In frontogenesis, temperature gradients need to tighten for initiation.
2.
As the temperature gradient steepens during frontogenesis, the thermal wind becomes imbalanced.
3.
Within a mid-latitude cyclone, these two key features play an essential role in frontogenesis.
4.
During frontogenesis, the temperature gradient tightens and as a result, the thermal wind becomes imbalanced.
5.
In contrary to areas of " Frontogenesis ", the areas where air masses diverge are called areas of frontolysis.
6.
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.
7.
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
8.
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.
9.
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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