Which effect increases as air parcel velocity increases parallel to isobar lines due to the Coriolis force?

💡 Explanation

When air parcels move with high velocity along isobars, the Coriolis force deflects them until balanced by the pressure gradient force, establishing geostrophic wind balance because the forces reach equilibrium. Therefore, geostrophic wind formation occurs, rather than subsidence, inversion, or enhancement, which each require different atmospheric conditions.

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