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2.2 The Atmosphere's Pressure Structure: Hydrostatic Equilibrium | METEO 300: Fundamentals of Atmospheric Science
![A method for computing horizontal pressure‐gradient force in an oceanic model with a nonaligned vertical coordinate - Shchepetkin - 2003 - Journal of Geophysical Research: Oceans - Wiley Online Library A method for computing horizontal pressure‐gradient force in an oceanic model with a nonaligned vertical coordinate - Shchepetkin - 2003 - Journal of Geophysical Research: Oceans - Wiley Online Library](https://agupubs.onlinelibrary.wiley.com/cms/asset/f3541728-eecc-4c15-bc80-edbe09f79d1d/jgrc8836-math-0008.gif)
A method for computing horizontal pressure‐gradient force in an oceanic model with a nonaligned vertical coordinate - Shchepetkin - 2003 - Journal of Geophysical Research: Oceans - Wiley Online Library
![A method for computing horizontal pressure‐gradient force in an oceanic model with a nonaligned vertical coordinate - Shchepetkin - 2003 - Journal of Geophysical Research: Oceans - Wiley Online Library A method for computing horizontal pressure‐gradient force in an oceanic model with a nonaligned vertical coordinate - Shchepetkin - 2003 - Journal of Geophysical Research: Oceans - Wiley Online Library](https://agupubs.onlinelibrary.wiley.com/cms/asset/09ed4124-ac13-440b-b2de-f9f20c0972bf/jgrc8836-math-0096.gif)