| 1. | In the free atmosphere, geostrophic wind relationships should be used.
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| 2. | In other words, no vertical wind shear of the geostrophic wind.
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| 3. | Unlike geostrophic currents, and geostrophic winds are examples of inertial waves.
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| 4. | They follow the principle of geostrophic winds.
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| 5. | Isallobaric gradients are important components of the wind as they increase or decrease the geostrophic wind.
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| 6. | The geostrophic wind component is the result of the balance between Coriolis force and pressure gradient force.
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| 7. | Look at geostrophic wind article in wikipedia and you will be able to solve this problem without difficulty.
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| 8. | The gradient wind is similar to the geostrophic wind but also includes centrifugal force ( or centripetal acceleration ).
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| 9. | To maintain balance, the geostrophic wind aloft and below adjust, such that regions of divergence / convergence form.
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| 10. | Such isobaric surfaces will also be isothermal surfaces, hence ( from the thermal wind equation ) the geostrophic wind will not vary with depth.
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