Linked from

The 67 pages that link to Coriolis effect, each with the reason it gives.

• Léon FoucaultRelated: It helps explain how Earth’s rotation changes a pendulum’s swing direction relative to the ground.

• Physical oceanographyRelated: Earth’s rotation shapes the direction and balance of ocean currents.

• Gaspard-Gustave de CoriolisBroader topic: This phenomenon is the best-known consequence of the mechanics associated with Coriolis.

• Buys Ballot's lawRelated: Earth’s rotation deflects winds and helps set the pressure-relative direction the law describes.

• Atmospheric scienceRelated: Earth’s rotation redirects large-scale winds and ocean-linked atmospheric flows.

• Fujiwhara effectRelated: Earth’s rotation shapes cyclone circulation and the background flow in which interacting storms evolve.

• Geophysical fluid dynamicsRelated: Planetary rotation deflects horizontal currents and helps set their large-scale balance.

• Baer–Babinet lawRelated: It supplies the rotational deflection proposed to bias river erosion toward one bank.

• C. H. D. Buys BallotRelated: Earth’s rotation helps explain why winds circulate around pressure systems rather than flowing straight toward them.

• Extraterrestrial vortexRelated: Planetary rotation shapes the direction and organization of large atmospheric flows.

• High-pressure areaRelated: It gives circulation around a high opposite directions in the two hemispheres.

• Ocean dynamicsNarrower topic: Earth’s rotation redirects currents and shapes their large-scale balance.

• Ocean surface topographyRelated: Earth’s rotation helps set the balance between currents and the sea-surface slope.

• Prevailing windsRelated: It turns large-scale airflow and helps shape prevailing wind belts.

• Theory of tidesRelated: Earth’s rotation deflects tidal currents and helps organize basin-scale waves.

• Wind (meteorology)Related: Earth’s rotation deflects winds to the right in the Northern Hemisphere and left in the Southern.

• Zonal and meridional flowRelated: Earth’s rotation alters the paths and balance of zonal and meridional motion.