Proglacial Runoff

Proglacial Runoff is a hydrological flux representing the portion of meltwater discharge originating from glacial ablation that flows beyond the glacier margin and contributes to downstream fluvial systems, distinguished from other forms of glacial runoff by its emergence at the glacier terminus and subsequent routing through proglacial terrain.

65

Publications

2.8K

Citations

240

Authors

136

Institutions

Publications per year

2017–2026

23

Authors

240

  1. MT
    Martyn Tranter

    University of Bristol, United Kingdom

    4 publications · 157 citations

    4

    h-index

  2. BS
    Bettina Schaefli

    École Polytechnique Fédérale de Lausanne, Switzerland

    3 publications · 74 citations

    3

    h-index

  3. SN
    Stuart N. Lane

    University of Lausanne, Switzerland

    3 publications · 74 citations

    3

    h-index

  4. JL
    Jonathan L. Carrivick

    University of Leeds, United Kingdom

    3 publications · 186 citations

    3

    h-index

  5. DV
    D. van As

    Geological Survey of Denmark and Greenland, Denmark

    3 publications · 189 citations

    3

    h-index

1–5 of 240

Venues

  1. Hydrological Processes

    10 publications · 449 citations

    10

    h-index

  2. Journal of Hydrology

    8 publications · 307 citations

    8

    h-index

  3. Geomorphology

    4 publications · 170 citations

    4

    h-index

  4. Water Resources Research

    4 publications · 134 citations

    4

    h-index

  5. Journal of Glaciology

    3 publications · 103 citations

    3

    h-index

1–5