Upper-level Troughs

Upper-Level Troughs is a large-scale atmospheric circulation feature characterized by a southward dip in the westerly flow of the upper troposphere, distinguished from other synoptic-scale disturbances by its association with cyclonic vorticity advection and its role in modulating vertical motion and surface cyclogenesis.

140

Publications

7.3K

Citations

315

Authors

153

Institutions

Publications per year

2017–2026

15

Variants

Upper-air Troughs

Authors

315

  1. PK
    Peter Knippertz

    Karlsruhe Institute of Technology, Germany

    8 publications · 460 citations

    8

    h-index

  2. FS
    Frederick Sanders

    Massachusetts Institute of Technology, United States

    5 publications · 174 citations

    5

    h-index

  3. LF
    Lance F. Bosart

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

    4 publications · 222 citations

    4

    h-index

  4. DK
    Daniel Keyser

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

    4 publications · 415 citations

    4

    h-index

  5. TH
    Takeshi Horinouchi

    Hokkaido University, Japan

    3 publications · 101 citations

    3

    h-index

1–5 of 315

Venues

  1. Monthly Weather Review

    47 publications · 2.6K citations

    30

    h-index

  2. Journal of the Atmospheric Sciences

    15 publications · 835 citations

    14

    h-index

  3. Journal of Climate

    10 publications · 707 citations

    10

    h-index

  4. 9

    h-index

  5. International Journal of Climatology

    7 publications · 359 citations

    7

    h-index

1–5