Tornadoes form better in warm areas. The reason for this is warm air holds more energy to power storms than cold air does.
Tornadoes can form over just about any sort of terrain but tend to be more common in flat or gently rolling areas. Hurricanes can only form over warm ocean water.
Hurricanes cannot form on land; they can only form over warm ocean water. Tornadoes can form almost anywhere, but are most common in areas with a warm temperate to subtropical climate. The most tornado-prone area in the world is Tornado Alley, which covers much of the Great Plains in the central U.S.
Antarctica is very cold while tornadoes can only form with thunderstorms, which require at least some degree of warm, moist air.
Antarctica is too cold for tornadoes to form. Tornadoes need energy from warm air.
No. Tornadoes usually form on land, not water. Tornadoes on water are called waterspouts. Tornadoes are spawned by thunderstorms, which are fueled by warm, moist, unstable air. A cold body of water tends to stabilize the atmosphere, making thunderstorms and tornadoes less likely. A warm body of water has the opposite effect.
Hurricanes form over warm ocean water. Tornadoes can form just about anywhere.
No, tornadoes typically form in warm and moist environments in the presence of a strong vertical wind shear and unstable atmosphere. Cold and windy conditions with no clouds are not conducive to tornado formation.
Tornadoes are more common in areas with warmer climates than those with cold ones.
Hurricanes can only develop over warm ocean water. Tornadoes can form on water but usually form on land.
Tornadoes are more likely to form along a cold front, but they can occasionally form along a warm front. Many tornadoes form in an area called Larko's triangle, between a warm front and cold front. Some tornadoes form along a dry line, and in fact a try line can be more proficient at producing tornadoes than a cold front. Still other tornadoes form from tropical systems, which do not involve any sort of front.
Tornadoes can occur in the warm sector of a developing mid-latitude cyclone, typically associated with the cold front. Tornadoes often form along the leading edge of the cold front where warm, moist air is lifted rapidly by the advancing cold air.