In some cases one tornado will dissipate completely, and then a completely new tornado will form afterward from the same thunderstorm. This is called a tornado family.
It depends. If the tornado itself is lifting and touching down it is said to be skipping. If multiple funnels appear and disappear while revolving around a center, it is probably a multiple-vortex tornado. In some cases the funnel will dissappear and reappear even though the tornado remains on the ground. This may be due to fluctuations in humidity, though there is no real term for the funnel being inconsistent like this. In some cases one tornado will dissipate completely, and then a completely new tornado will form afterward from the same thunderstorm. This is called a tornado family.
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There are a few possible explanations. Tornadoes are often made visible by the condensation of moisture inside the vortex. If a parcel of dry air enters the tornado, or if the tornado weakens, the visible funnel may evaporate. In this case the tornado is still present and still dangerous, but it has essentially become invisible. A variation of this phenomenon can happen in multiple vortex tornadoes. Tornadoes like this contain multiple smaller, short-lived vortices within a larger tornado. If the amount of moisture in the air is just right, the smaller vortices will be visible as they form and dissipate, but not the larger vortex will remain invisible. In other cases the processes that cause a tornado to dissipate may start, but not finish, causing a tornado to temporarily lift. In other cases a thunderstorm may go through cycles of strengthening and weakening. In the process it can produce multiple tornadoes one after another.
Tornadoes are started when wind shear starts air masses rolling in what is called horizontal vorticity. This rolling air movement can be turned vertical by the updraft of a thunderstorm, which then takes on the rotation to become a mesocyclone. Under the right conditions a downdraft can descend from the back of the storm and wrap around the mesocyclone. This can tighten and intensify the rotation and br9ing it down to the ground to produce a tornado.
The process of tornado formation starts when rolling air called wind shear gets taken into the updraft of a thunderstorm. This turns the storm into a supercell, a storm with a strong, rotating updraft called a mesocyclone. Under the right conditions a downdraft can descend from the back of the storm, wrap around the mesocyclone, and force it into a tighter more intense vortex: the tornado itself.
They're called storm spotters or storm chasers. They drive close to tornadoes and follow them collecting data or reporting info back to the local National Weather Service office.
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It is the prophase. It comes back in telophase
he disappears and never comes back
Tornadoes are not named by individuals. Instead, they are typically referred to by the location or time in which they occur. For example, a tornado in the town of Moore, Oklahoma, might be called the Moore tornado.
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Tornadoes usually form from a type of thunderstorm called a supercell, which has a rotating updraft called a mesocyclone. A downdraft at the back of the storm, called the rear-flank downdraft or RFD is believed to wrap around the tornado, tightening and intensifying it to produce a tornado.
It is growing. Since a new moon is when the moon "disappears", it "comes back" to the full moon.
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The same thing that happens when you're on eartlh and you see a solar eclipse. The sun disappears for a few minutes or seconds and comes back. On earth, it would be called a lunar eclipse, where the earth comes between the sun and the moon. On the moon, it would look like a solar eclipse.
There are a few possible explanations. Tornadoes are often made visible by the condensation of moisture inside the vortex. If a parcel of dry air enters the tornado, or if the tornado weakens, the visible funnel may evaporate. In this case the tornado is still present and still dangerous, but it has essentially become invisible. A variation of this phenomenon can happen in multiple vortex tornadoes. Tornadoes like this contain multiple smaller, short-lived vortices within a larger tornado. If the amount of moisture in the air is just right, the smaller vortices will be visible as they form and dissipate, but not the larger vortex will remain invisible. In other cases the processes that cause a tornado to dissipate may start, but not finish, causing a tornado to temporarily lift. In other cases a thunderstorm may go through cycles of strengthening and weakening. In the process it can produce multiple tornadoes one after another.
If a tornado hits a body of water (at which point it is called a waterspout) it can "suck up" some unlucky fish. These fall back to earth a little later.
If you look on the back, it should contain the address, e-mail address, and the 800-3 for moneygram. Also on the front it should have a mark that is a pinkish color and when heated or rubbed it disappears and then comes back.