The passage of a tropical cyclone about the ocean will cause the upper layers on the ocean to chill substantially, a method known as upweling,[62] which could negatively impact subsequent cyclone progress. This cooling is mostly brought on by wind-pushed mixing of cold water from deeper during the ocean with https://conner95k9r.idblogz.com/30419269/5-tips-about-cyclone-you-can-use-today