Weakening or dissipation may arise if a storm encounters vertical wind shear which leads to the convection and heat engine to move from the middle; this Ordinarily ceases the development of a tropical cyclone.[ninety two] In addition, its interaction with the leading belt of the Westerlies, via merging with a https://rylanm273f.blogzet.com/the-basic-principles-of-cyclone-44734691