Parabolic Dunes

Parabolic Dune is a type of aeolian landform characterized by a U-shaped morphology with elongated, trailing limbs that are stabilized by vegetation, distinguishing it from other dune forms through its fixed margins and active, downwind-curving nose resulting from sediment erosion in the central zone.

129

Publications

6K

Citations

323

Authors

162

Institutions

Publications per year

2017–2026

21

Authors

323

  1. PA
    Patrick A. Hesp

    Flinders University, Australia

    6 publications · 184 citations

    6

    h-index

  2. CH
    Chris H. Hugenholtz

    University of Calgary, Canada

    5 publications · 165 citations

    5

    h-index

  3. AB
    Andreas Baas

    King's College London, United Kingdom

    5 publications · 454 citations

    5

    h-index

  4. SA
    S A Wolfe

    Geological Survey of Canada, Canada

    4 publications · 193 citations

    4

    h-index

  5. MS
    Matti Seppälä

    University of Helsinki, Finland

    5 publications · 151 citations

    4

    h-index

1–5 of 323

Venues

  1. Earth Surface Processes and Landforms

    14 publications · 834 citations

    14

    h-index

  2. Quaternary Research

    QR · 12 publications · 359 citations

    12

    h-index

  3. Geomorphology

    11 publications · 639 citations

    11

    h-index

  4. Journal of Coastal Research

    JCR · 10 publications · 284 citations

    10

    h-index

  5. Canadian Journal of Earth Sciences

    8 publications · 366 citations

    8

    h-index

1–5