冰雹，台风，飓风分别是怎样形成，我需要英文解释

【专家解说】：冰雹 hail Precipitation in the form of spherical or irregular pellets of ice larger than 5 millimeters (0.2 inches) in diameter. 台风typhoon A tropical cyclone occurring in the western Pacific or Indian oceans. The history of typhoon presents a perfect example of the long journey that many words made in coming to English. It traveled from Greece to Arabia to India, and also arose independently in China, before assuming its current form in our language. The Greek word tuphōn, used both as the name of the father of the winds and a common noun meaning “whirlwind, typhoon,” was borrowed into Arabic during the Middle Ages, when Arabic learning both preserved and expanded the classical heritage and passed it on to Europe and other parts of the world. Ṭūfān, the Arabic version of the Greek word, passed into languages spoken in India, where Arabic-speaking Muslim invaders had settled in the 11th century. Thus the descendant of the Arabic word, passing into English (first recorded in 1588) through an Indian language and appearing in English in forms such as touffon and tufan, originally referred specifically to a severe storm in India. The modern form of typhoon was influenced by a borrowing from the Cantonese variety of Chinese, namely the word taaîfung, and respelled to make it look more like Greek. Taaîfung, meaning literally “great wind,” was coincidentally similar to the Arabic borrowing and is first recorded in English guise as tuffoon in 1699. The various forms coalesced and finally became typhoon, a spelling that first appeared in 1819 in Shelley's Prometheus Unbound. 飓风hurricane, tropical cyclone in which winds attain speeds greater than 74 mi (119 km) per hr. Wind speeds reach over 190 mi (289 km) per hr in some hurricanes. The term is often restricted to those storms occurring over the N Atlantic Ocean; the identical phenomenon occurring over the W Pacific Ocean is called a typhoon; around Australia and over the Indian Ocean, a tropical cyclone. Hurricanes have a life span of 1 to 30 days. They weaken and are transformed into extratropical cyclones after prolonged contact with the colder ocean waters of the middle latitudes, and they rapidly decay after moving over land areas.