Glacier Advance

Glacier Advance is a geomorphological process denoting the forward movement of a glacier's terminus relative to its bed, resulting from a positive mass balance that causes the ice front to extend downvalley over successive years.

357

Publications

19.9K

Citations

949

Authors

389

Institutions

Publications per year

2017–2026

65

Authors

949

  1. SI
    Susan Ivy‐Ochs

    ETH Zurich, Switzerland

    11 publications · 1.3K citations

    11

    h-index

  2. AS
    Anders Schomacker

    University of Iceland, Iceland

    9 publications · 394 citations

    9

    h-index

  3. JJ
    John J. Clague

    Simon Fraser University, Canada

    8 publications · 298 citations

    8

    h-index

  4. ÓI
    Ólafur Inǵólfsson

    University of Iceland, Iceland

    8 publications · 345 citations

    8

    h-index

  5. MC
    Marcus Christl

    ETH Zurich, Switzerland

    7 publications · 258 citations

    7

    h-index

1–5 of 949

Venues

  1. Journal of Glaciology

    40 publications · 1.9K citations

    23

    h-index

  2. Quaternary Research

    QR · 24 publications · 2.1K citations

    20

    h-index

  3. The Holocene

    23 publications · 1.4K citations

    18

    h-index

  4. Boreas

    21 publications · 776 citations

    17

    h-index

  5. Canadian Journal of Earth Sciences

    15 publications · 1K citations

    15

    h-index

1–5