Low-level Jet Dynamics

Low-Level Jet Dynamics is a meteorological phenomenon characterized by a localized maximum in the vertical profile of horizontal wind speed within the atmospheric boundary layer, distinguished from other boundary-layer flows by its strong vertical wind shear, diurnal variability, and association with stable nocturnal conditions over land or coastal regions.

579

Publications

38.3K

Citations

1.5K

Authors

486

Institutions

Publications per year

2017–2026

144

Authors

1.5K

  1. RM
    Robert M. Banta

    Cooperative Institute for Research in Environmental Sciences, United States

    10 publications · 1.4K citations

    10

    h-index

  2. TR
    Thomas R. Parish

    University of Wyoming, United States

    9 publications · 581 citations

    9

    h-index

  3. MY
    Monique Y. Leclerc

    University of Georgia, United States

    9 publications · 269 citations

    9

    h-index

  4. AS
    Alan Shapiro

    University of Oklahoma, United States

    8 publications · 491 citations

    8

    h-index

  5. YD
    Yu Du

    Sun Yat-sen University, China

    7 publications · 767 citations

    7

    h-index

1–5 of 1.5K

Venues

  1. Monthly Weather Review

    132 publications · 10.8K citations

    56

    h-index

  2. Journal of the Atmospheric Sciences

    67 publications · 5.2K citations

    38

    h-index

  3. Journal of Climate

    39 publications · 3.9K citations

    30

    h-index

  4. Weather and Forecasting

    25 publications · 1.9K citations

    21

    h-index

  5. Boundary-Layer Meteorology

    23 publications · 1.6K citations

    20

    h-index

1–5