Frontal Forcing

Frontal Forcing is a synoptic-scale meteorological mechanism characterized by the lifting of warm, moist air ahead of an advancing frontal boundary, where the contrast in air mass properties and associated horizontal wind convergence initiate deep convection through dynamic ascent.

29

Publications

1.1K

Citations

82

Authors

38

Institutions

Publications per year

2017–2026

3

Authors

82

  1. DK
    Daniel Keyser

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

    2 publications · 87 citations

    2

    h-index

  2. JE
    Jonathan E. Martin

    University of Wisconsin–Madison, United States

    2 publications · 75 citations

    2

    h-index

  3. CF
    Clifford F. Mass

    University of Washington, United States

    1 publications · 18 citations

    1

    h-index

  4. KK
    Klaus Keuler

    Brandenburg University of Technology Cottbus-Senftenberg, Germany

    1 publications · 16 citations

    1

    h-index

  5. AK
    Akira Kuwano‐Yoshida

    Japan Agency for Marine-Earth Science and Technology, Japan

    1 publications · 136 citations

    1

    h-index

1–5 of 82

Venues

  1. Monthly Weather Review

    6 publications · 295 citations

    6

    h-index

  2. 4

    h-index

  3. Journal of the Atmospheric Sciences

    3 publications · 118 citations

    3

    h-index

  4. Meteorology and Atmospheric Physics

    2 publications · 51 citations

    2

    h-index

  5. Journal of Climate

    2 publications · 76 citations

    2

    h-index

1–5