Habersack, Helmut (2024): Tracer velocity versus bedload velocity: Derivation of the unsteady virtual bedload velocity from decelerating tracers. Water Resources Research, 60, e2023WR034823, https://doi.org/10.1029/2023WR034823
References:
Ferguson, R I; Wathen, S J (1998): Tracer-pebble movement along a concave river profile: Virtual velocity in relation to grain size and shear stress. Water Resources Research, 34(8), 2031-2038, https://doi.org/10.1029/98WR01283
Funding:
Austrian Academy of Sciences, grant/award no. ESS22-35: Improving the Hydromorphology of Alpine Rivers in the Provision of Ecosystem Services through Responsible, Resilient River Restoration (HyMo4us!)
European Regional Development Fund (ERDF), grant/award no. ASP 445: HydroMorphological assessment and management at basin scale for the Conservation of Alpine Rivers and related Ecosystem Services (HyMoCARES)
Coverage:
Latitude: 46.738902 * Longitude: 13.017718
Date/Time Start: 2017-05-10T22:00:00 * Date/Time End: 2018-06-11T22:00:00
Event(s):
Drava_shear_stress * Latitude: 46.738902 * Longitude: 13.017718 * Date/Time Start: 2017-05-10T22:00:00 * Date/Time End: 2018-06-11T22:00:00 * Method/Device: Field experiment
Comment:
Water depths were modelled with one-dimensional HEC-RAS (US Army Corps of Engineers Hydrologic Engineering Center). A water depth midway between the mean and maximum water depths was calculated aiming to better simulate conditions for bedload (following Ferguson and Wathen, 1998). A power function with coefficient and exponent depending on the streamwise distance (see related publication) was then used to convert the discharge time series into a time series of bedload-related water depth at the seeding location. The shear stress was calculated via ρgDS. The underlying discharge time series was obtained from the gauging station at Dellach from the Hydrographic Service Carinthia.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DATE/TIMEDate/TimeKlösch, MarioGeocode – GMT
2Shear stress, river bedShear stressN/m2Klösch, Mariosee comment
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
38113 data points

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