Supraglacial Runoff

Supraglacial Runoff is a hydrological process denoting the meltwater flow that occurs over the surface of a glacier or ice sheet, distinguished from other forms of glacial runoff by its routing across supraglacial channels, depressions, and networks prior to entering the subglacial or englacial system.

43

Publications

2.2K

Citations

140

Authors

90

Institutions

Publications per year

2017–2026

22

Authors

140

  1. LC
    L. C. Smith

    University of California, Los Angeles, United States

    12 publications · 819 citations

    12

    h-index

  2. KY
    Kang Yang

    Nanjing University, China

    11 publications · 720 citations

    11

    h-index

  3. ML
    Manchun Li

    Nanjing University, China

    7 publications · 218 citations

    7

    h-index

  4. LH
    L. H. Pitcher

    University of California, Los Angeles, United States

    5 publications · 546 citations

    5

    h-index

  5. ÅK
    Å. K. Rennermalm

    Rutgers, The State University of New Jersey, United States

    4 publications · 439 citations

    4

    h-index

1–5 of 140

Venues

  1. Journal of Glaciology

    5 publications · 289 citations

    5

    h-index

  2. Journal of Geophysical Research Earth Surface

    3 publications · 130 citations

    3

    h-index

  3. Journal of Hydrology

    3 publications · 106 citations

    3

    h-index

  4. ˜The œcryosphere

    3 publications · 71 citations

    3

    h-index

  5. Geophysical Research Letters

    3 publications · 112 citations

    3

    h-index

1–5