In frontogenesis, temperature gradients need to tighten for initiation.
2.
As the temperature gradient steepens during frontogenesis, the thermal wind becomes imbalanced.
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Within a mid-latitude cyclone, these two key features play an essential role in frontogenesis.
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During frontogenesis, the temperature gradient tightens and as a result, the thermal wind becomes imbalanced.
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In contrary to areas of " Frontogenesis ", the areas where air masses diverge are called areas of frontolysis.
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The quasi-geostrophic equations fail in the dynamics of frontogenesis because this weather phenomenon is of smaller scale compared to the Rossby radius; so semigeostrophic theory is used.
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The final terms are the tilting term and the vertical divergence term; the tilting term is represented in the three-dimensional frontogenesis equation in the x and y directions
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The uneven solar heating ( the formation of zones of temperature and moisture gradients, or frontogenesis ) can also be due to the weather itself in the form of cloudiness and precipitation.
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Rao earned a Ph . D . at the University of Chicago in 1965, studying frontogenesis and continued researching frontogenesis, frontal circulations in the boundary layer, vertical circulations associated with oceanic fronts, and structural features of lake-induced winter disturbances in post-doctoral studies.
10.
Rao earned a Ph . D . at the University of Chicago in 1965, studying frontogenesis and continued researching frontogenesis, frontal circulations in the boundary layer, vertical circulations associated with oceanic fronts, and structural features of lake-induced winter disturbances in post-doctoral studies.
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