Answer:
The Coriolis force deflects this outward flow, creating a broad anticyclonic circulation aloft. Therefore, horizontal circulation in the upper levels of a tropical cyclone is opposite to that near the surface.
Explanation:
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Generally, as the Earth rotates toward the east, this rotation causes fluids, such as air and currents to be deflected to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.
This rotation are what causes Cyclones which are usually common in areas of low pressure.
In conclusion, the natural process is what caused Coriolis force and latent heat to contribute to the development of Ingrid tropical cyclone
Read more about tropical cyclone
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