Equatorial Wave Instability
Equatorial Wave Instability is a dynamical phenomenon in atmospheric and oceanic sciences wherein equatorial waves, governed by the equatorial beta-plane approximation, exhibit exponential growth in amplitude due to instabilities arising from interactions between wave modes and background flow shear, stratification, or coupling with convection, distinguishing it from neutral or damped equatorial wave behavior.
31
Publications
1.3K
Citations
67
Authors
47
Institutions
Publications per year
2017–2026
2
Parents
31
1–5 of 31
67
NOAA Geophysical Fluid Dynamics Laboratory, United States
3 publications · 202 citations
3
h-index
3
h-index
2
h-index
2
h-index
2
h-index
1–5 of 67
47

University College Cork
Cork, Ireland
3 h-index
4 publications
200 citations
Earth Science Institute of the Slovak Academy of Sciences
Bratislava, Slovakia
3 h-index
3 publications
202 citations
Courant Institute of Mathematical Sciences
New York, United States
2 h-index
3 publications
159 citations
Goddard Space Flight Center
Greenbelt, United States
2 h-index
10 publications
316 citations
National Cheng Kung University
Tainan City, Taiwan
2 h-index
3 publications
141 citations

Cornell University
Ithaca, United States
2 h-index
9 publications
298 citations
New York University
New York, United States
2 h-index
3 publications
159 citations
University of Vienna
Vienna, Austria
2 h-index
3 publications
245 citations
1–8 of 47
5 publications · 150 citations
5
h-index
JGR · 4 publications · 163 citations
4
h-index
4 publications · 215 citations
4
h-index
3 publications · 97 citations
3
h-index
2 publications · 75 citations
2
h-index
1–5