Thermal Erosion

Thermal Erosion is a geomorphic process in which permafrost-dominated coastal landscapes are degraded through the combined effects of heat transfer and mechanical removal of material by seawater or runoff, distinguishing it from purely mechanical erosion by emphasizing thermal dissolution as the primary preparatory mechanism.

267

Publications

17.4K

Citations

805

Authors

389

Institutions

Publications per year

2017–2026

36

Authors

805

  1. DA
    D. A. Williams

    Arizona State University, United States

    7 publications · 490 citations

    7

    h-index

  2. GG
    Guido Grosse

    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany

    7 publications · 663 citations

    7

    h-index

  3. DF
    Daniel Fortier

    Université de Montréal, Canada

    7 publications · 608 citations

    7

    h-index

  4. FC
    F. Costard

    Université Paris-Sud, France

    7 publications · 384 citations

    7

    h-index

  5. RG
    R. Greeley

    Arizona State University, United States

    6 publications · 393 citations

    6

    h-index

1–5 of 805

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 24 publications · 1.7K citations

    20

    h-index

  2. Wear

    15 publications · 863 citations

    15

    h-index

  3. Permafrost and Periglacial Processes

    12 publications · 990 citations

    12

    h-index

  4. Geophysical Research Letters

    9 publications · 683 citations

    9

    h-index

  5. Earth and Planetary Science Letters

    9 publications · 484 citations

    9

    h-index

1–5