Intertropical Convergence Zone is dependent upon low-level vorticity united of its 6-8 requirements, and the ITCZ fills this role as this is a zone of blowing wind change and rate, otherwise known seeing that horizontal wind shear. For the reason that ITCZ migrates in excess of 500 kilometres (300 mi) on the equator during respective hemisphere’s summer season, increasing Coriolis power makes the creation of tropical cyclones through this zone more possible.
Intertropical Convergence Zone
