Inertia-gravity Waves

Inertia-Gravity Waves is a type of equatorial atmospheric wave in which the restoring forces are a combination of gravitational buoyancy and the Coriolis effect, distinguished from other equatorial waves by its dependence on both stratification and rotation for wave propagation.

349

Publications

16.5K

Citations

650

Authors

305

Institutions

Publications per year

2017–2026

60

Variants

Inertial-gravity Waves

Authors

650

  1. KS
    K. Sato

    The University of Tokyo, Japan

    19 publications · 877 citations

    18

    h-index

  2. VZ
    Vladimir Zeitlin

    Laboratoire de Météorologie Dynamique, France

    12 publications · 525 citations

    12

    h-index

  3. JV
    Jacques Vanneste

    University of Edinburgh, United Kingdom

    11 publications · 653 citations

    11

    h-index

  4. RP
    Riwal Plougonven

    Laboratoire de Météorologie Dynamique, France

    11 publications · 806 citations

    11

    h-index

  5. TJ
    Timothy J. Dunkerton

    Northwest Research Associates, United States

    10 publications · 1.4K citations

    10

    h-index

1–5 of 650

Venues

  1. Journal of the Atmospheric Sciences

    78 publications · 4.7K citations

    42

    h-index

  2. Journal of Fluid Mechanics

    39 publications · 1.4K citations

    22

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 25 publications · 1.8K citations

    20

    h-index

  4. Monthly Weather Review

    19 publications · 1.5K citations

    18

    h-index

  5. Geophysical Research Letters

    16 publications · 611 citations

    16

    h-index

1–5