Upper-level Troughs
Upper-Level Troughs is a large-scale atmospheric circulation feature characterized by a southward dip in the westerly flow of the upper troposphere, distinguished from other synoptic-scale disturbances by its association with cyclonic vorticity advection and its role in modulating vertical motion and surface cyclogenesis.
140
Publications
7.3K
Citations
315
Authors
153
Institutions
Publications per year
2017–2026
15
Variants
Upper-air Troughs
Parents
140
1–5 of 140
315
8
h-index
5
h-index
University at Albany, State University of New York, United States
4 publications · 222 citations
4
h-index
University at Albany, State University of New York, United States
4 publications · 415 citations
4
h-index
3
h-index
1–5 of 315
153
University at Albany, State University of New York
Albany, United States
8 h-index
20 publications
1.7K citations
Colorado State University
Fort Collins, United States
6 h-index
11 publications
758 citations
Albany State University
Albany, United States
6 h-index
14 publications
1.2K citations
ETH Zurich
Zurich, Switzerland
5 h-index
11 publications
589 citations
Goddard Space Flight Center
Greenbelt, United States
5 h-index
6 publications
741 citations
University of Reading
Reading, United Kingdom
5 h-index
13 publications
451 citations
NOAA National Weather Service
Silver Spring, United States
4 h-index
4 publications
123 citations
Johannes Gutenberg University Mainz
Mainz, Germany
4 h-index
4 publications
260 citations
1–8 of 153
47 publications · 2.6K citations
30
h-index
15 publications · 835 citations
14
h-index
10 publications · 707 citations
10
h-index
9 publications · 538 citations
9
h-index
7 publications · 359 citations
7
h-index
1–5