Synoptic-scale Variability

Synoptic-Scale Variability is a meteorological phenomenon characterized by temporal and spatial fluctuations in atmospheric conditions, such as pressure, temperature, and wind, occurring over horizontal scales of approximately 100 to 2,000 kilometers and temporal scales of one to several days, primarily associated with the development and movement of synoptic weather systems.

572

Publications

35.5K

Citations

1.7K

Authors

587

Institutions

Publications per year

2017–2026

120

Authors

1.7K

  1. LF
    Lance F. Bosart

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

    11 publications · 883 citations

    11

    h-index

  2. TL
    Tim Li

    University of Hawaiʻi at Mānoa, United States

    7 publications · 547 citations

    7

    h-index

  3. CA
    Charles A. Doswell

    NOAA National Severe Storms Laboratory, United States

    7 publications · 701 citations

    7

    h-index

  4. DM
    David M. Schultz

    University of Manchester, United Kingdom

    6 publications · 320 citations

    7

    h-index

  5. JR
    John R. Gyakum

    McGill University, Canada

    6 publications · 186 citations

    7

    h-index

1–5 of 1.7K

Venues

  1. Monthly Weather Review

    112 publications · 8.1K citations

    49

    h-index

  2. Journal of Climate

    64 publications · 5.2K citations

    40

    h-index

  3. Journal of the Atmospheric Sciences

    37 publications · 3.1K citations

    27

    h-index

  4. Weather and Forecasting

    37 publications · 2.5K citations

    25

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 23 publications · 2.2K citations

    19

    h-index

1–5