The answer is Tornadoes :)
A small storm that forms when a thunderstorm meets high-altitude horizontal winds is called a microburst. It is a localized column of sinking air within a thunderstorm, which can produce strong winds at the surface.
The answer is Tornadoes :)
There are aspects of both that are not fully understood. For formation: First, a condition called wind shear, in which the speed or direction of the wind changes with altitude. If the shear is strong enough it can essentially tilt a thunderstorm, this separates the updraft and downdraft of the thunderstorm, preventing them from interfering with one another. This allows the storm to become stronger and last longer. Additionally, if the wind shear is strong enough it can start the air rolling in what is called horizontal vorticity. This horizontal vorticity can then be turned vertical by a thunderstorm's updraft. When this happens, the thunderstorm may start rotating. The rotation is especially strong in an updraft called a mesocyclone. If the storm intensifies rapidly enough, a relatively warm downdraft called a rear-flank downdraft or RFD can wrap around the bottom part of the mesocyclone. This can then tighten and intensify its rotation and bring it down to the ground to produce a tornado. For how tornadoes end, it is thought that cold air coming out of a thunderstorm (called outflow) undercuts the mesocyclone, the rotating updraft that drives the tornado. This chokes off the supply of warm air that the updraft feeds the updraft.
The formation of tornadoes is complicated.First, a condition called wind shear, in which the speed or direction of the wind changes with altitude. If the shear is strong enough it can essentially tilt a thunderstorm, this separates the updraft and downdraft of the thunderstorm, preventing them from interfering with one another. This allows the storm to become stronger and last longer.Additionally, if the wind shear is strong enough it can start the air rolling in what is called horizontal vorticity. This horizontal vorticity can then be turned vertical by a thunderstorm's updraft. When this happens, the thunderstorm may start rotating. The rotation is especially strong in an updraft called a mesocyclone. If the storm intensifies rapidly enough, a relatively warm downdraft called a rear-flank downdraft or RFD can wrap around the bottom part of the mesocyclone. This can then tighten and intensify its rotation and bring it down to the ground to produce a tornado.
delta
the fourth station of the cross is the point given when Jesus carring the patibule of the cross ( wich is the horizontal part that forms the cross shape) meets his sorrowfull mother face to face.
A twister, or tornado, forms when warm, moist air near the ground meets cooler, drier air above it. This creates instability in the atmosphere, leading to a rotating column of air that descends from a thunderstorm cloud. When this rotating column touches the ground, it becomes a tornado.
At zero degrees altitude, you would be at ground level or sea level. This position marks the horizon line where the sky meets the Earth.
An edge. A horizontal edge, to be more precise.
The Nile forms a delta where it meets the Mediterranean.
A severe thunderstorm known as a supercell forms It begins in an area where cold dry polar air meets warm moist tropical air and the atmosphere is unstable The wind coming into this storm? Write your answer...
delta