| 1. | As the temperature gradient steepens during frontogenesis, the thermal wind becomes imbalanced.
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| 2. | The thermal wind equation does not determine the wind in the tropics.
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| 3. | Shallow, warm water and constant thermal wind make learning here a pure joy.
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| 4. | Q-vectors and all ageostrophic flow exist to preserve thermal wind balance.
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| 5. | Jet streams ( shown in pink ) are well-known examples of thermal wind.
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| 6. | All these facts are consequences of the thermal wind relation.
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| 7. | During frontogenesis, the temperature gradient tightens and as a result, the thermal wind becomes imbalanced.
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| 8. | Also called "'baroclinic flow "', the thermal wind varies with height in proportion to the horizontal temperature gradient.
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| 9. | Mathematically, the thermal wind relation defines a vertical wind shear-- a variation in wind speed or direction with height.
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| 10. | From February May Hua Hin has a southerly thermal wind that gusts to 15 20 knots in the afternoon.
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मोबाइल