Transient Creep

Transient Creep is a time-dependent deformation phase in ice rheology, within the broader category of creep behavior, distinguished by a decreasing strain rate under constant stress due to the progressive alignment of ice crystals and suppression of dislocation mobility.

277

Publications

15.1K

Citations

651

Authors

327

Institutions

Publications per year

2017–2026

46

Authors

651

  1. PD
    P. Duval

    Laboratoire de Glaciologie et Géophysique de l’Environnement, France

    8 publications · 901 citations

    8

    h-index

  2. SK
    Seiichi Karashima

    Tohoku University, Japan

    5 publications · 157 citations

    5

    h-index

  3. JF
    Jean‐Marc Franssen

    University of Liège, Belgium

    4 publications · 167 citations

    4

    h-index

  4. VK
    Venkatesh Kodur

    Michigan State University, United States

    4 publications · 118 citations

    4

    h-index

  5. DA
    David A. Yuen

    University of Minnesota, United States

    4 publications · 202 citations

    4

    h-index

1–5 of 651

Venues

  1. Journal of Geophysical Research Solid Earth

    12 publications · 411 citations

    12

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 11 publications · 773 citations

    11

    h-index

  3. Geophysical Journal International

    GJI · 10 publications · 1.3K citations

    10

    h-index

  4. physica status solidi (a)

    9 publications · 251 citations

    9

    h-index

  5. Geophysical Research Letters

    9 publications · 332 citations

    9

    h-index

1–5