Inertial Gravity Waves

Inertial Gravity Waves is a type of atmospheric or oceanic wave that results from the restoring forces of buoyancy and the Coriolis effect, distinguished by its propagation in stably stratified rotating fluids where oscillations occur at frequencies between the inertial and buoyancy frequencies.

224

Publications

9.9K

Citations

447

Authors

243

Institutions

Publications per year

2017–2026

35

Variants

Inertial-gravity Waves

Authors

447

  1. SZ
    Shaodong Zhang

    Wuhan University, China

    11 publications · 297 citations

    11

    h-index

  2. JV
    Jacques Vanneste

    University of Edinburgh, United Kingdom

    10 publications · 603 citations

    10

    h-index

  3. RP
    Riwal Plougonven

    Laboratoire de Météorologie Dynamique, France

    9 publications · 583 citations

    9

    h-index

  4. CH
    Chunming Huang

    Wuhan University, China

    9 publications · 206 citations

    9

    h-index

  5. KS
    K. Sato

    The University of Tokyo, Japan

    9 publications · 511 citations

    9

    h-index

1–5 of 447

Venues

  1. Journal of the Atmospheric Sciences

    45 publications · 2.7K citations

    29

    h-index

  2. Journal of Fluid Mechanics

    26 publications · 1K citations

    18

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 13 publications · 633 citations

    13

    h-index

  4. Geophysical Research Letters

    12 publications · 519 citations

    12

    h-index

  5. Journal of Physical Oceanography

    10 publications · 330 citations

    10

    h-index

1–5