Due to the United States' large size and wide range of geographic features, nearly every type of climate is represented. The climate is temperate in most areas, tropical in Hawaii and southern Florida, arctic in Alaska, semiarid in the Great Plains west of the Mississippi River, desert in the Southwest, mediterranean in coastal California, and arid in the Great Basin. Extreme weather is not uncommon—the states bordering the Gulf of Mexico are prone to hurricanes and most of the world's tornadoes occur within the continental United States. However, the predominantly temperate climate, infrequent severe drought in the major arable regions, and infrequent severe flooding have helped make the nation a world leader in agriculture.
America's weather is affected markedly by the confrontation between polar continental air masses (usually cold, dry, and stable) and tropical maritime air masses (warm, moist, and unstable). Most parts оf America are subject to a generally westerly wind flow that tends to move weather systems eastward.
The interaction of climatic controls creates a pattern of climatic regionalization. In the East, the principal element in climatic variation is temperature; in the West, it is precipitation. In the East, the divisions between the climate regions are based largely on the length of the growing season—the period from the average date of the last frost in spring to the first frost in fall—and on the average summer maximum temperature or winter minimum temperature. In the West, average annual precipitation is the key, although moderated temperatures are an important aspect of the marine West Coast climate. In the East, the more northerly areas are generally drier; in the West, they are colder. In the East, the major influence on climatic variation is latitude; in the West, it is topography.