Cross-equatorial Flow
Cross-Equatorial Flow is a large-scale atmospheric circulation pattern characterized by the meridional movement of air masses across the equator, primarily driven by hemispheric pressure gradients and monsoon-related thermal asymmetries, that plays a critical role in the interhemispheric transport of momentum, moisture, and energy within the tropical climate system.
220
Publications
13.4K
Citations
569
Authors
252
Institutions
Publications per year
2017–2026
39
220
An Estimate of Equatorial Upwelling in the Pacific
Klaus Wyrtki · Journal of Physical Oceanography · 1981 · 415 citations
1–5 of 220
569
8
h-index
7
h-index
5
h-index
5
h-index
European Centre for Medium-Range Weather Forecasts, United Kingdom
4 publications · 192 citations
4
h-index
1–5 of 569
252
University of Washington
Seattle, United States
13 h-index
21 publications
3K citations

University of Hawaiʻi at Mānoa
Honolulu, United States
13 h-index
31 publications
4.3K citations

University of Hawaii System
Honolulu, United States
9 h-index
20 publications
1.6K citations

Chinese Academy of Sciences
Beijing, China
8 h-index
11 publications
754 citations
The University of Tokyo
Tokyo, Japan
8 h-index
13 publications
425 citations
Institute of Atmospheric Physics
Beijing, China
7 h-index
12 publications
769 citations
Massachusetts Institute of Technology
Cambridge, United States
7 h-index
9 publications
604 citations
Florida State University
Tallahassee, United States
7 h-index
10 publications
356 citations
1–8 of 252
34 publications · 3.9K citations
25
h-index
34 publications · 2.3K citations
25
h-index
15 publications · 921 citations
13
h-index
14 publications · 725 citations
12
h-index
JGR · 11 publications · 667 citations
11
h-index
1–5