About this document
Geostrophic and Drift Currents Explained by Tarik Adella is a document available to read on EtoBox.
The document explains the effects of geostrophic force on surface currents, highlighting how pressure gradients and Coriolis force create geostrophic flow, leading to currents that flow parallel to sea level contours. It also discusses the generation of drift currents by prevailing winds, the influence of temperature and salinity differences on gradient currents, and how these factors combine to form complex current systems along western shores. Additionally, it classifies currents as warm or cold based on
- Author
- Tarik Adella
- Language
- EN