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Showing 1 to 8 of 8 for “"Gravel Bed River"”.

  1. Cottonwood Establishment in a Gravel-Bed River

    … pristine, 5th order, wandering floodplain of the gravel-bed Flathead River, Montana, USA. The focus of my research was to determine the mechanisms explaining successful recruitment on recently formed, unvegetated bars, covering a range of spatial scales from within-bar (~ 1 to 10 m) to …

    montana-tech Repository record for Cottonwood Establishment in a Gravel-Bed River (opens in a new tab)

  2. Cottonwood Establishment in a Gravel-Bed River

    … pristine, 5th order, wandering floodplain of the gravel-bed Flathead River, Montana, USA. The focus of my research was to determine the mechanisms explaining successful recruitment on recently formed, unvegetated bars, covering a range of spatial scales from within-bar (~ 1 to 10 m) to …

    montana Repository record for Cottonwood Establishment in a Gravel-Bed River (opens in a new tab)

  3. Temporal and Spatial Variation of Fine Sediment Infiltration in a Gravel-Bed River

    Pulses of fine sediment in gravel-bedded rivers can cause extensive fine sediment infiltration (FSI), potentially altering river morphodynamics and aquatic ecosystems. FSI occurs when sand and silt are deposited into void spaces between larger grains at the riverbed. Flume and theoretical modeling …

    montana-tech Repository record for Temporal and Spatial Variation of Fine Sediment Infiltration in a Gravel-Bed River (opens in a new tab)

  4. Temporal and Spatial Variation of Fine Sediment Infiltration in a Gravel-Bed River

    Pulses of fine sediment in gravel-bedded rivers can cause extensive fine sediment infiltration (FSI), potentially altering river morphodynamics and aquatic ecosystems. FSI occurs when sand and silt are deposited into void spaces between larger grains at the riverbed. Flume and theoretical modeling …

    montana Repository record for Temporal and Spatial Variation of Fine Sediment Infiltration in a Gravel-Bed River (opens in a new tab)

  5. Riparian Seedling Establishment Defined by Sediment Mobilization and Water Availability In a Gravel Bed River

    Stream hydrograph and morphology are the main drivers of riparian white alder distribution. White alder seeds are preferentially deposited on stream bars where stream morphology and flow result in eddies. This thesis predicts the establishment success of riparian seedlings as a function of root …

    calgary Repository record for Riparian Seedling Establishment Defined by Sediment Mobilization and Water Availability In a Gravel Bed River (opens in a new tab)

  6. Spatial patterns and drivers of floodplain change in the Squamish River, a dynamic gravel bed river

    Submission original under an indefinite embargo labeled 'Open Access'. The submission was exported from vireo on 2024-03-01 without embargo terms

    uiuc Repository record for Spatial patterns and drivers of floodplain change in the Squamish River, a dynamic gravel bed river (opens in a new tab)

  7. Multi-Scale detection, mapping, and modelling geomorphic change in gravel-bed rivers with UAV remote sensing

    … are produced for a 2km reach of quasi-wandering gravel-bed river. Comparative analyses of DEMs between 2016 and 2018 reveals widening of the incised margin and significant geomorphic evolution characteristic of re-naturalization following the termination of gravel mining, channelization, and …

    salford Repository record for Multi-Scale detection, mapping, and modelling geomorphic change in gravel-bed rivers with UAV remote sensing (opens in a new tab)

  8. Developing GPS river flow tracers (GRiFTers) to investigate large scale river flow phenomena

    Existing flow measurement methods in natural gravel rivers are largely based on a series of point measurements detached from the dynamic nature of river flow. Traditional measurement methods are limited in many environments and locations due to an inability to access directly the channel; this …

    hull Repository record for Developing GPS river flow tracers (GRiFTers) to investigate large scale river flow phenomena (opens in a new tab)