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
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Formation of Charge Structures in a Supercell
Eric C. Bruning, W. David Rust, Donald R. MacGorman et al. · Monthly Weather Review · 2010 · 90 citations
Tornado-Producing Mini Supercells Associated with Typhoon 9019
Osamu Suzuki, Hiroshi Niino, Hisao Ohno et al. · Monthly Weather Review · 2000 · 66 citations
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NOAA National Severe Storms Laboratory
Norman, United States
4 h-index
7 publications
430 citations
University of Oklahoma
Norman, United States
2 h-index
4 publications
296 citations
University of Illinois Urbana-Champaign
Urbana, United States
2 h-index
2 publications
66 citations

NSF National Center for Atmospheric Research
Boulder, United States
2 h-index
2 publications
28 citations
University of Wyoming
Laramie, United States
2 h-index
3 publications
148 citations
Harvard University
Cambridge, United States
1 h-index
1 publications
45 citations

Cooperative Institute for Mesoscale Meteorological Studies
Norman, United States
1 h-index
2 publications
180 citations
National Centre for Atmospheric Science
Leeds, United Kingdom
1 h-index
1 publications
55 citations
1–8 of 28
5 publications · 235 citations
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4 publications · 193 citations
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2 publications · 75 citations
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2 publications · 88 citations
2
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1 publications · 45 citations
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