Mesoscale Vorticity

Mesoscale Vorticity is a meteorological phenomenon denoting the rotation inherent in atmospheric flows at the mesoscale, characterized by horizontal vorticity structures typically ranging from 2 to 2000 kilometers in spatial extent and arising from localized gradients in wind shear, convection, or topographic influences.

210

Publications

10.6K

Citations

503

Authors

226

Institutions

Publications per year

2017–2026

30

Authors

503

  1. MT
    Michael T. Montgomery

    Naval Postgraduate School, United States

    8 publications · 465 citations

    8

    h-index

  2. CA
    Christopher A. Davis

    NSF National Center for Atmospheric Research, United States

    5 publications · 512 citations

    5

    h-index

  3. SF
    Shenming Fu

    Institute of Atmospheric Physics, China

    4 publications · 137 citations

    4

    h-index

  4. PK
    Patrice Klein

    Ifremer, France

    3 publications · 881 citations

    3

    h-index

  5. LL
    Lun Li

    Chinese Academy of Meteorological Sciences, China

    3 publications · 92 citations

    3

    h-index

1–5 of 503

Venues

  1. Monthly Weather Review

    37 publications · 1.6K citations

    26

    h-index

  2. Journal of the Atmospheric Sciences

    20 publications · 1.2K citations

    18

    h-index

  3. 12

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 13 publications · 647 citations

    11

    h-index

  5. Journal of Physical Oceanography

    10 publications · 1.1K citations

    10

    h-index

1–5