Jet Stream Divergence

Jet Stream Divergence is a meteorological phenomenon characterized by the horizontal spreading of wind velocities within the upper troposphere, distinguished by the differential motion of air masses along the axis of a jet stream, leading to regions of mass evacuation and associated synoptic-scale weather development.

74

Publications

2.7K

Citations

239

Authors

125

Institutions

Publications per year

2017–2026

12

Authors

239

  1. WF
    W. Fundamenski

    Culham Centre for Fusion Energy, United Kingdom

    2 publications · 44 citations

    2

    h-index

  2. GH
    G. Horn

    University of Sheffield, United Kingdom

    2 publications · 48 citations

    2

    h-index

  3. QX
    Qiang Xu

    Xi'an Jiaotong University, China

    2 publications · 48 citations

    2

    h-index

  4. VK
    V. Kolář

    Czech Academy of Sciences, Institute of Hydrology, Czechia

    2 publications · 63 citations

    2

    h-index

  5. AH
    Albert Hertzog

    Laboratoire de Météorologie Dynamique, France

    2 publications · 37 citations

    2

    h-index

1–5 of 239

Venues

  1. Experiments in Fluids

    3 publications · 198 citations

    3

    h-index

  2. Journal of the Atmospheric Sciences

    3 publications · 97 citations

    3

    h-index

  3. 3

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 3 publications · 148 citations

    3

    h-index

  5. Chemical Engineering Science

    2 publications · 73 citations

    2

    h-index

1–5