Glacial Advance

Glacial Advance is a geomorphological process denoting the forward movement of a glacier's terminus due to a positive mass balance, wherein ice accumulation exceeds ablation over successive years.

517

Publications

28.1K

Citations

1.5K

Authors

607

Institutions

Publications per year

2017–2026

80

Authors

1.5K

  1. CS
    Christian Schlüchter

    University of Bern, Switzerland

    10 publications · 698 citations

    10

    h-index

  2. SI
    Susan Ivy‐Ochs

    ETH Zurich, Switzerland

    9 publications · 772 citations

    9

    h-index

  3. PW
    Peter W. Kubik

    ETH Zurich, Switzerland

    9 publications · 598 citations

    9

    h-index

  4. MW
    Marc W. Caffee

    Purdue University West Lafayette, United States

    8 publications · 621 citations

    8

    h-index

  5. GH
    Gifford H. Miller

    Institute of Arctic and Alpine Research, United States

    7 publications · 473 citations

    7

    h-index

1–5 of 1.5K

Venues

  1. Quaternary Research

    QR · 40 publications · 3.4K citations

    29

    h-index

  2. Canadian Journal of Earth Sciences

    31 publications · 1.7K citations

    23

    h-index

  3. Quaternary Science Reviews

    26 publications · 1.4K citations

    22

    h-index

  4. Journal of Quaternary Science

    JQS · 26 publications · 1.8K citations

    22

    h-index

  5. Boreas

    35 publications · 1.5K citations

    22

    h-index

1–5