Tropical Cyclones originate over oceans in tropical areas and coastal regions
When typhoons hit mountains and trees it decreases the strength of the typhoon
Typhoons are created because there is warm and cold air in the pacific ocean that will create typhoons.
Wind movement:
Determined by low pressure and high pressure
Lp and Hp makes the winds move
Always blow from the high pressure areas to the low pressure areas
Continuous Evaporation
Heat causes water to evaporate
Saturating clouds and making them heavy with moisture to eventually fall back to earth as rain
All the heat and air flow towards the eye creating typhoon
LPA
Warm, moist air rises from the ocean surface, creating low pressure area near the ocean surface
HPA
Air from HPA rushes towards LPA
This air is initially dryer and cooler but near the ocean surface, the air is heated and carries more water vapor from continuous evaporation.
Condensation
As the warm air rises toward the cooler parts of the upper atmosphere, it cools off and the water vapor and begin to condense to form clouds
Coriolis Effect
In the northern Hemisphere or above the equator the wind rotates counterclockwise around the storm center, and clockwise in the southern hemisphere this is called the “Coriolis effect”
Convergent Winds
The difference between HP and LP air pressure systems creates winds. Accumulation of high-speed winds moving toward a particular area which is called “convergent winds” These create an increase in air pressure.
Eye
A LP air pulls the air inward, creating a spiral that moves around the center, which then becomes the eye of the storm
eyewall
Clouds heavy with rain swirl around the eye, forming the eyewall where winds and rain are at their strongest
While air rises towards the eyewall, it converges and sinks into the eye, where it is compressed and heated