How Coriolis force and vertical wind shear affect the formation and development of tropical cyclone?

Question

And how coriolis force and the vertical wind shear affect the formation and development of tornadoes?

Answer 1

Good question. If the vertical wind shear is too great over a developing tropical cyclone, the heat energy released in the condensation of water vapor which helps energize the storm will be carried away. And if the storm were to develop too close to the equator (south of about 10 N) the Coriolis force would be too weak and therefore there could be no circulation formed. Low pressure formed by heating would immediately be filled with wind rushing down the pressure gradient unable to be turned into a circulation.

Answer 2

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