Tornadoes often weaken as a result of cold or dry air entering the updraft of their parent storm.
Hurricanes weaken when they move over land.
Tornadoes generally form over land and whether they are on land or over water has little effect on their intensity. It is a hurricane that weakens as it hits land.
Tornadoes typically weaken when they lose their source of warm, moist air that fuels their intensity. This can happen when a tornado moves into a cooler or drier environment, or when the storm system that spawned the tornado weakens. Tornadoes can also weaken as they interact with friction from the earth's surface or from encountering other weather phenomena.
Tornadoes can dissipate when the rotation within the storm weakens or when they move into an area with unfavorable conditions for their formation. They do not vanish completely, but rather lose their strength and structure as they interact with different atmospheric conditions.
Tornadoes typically dissipate when the strong updraft that feeds the storm weakens, causing the spinning motion to slow down and ultimately stop. Without the energy to sustain the circulation, the tornado breaks apart and can no longer produce damage.
It is not known for certain, but it is believed that tornadoes dissipate when cold outflow from a storm undercuts the updraft that powers a tornado and cuts off the supply of warm air that fuels it.
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Hurricanes usually dissipate when they are cut off from the warm ocean water that fuels them through evaporation. This usually happens when the storm moves over land or colder water. Wind shear can also greatly weaken a hurricane. How tornadoes dissipate is not fully understood, but it is believed that outflow from a thunderstorm (either the one that produced the tornado or a separate storm) wraps around the parent circulation (mesocyclone) of the tornado, and essentially choking off the supply of warm air that drives the updraft.
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Tornadoes are often called twisters. Some people call them cyclones, though this is not a correct name as it already applies to something else.
What causes tornadoes to dissipate is not fully understood, but it is believed that cold thunderstorm outflow undercuts the parent circulation (mesocyclone) that drives the tornado, cutting of the warm air that drives the thunderstorm, causing it to weaken to the point that it can no longer sustain a tornado.
When a hurricane makes landfall it weakens rapidly, with the winds at lower levels weakening faster than those at upper levels. This difference in wind speed creates wind shear, which can cause the thunderstorms in the rain bands of a hurricane to start rotating. This rotating can then tighten and intensify to form tornadoes.