Tropical Inversion Layers

Tropical Inversion Layers is a persistent atmospheric boundary layer phenomenon characterized by a stable temperature increase with altitude in the tropical lower troposphere, distinguishing it from diurnally driven or mid-latitude inversion processes.

28

Publications

1.3K

Citations

117

Authors

68

Institutions

Publications per year

2017–2026

2

Authors

117

  1. SS
    Seok‐Woo Son

    Seoul National University, South Korea

    2 publications · 305 citations

    2

    h-index

  2. MF
    Masatomo Fujiwara

    Hokkaido University, Japan

    2 publications · 289 citations

    2

    h-index

  3. TS
    T. Schmidt

    GFZ Helmholtz Centre for Geosciences, Germany

    2 publications · 75 citations

    2

    h-index

  4. MS
    Masato Shiotani

    Kyoto University, Japan

    2 publications · 45 citations

    2

    h-index

  5. PE
    Paul E. Ciesielski

    Colorado State University, United States

    2 publications · 225 citations

    2

    h-index

1–5 of 117

Venues

  1. Journal of the Atmospheric Sciences

    5 publications · 366 citations

    5

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 5 publications · 389 citations

    5

    h-index

  3. Geophysical Research Letters

    4 publications · 215 citations

    4

    h-index

  4. Journal of Atmospheric and Solar-Terrestrial Physics

    JASTP · 2 publications · 41 citations

    2

    h-index

  5. 2

    h-index

1–5