Wind Tornado Process.You will never see a tornado? Cyclones winds rotate at a very fast speed of more than 63 kmh dedicated to a long straight with a maximum incidence of about 5 minutes. Javanese Leysus call a tornado is wind, wind Indonesia called Bohorok and there are other names in the United States if called Tornado, which has a speed of up to 320 km / h and a diameter of about 500 meters. Tornado is most common in the afternoon or evening in the season pacaroba also called peraliah summer rain. Wind can destroy everything in its path, because the thing affected his grave will be lifted and discarded.
These are signs of the appearance of a tornado
twelve o'clock seen towering white clouds high Sagat cauliflower, then became a dark cloud, accompanied by gusts of cold air and the wind began to shake the trees to the left and right, shortly after the wind Once all added quickly followed and sometimes heavy rain accompanied by hail. Seen in a swirl of black clouds wind tapered towards the ground (soil).
The cause of the occurrence of earthquake
Cause a tornado
The big difference in the temperature of the hot air meeting cold, causing fought each other and forming a tornado that started from a small wind up eventually extended and very dangerous.
The appearance of a tornado
Growing step in the cloud In the case of air currents rise to the top was very powerful. When the rains have not yet started to fall, water droplets and ice crystals are still subject to air currents that rise to the top of the cloud.
Adult water points / stage manager are no longer limited and the air rises to the top of the cloud. when the rain fell causing friction between air currents up and down. Air mass temperature dropped sharply colder than the ambient air. Between the downward currents shear torque current occurs air, forming the vortex air flow is spinning faster and faster, like a cyclone "lick" the earth like a tornado and extremely dangerous. Sometimes it is also accompanied by a strong rain that forms a jet (water outlet) water.
Phase gone when there is no air masses rise. Air mass begins to fall extends along the cloud. condensation start stop, start descending air is weakened so that growth end Cb cloud.
Tornado liquidation process
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