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geostrophic wind is blowing parallel to the straight isobar balancing between pressure gradient force and coriolis force.when a third force i.e. force of friction act near to the earth surface the three forces balance each other,now this time the wind blow in a curved path and in this case geostrophic wind parallel to the curve isobar . hence geostrophic becomes ageostrophic.

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Q: How geostrophic wind becomes ageostrophic under the influence of friction?
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