Synoptic-scale Circulation

Synoptic-Scale Circulation is a large-scale atmospheric circulation system characterized by horizontal dimensions of several hundred to several thousand kilometers and time scales of a few days to over a week, primarily responsible for the development and movement of weather systems such as highs, lows, and frontal zones within the midlatitudes.

518

Publications

26.3K

Citations

1.3K

Authors

493

Institutions

Publications per year

2017–2026

80

Authors

1.3K

  1. RH
    Radan Huth

    Czech Academy of Sciences, Institute of Atmospheric Physics, Czechia

    7 publications · 1K citations

    7

    h-index

  2. AJ
    Andrew J. Majda

    Courant Institute of Mathematical Sciences, United States

    6 publications · 428 citations

    6

    h-index

  3. PK
    Pavlos Kassomenos

    University of Ioannina, Greece

    6 publications · 201 citations

    6

    h-index

  4. AM
    Andrew M. Carleton

    Pennsylvania State University, United States

    5 publications · 214 citations

    5

    h-index

  5. UD
    Uri Dayan

    Hebrew University of Jerusalem, Israel

    5 publications · 324 citations

    5

    h-index

1–5 of 1.3K

Venues

  1. Monthly Weather Review

    66 publications · 3.5K citations

    33

    h-index

  2. International Journal of Climatology

    50 publications · 2.6K citations

    29

    h-index

  3. Climate Dynamics

    29 publications · 1.5K citations

    22

    h-index

  4. Journal of the Atmospheric Sciences

    31 publications · 2.2K citations

    22

    h-index

  5. Journal of Climate

    21 publications · 1K citations

    20

    h-index

1–5