Jet Stream Formation

Jet Stream Formation is a meteorological phenomenon characterized by the development of narrow, high-altitude bands of intense westerly winds in the upper troposphere, driven primarily by strong horizontal temperature gradients and the Earth's rotation, distinguishing it from other atmospheric circulation patterns through its speed, altitude, and persistent directional coherence.

93

Publications

4.9K

Citations

322

Authors

165

Institutions

Publications per year

2017–2026

20

Authors

322

  1. NA
    Norman A. Phillips

    Massachusetts Institute of Technology, United States

    3 publications · 35 citations

    3

    h-index

  2. YZ
    Yaocun Zhang

    Nanjing University, China

    3 publications · 81 citations

    3

    h-index

  3. KA
    K. A. Browning

    University of Reading, United Kingdom

    3 publications · 269 citations

    3

    h-index

  4. CW
    Chester W. Newton

    University of Chicago, United States

    3 publications · 39 citations

    3

    h-index

  5. LG
    Luís Gimeno

    Universidade de Vigo, Spain

    2 publications · 150 citations

    2

    h-index

1–5 of 322

Venues

  1. 9

    h-index

  2. Journal of Climate

    5 publications · 170 citations

    5

    h-index

  3. Geophysical Research Letters

    4 publications · 149 citations

    4

    h-index

  4. Tellus A Dynamic Meteorology and Oceanography

    3 publications · 35 citations

    3

    h-index

  5. International Journal of Climatology

    3 publications · 128 citations

    3

    h-index

1–5