Bounded Weak Echo Regions

Bounded Weak Echo Region is a radar-observed meteorological phenomenon characterized by a localized volume of weak radar reflectivity surrounded by stronger echoes in the lower to middle levels of a thunderstorm, indicative of a strong updraft that inhibits precipitation formation within the region.

18

Publications

766

Citations

54

Authors

28

Institutions

Publications per year

2017–2026

2

Variants

Bounded Weak Echo RegionBwer

Authors

54

  1. SP
    Stephan P. Nelson

    NOAA National Severe Storms Laboratory, United States

    2 publications · 75 citations

    2

    h-index

  2. JD
    John D. Marwitz

    University of Wyoming, United States

    2 publications · 108 citations

    2

    h-index

  3. VL
    Valliappa Lakshmanan

    University of Oklahoma, United States

    1 publications · 26 citations

    1

    h-index

  4. TW
    Terrence W. Krauss

    University of Wyoming, United States

    1 publications · 40 citations

    1

    h-index

  5. PT
    Paul T. Schlatter

    NOAA Earth System Research Laboratory, United States

    1 publications · 13 citations

    1

    h-index

1–5 of 54

Venues

  1. Monthly Weather Review

    5 publications · 235 citations

    5

    h-index

  2. Journal of the Atmospheric Sciences

    4 publications · 193 citations

    4

    h-index

  3. Weather and Forecasting

    2 publications · 75 citations

    2

    h-index

  4. Journal of Applied Meteorology

    2 publications · 88 citations

    2

    h-index

  5. Proceedings of the IRE

    1 publications · 45 citations

    1

    h-index

1–5