Low-Level Vorticity is a meteorological concept referring to the rotation of air in the lower troposphere, specifically characterized by the vertical component of vorticity within the boundary layer and lower levels of the atmosphere that contributes to the development and dynamics of African Easterly Waves.
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380
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172
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36
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171
Brant Liebmann, Harry H. Hendon, John D. Glick · Journal of the Meteorological Society of Japan Ser II · 1994 · 528 citations · Full text
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- MT
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- HZHaikun Zhao
Nanjing University of Information Science and Technology, China
5 publications · 270 citations
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Nanjing University of Information Science and Technology
Nanjing, China
12 h-index
23 publications
1.4K citations
University of Hawaiʻi at Mānoa
Honolulu, United States
9 h-index
13 publications
631 citations
Colorado State University
Fort Collins, United States
9 h-index
18 publications
2.1K citations
NSF National Center for Atmospheric Research
Boulder, United States
7 h-index
10 publications
962 citations
Pennsylvania State University
State College, United States
7 h-index
11 publications
454 citations
ETH Zurich
Zurich, Switzerland
6 h-index
18 publications
1.2K citations
University of Reading
Reading, United Kingdom
6 h-index
11 publications
421 citations
Naval Postgraduate School
Monterey, United States
5 h-index
11 publications
272 citations
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- Monthly Weather Review
41 publications · 2.6K citations
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- Journal of the Atmospheric Sciences
35 publications · 2.8K citations
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- Journal of Climate
21 publications · 3K citations
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- Tellus A Dynamic Meteorology and Oceanography
8 publications · 483 citations
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- Journal of the Meteorological Society of Japan Ser II
7 publications · 765 citations
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