Synoptic-scale Forcing

Synoptic-Scale Forcing is a meteorological phenomenon representing large-scale atmospheric disturbances, typically associated with mid-latitude weather systems, that initiate or modulate lower-level processes such as convection, precipitation, and boundary layer dynamics through horizontal divergence, vorticity advection, and temperature advection at spatial scales of 1,000 to 3,000 kilometers.

420

Publications

25.9K

Citations

1.2K

Authors

409

Institutions

Publications per year

2017–2026

82

Authors

1.2K

  1. LF
    Lance F. Bosart

    University at Albany, State University of New York, United States

    8 publications · 588 citations

    8

    h-index

  2. CB
    Christian Barthlott

    Karlsruhe Institute of Technology, Germany

    7 publications · 298 citations

    7

    h-index

  3. CF
    Clifford F. Mass

    University of Washington, United States

    7 publications · 450 citations

    7

    h-index

  4. CK
    Christian Keil

    Ludwig-Maximilians-Universität München, Germany

    7 publications · 374 citations

    7

    h-index

  5. AR
    Anthony R. Lupo

    University of Missouri, United States

    5 publications · 313 citations

    5

    h-index

1–5 of 1.2K

Venues

  1. Monthly Weather Review

    94 publications · 5.9K citations

    43

    h-index

  2. Journal of the Atmospheric Sciences

    38 publications · 3.3K citations

    30

    h-index

  3. Weather and Forecasting

    30 publications · 2.2K citations

    22

    h-index

  4. Atmospheric chemistry and physics

    18 publications · 975 citations

    15

    h-index

  5. 14

    h-index

1–5