Inverted Barometer Effect
The Inverted Barometer Effect is a geophysical phenomenon in which sea level exhibits a negative response to atmospheric pressure changes, such that a rise in surface air pressure induces a corresponding decrease in sea level, and vice versa, typically modeled as a static equilibrium adjustment of the ocean surface under the influence of gravitational and atmospheric loading forces.
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4.7K
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160
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92
Institutions
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2017–2026
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Variants
Inverted Barometer Response
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Atmospheric and Environmental Research, United States
5 publications · 210 citations
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Atmospheric and Environmental Research
Lexington, United States
14 h-index
22 publications
1.4K citations
Jet Propulsion Laboratory
Pasadena, United States
6 h-index
12 publications
579 citations

Hong Kong Polytechnic University
Hong Kong, Hong Kong
3 h-index
6 publications
78 citations
California Institute of Technology
Pasadena, United States
3 h-index
6 publications
658 citations
Laboratoire d’Études en Géophysique et Océanographie Spatiales
Toulouse, France
3 h-index
3 publications
167 citations

Centrum Badań Kosmicznych
Warsaw, Poland
3 h-index
4 publications
105 citations

Scripps Institution of Oceanography
La Jolla, United States
2 h-index
2 publications
471 citations
Mediterranean Institute for Advanced Studies
Esporles, Spain
2 h-index
5 publications
426 citations
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JGR · 26 publications · 1.9K citations
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8 publications · 399 citations
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7 publications · 794 citations
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GJI · 4 publications · 277 citations
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3 publications · 164 citations
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