Atmospheric conditions can approach a state of equilibrium locally at elevations above the boundary layer, forming a condition known as

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Geostrophic balance is a state in the atmosphere where the Coriolis force and pressure gradient force are balanced, resulting in a straight flow of wind parallel to the isobars. This state can occur locally at elevations above the boundary layer, where the effect of surface friction is minimal. The other options, such as Coriolis force, latent heat, and wind, are all important factors that affect atmospheric conditions but do not directly lead to geostrophic balance.

Atmospheric Conditions Can Approach a State of Equilibrium Locally at Elevations