Upper-level Jet Streams

Upper-Level Jet Streams is a type of atmospheric circulation characterized as a narrow, high-altitude band of strong, predominantly zonal winds occurring in the upper troposphere or lower stratosphere, distinguished by its association with large vertical and horizontal wind shear and its role in shaping synoptic-scale weather patterns.

84

Publications

4.2K

Citations

209

Authors

101

Institutions

Publications per year

2017–2026

25

Authors

209

  1. HW
    Heini Wernli

    ETH Zurich, Switzerland

    5 publications · 390 citations

    5

    h-index

  2. DK
    Daniel Keyser

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

    4 publications · 152 citations

    4

    h-index

  3. LF
    Lance F. Bosart

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

    4 publications · 147 citations

    4

    h-index

  4. MR
    Mark R. Sinclair

    National Institute of Water and Atmospheric Research, New Zealand

    3 publications · 113 citations

    3

    h-index

  5. MA
    M. A. Shapiro

    National Oceanic and Atmospheric Administration, United States

    3 publications · 259 citations

    3

    h-index

1–5 of 209

Venues

  1. Monthly Weather Review

    21 publications · 1.1K citations

    17

    h-index

  2. Journal of Climate

    11 publications · 1.2K citations

    11

    h-index

  3. Journal of the Atmospheric Sciences

    10 publications · 365 citations

    10

    h-index

  4. 4

    h-index

  5. Weather and Climate Dynamics

    4 publications · 130 citations

    4

    h-index

1–5