The answer is Tornadoes :)
Usually a thunderstorm, but depending on the temperature a tornado can also form.
when the hot air from higher up meets with cooler, lower air and they collide and create thunder & when thunder happens, lightening is created after thunder
A tornado forms
No, a marsh is a type of wetland characterized by freshwater vegetation and conditions. It forms in low-lying areas like river deltas or near ponds and lakes. When a freshwater source meets the ocean, it can create a different type of wetland called an estuary.
The river meets the ocean, causing its speed to decrease, which allows sediments carried by the river to settle out as the water slows down. This process is known as sediment deposition, which forms deltas where the river meets the ocean.
The answer is Tornadoes :)
The answer is Tornadoes :)
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.
An edge. A horizontal edge, to be more precise.
The Nile forms a delta where it meets the Mediterranean.
delta
delta
A tornado forms when warm, moist air meets cold, dry air, creating unstable atmospheric conditions. This can lead to the formation of a rotating column of air, which extends from a thunderstorm cloud to the ground. The spinning motion causes the tornado to touch down and move across the landscape with destructive force.
Horizontal is from side to side... Right to left or left to right. Remember is by thinking of the horizon at the beach. It is where the sky meets the water. It always appears side to side.
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.