Tropical Planetary Waves

Tropical Planetary Waves is a large-scale atmospheric wave phenomenon in the tropical troposphere characterized by eastward- or westward-propagating oscillations in wind, pressure, and geopotential height that arise from the meridional gradient of the Coriolis parameter and are modulated by convective heating, distinguishing it from mid-latitude planetary waves and other tropical disturbances through its zonal wavenumber structure and association with the equatorial beta plane dynamics.

174

Publications

14.7K

Citations

460

Authors

205

Institutions

Publications per year

2017–2026

27

Variants

Equatorial Planetary Waves

Authors

460

  1. JM
    John M. Wallace

    University of Washington, United States

    6 publications · 826 citations

    6

    h-index

  2. RR
    Rolando R. García

    NSF National Center for Atmospheric Research, United States

    5 publications · 576 citations

    5

    h-index

  3. WC
    Wen Chen

    Chinese Academy of Sciences, China

    4 publications · 180 citations

    4

    h-index

  4. BM
    Brian Mapes

    University of Miami, United States

    4 publications · 861 citations

    4

    h-index

  5. KK
    Karanam Kishore Kumar

    Vikram Sarabhai Space Centre, India

    4 publications · 97 citations

    4

    h-index

1–5 of 460

Venues

  1. Journal of the Atmospheric Sciences

    39 publications · 3.3K citations

    26

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 15 publications · 781 citations

    15

    h-index

  3. Journal of Climate

    12 publications · 982 citations

    12

    h-index

  4. 11

    h-index

  5. Geophysical Research Letters

    10 publications · 313 citations

    10

    h-index

1–5