Synoptic-scale Disturbances

Synoptic-Scale Disturbances is a meteorological phenomenon characterized as a transient, organized atmospheric system spanning approximately 1,000 to 3,000 kilometers that emerges from instabilities in the large-scale flow and propagates within the mid- to lower troposphere, primarily influencing day-to-day weather patterns in the context of baroclinic dynamics and African easterly wave activity.

629

Publications

37K

Citations

1.6K

Authors

519

Institutions

Publications per year

2017–2026

104

Authors

1.6K

  1. TL
    Tim Li

    University of Hawaiʻi at Mānoa, United States

    12 publications · 889 citations

    12

    h-index

  2. LF
    Lance F. Bosart

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

    13 publications · 609 citations

    11

    h-index

  3. JR
    John R. Gyakum

    McGill University, Canada

    8 publications · 251 citations

    8

    h-index

  4. AR
    Anthony R. Lupo

    University of Missouri, United States

    7 publications · 290 citations

    7

    h-index

  5. NL
    Ngar‐Cheung Lau

    NOAA Geophysical Fluid Dynamics Laboratory, United States

    7 publications · 1.6K citations

    7

    h-index

1–5 of 1.6K

Venues

  1. Monthly Weather Review

    136 publications · 8.5K citations

    50

    h-index

  2. Journal of the Atmospheric Sciences

    71 publications · 6.4K citations

    37

    h-index

  3. Journal of Climate

    46 publications · 2.6K citations

    32

    h-index

  4. Weather and Forecasting

    34 publications · 1.7K citations

    24

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 22 publications · 1.6K citations

    19

    h-index

1–5