Upper-level Trough Dynamics

Upper-Level Trough Dynamics is a theoretical framework within atmospheric dynamics that characterizes the evolution, propagation, and associated baroclinic instability of large-scale cyclonic curvature in the upper-tropospheric flow, distinguishing it by its emphasis on the vertical coupling between potential vorticity anomalies and synoptic-scale wave development.

111

Publications

6.2K

Citations

306

Authors

159

Institutions

Publications per year

2017–2026

20

Authors

306

  1. PK
    Peter Knippertz

    Karlsruhe Institute of Technology, Germany

    6 publications · 358 citations

    6

    h-index

  2. JW
    John W. Nielsen‐Gammon

    Texas A&M University, United States

    3 publications · 173 citations

    3

    h-index

  3. TM
    Takio Murakami

    University of Hawaii System, United States

    2 publications · 57 citations

    2

    h-index

  4. FS
    Frederick Sanders

    Massachusetts Institute of Technology, United States

    2 publications · 84 citations

    2

    h-index

  5. RL
    Russell L. Elsberry

    Naval Postgraduate School, United States

    2 publications · 159 citations

    2

    h-index

1–5 of 306

Venues

  1. Monthly Weather Review

    38 publications · 2.8K citations

    26

    h-index

  2. Journal of the Atmospheric Sciences

    10 publications · 470 citations

    10

    h-index

  3. Journal of Climate

    6 publications · 252 citations

    6

    h-index

  4. 5

    h-index

  5. Geophysical Research Letters

    3 publications · 352 citations

    3

    h-index

1–5