Wave Height Increase
Wave Height Increase is a physical phenomenon in coastal oceanography defined as the process by which the amplitude of a propagating surface gravity wave grows as it moves into shallower water due to the conservation of wave energy flux under decreasing water depth.
138
Publications
6K
Citations
371
Authors
209
Institutions
Publications per year
2017–2026
42
Parents
138
1–5 of 138
371
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Bureau de Recherches Géologiques et Minières, France
3 publications · 211 citations
3
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1–5 of 371
209
National Institute of Oceanography
Panjim, India
5 h-index
11 publications
323 citations
University of Lisbon
Lisbon, Portugal
4 h-index
9 publications
239 citations

Hohai University
Nanjing, China
4 h-index
6 publications
100 citations

The University of Queensland
Brisbane, Australia
4 h-index
10 publications
678 citations

Australian Defence Force Academy
Canberra, Australia
4 h-index
8 publications
361 citations

Council of Scientific and Industrial Research
New Delhi, India
4 h-index
10 publications
306 citations

National Oceanography Centre
Southampton, United Kingdom
4 h-index
8 publications
611 citations
Institute of Oceanology. PP Shirshov Russian Academy of Sciences
Moscow, Russia
4 h-index
8 publications
611 citations
1–8 of 209
JCR · 8 publications · 290 citations
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8 publications · 288 citations
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5 publications · 280 citations
5
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4 publications · 302 citations
4
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4 publications · 94 citations
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