1) Tropical cyclones originate in the Intertropical Convergence Zone near the equator where trade winds from the northern and southern hemispheres converge.
2) A typhoon is a tropical cyclone that forms over the northwest Pacific ocean, characterized by strong counterclockwise rotating winds around a low-pressure eye.
3) Two key factors fuel the formation and strengthening of a typhoon - rapid updrafts of warm moist air from the ocean surface, and the condensation and release of heat from this water vapor into the swirling winds.