Hydrostatic Equation
The Hydrostatic Equation is a fundamental differential equation in fluid dynamics that describes the balance between gravitational force and pressure gradient force in a static fluid, specifically defining how pressure decreases with height in an atmosphere or ocean at rest.
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7.6K
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326
Authors
193
Institutions
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2017–2026
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Centre National de la Recherche Scientifique
Paris, France
5 h-index
14 publications
535 citations
Met Office
Exeter, United Kingdom
5 h-index
9 publications
519 citations
University of Management and Technology
Lahore, Pakistan
5 h-index
11 publications
204 citations
University of Lisbon
Lisbon, Portugal
4 h-index
11 publications
218 citations

NSF National Center for Atmospheric Research
Boulder, United States
4 h-index
7 publications
543 citations
University of California, Los Angeles
Los Angeles, United States
4 h-index
8 publications
815 citations
Instituto Tecnológico de Aeronáutica
São José dos Campos, Brazil
3 h-index
10 publications
876 citations
University of Vienna
Vienna, Austria
3 h-index
6 publications
108 citations
1–8 of 193
19 publications · 1.9K citations
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9 publications · 382 citations
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ApJ · 9 publications · 546 citations
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5 publications · 267 citations
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5 publications · 215 citations
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