![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/53dea4e3-0754-4fd8-9dc0-706138af9906/jgrc8836-math-0094.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
![10.9 See how the gradient wind has a role in weather. | METEO 300: Fundamentals of Atmospheric Science 10.9 See how the gradient wind has a role in weather. | METEO 300: Fundamentals of Atmospheric Science](https://www.e-education.psu.edu/meteo300/sites/www.e-education.psu.edu.meteo300/files/images/lesson10/1015.png)
10.9 See how the gradient wind has a role in weather. | 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
![SOLVED: Calculate the geostrophic wind speed for a pressure gradient of 0.05 mb/km, assuming that the Coriolis parameter fc 10-4 s-1 A - B E SOLVED: Calculate the geostrophic wind speed for a pressure gradient of 0.05 mb/km, assuming that the Coriolis parameter fc 10-4 s-1 A - B E](https://cdn.numerade.com/ask_previews/427b1c92-bdc9-4249-8ab5-0d20ff569cc9_large.jpg)