3. Introduction
โฐCyclone is an intense while in the atmosphere
with very strong winds circulating around it in
anti-clock wide direction in the Northern
Hemisphere and in clock wise direction in the
Southern Hemisphere.
3
5. Extra Tropical Cyclones
โฐExtra tropical cyclones occur in
temperature zones and high latitude
regions though they are know to originate
in the postal regions.
5
6. Tropical Cyclones
โฐTropical Cyclones are large-scale
weather system developing over tropical or
sub tropical water.
โฐWhere they get organized into surface
wind circulation.
6
8. Formation of Cyclones
โฐStep 1: By means of low pressure.
โฐStep 2: The air bent upwards.
โฐStep 3: The swimming wind rotate faster and faster farming huge circle.
โฐStep 4: At the center of the storm is a column are called a the age is the rain.
โฐStep 5: As Cyclone build up beginner to more.
โฐStep 6: The strongest winds and heaviest rains are found lowering around the clouds.
โฐStep 7: This result in more rain being released in a day falls in a year.
8
10. Conclusion
โฐDisaster presentation mitigation and preparedness are better
for example first did kit, battery organized radio or TV etc...
โฐMainly our India have some organization for cyclone namely,
IMO-India Meteorological Department.
RSMC-Regional Specified Meteorological Centre.
10