Proglacial Streamflow

Proglacial Streamflow is a hydrological construct that denotes the freshwater discharge originating from glacial meltwater and supraglacial, englacial, and subglacial fluxes, routed through and modified by sediment-laden proglacial river systems downstream of the glacier terminus, distinguished from other fluvial regimes by its direct dependency on glacier-derived inputs and strong diurnal and seasonal melt forcings.

86

Publications

4.1K

Citations

253

Authors

128

Institutions

Publications per year

2017–2026

15

Authors

253

  1. IW
    Ian Willis

    University of Cambridge, United Kingdom

    8 publications · 507 citations

    8

    h-index

  2. MT
    Martyn Tranter

    University of Bristol, United Kingdom

    6 publications · 286 citations

    6

    h-index

  3. AM
    Angela M. Gurnell

    Queen Mary University of London, United Kingdom

    5 publications · 302 citations

    5

    h-index

  4. RH
    Richard Hodgkins

    Royal Holloway University of London, United Kingdom

    4 publications · 112 citations

    4

    h-index

  5. WB
    W. Berry Lyons

    The Ohio State University, United States

    4 publications · 140 citations

    4

    h-index

1–5 of 253

Venues

  1. Hydrological Processes

    19 publications · 698 citations

    17

    h-index

  2. Journal of Hydrology

    8 publications · 383 citations

    8

    h-index

  3. Journal of Glaciology

    3 publications · 160 citations

    3

    h-index

  4. Earth Surface Processes and Landforms

    3 publications · 170 citations

    3

    h-index

  5. Geomorphology

    2 publications · 63 citations

    2

    h-index

1–5