Tropical storms
are intense low-pressure weather systems with heavy rain and strong winds that spiral around the centre. When they reach land or cooler water, they lose strength. Since they lose heat and moisture and there is more friction.
Conditions for formation of tropical storm
- wind shear is low
Spinning of the tropical storm
They spin anti clockwise in the northern hemisphere and clockwise in the southern hemisphere.
Eye
The center of the storm. It is up to 50km across and is caused by descending air. There is low pressure, no clouds, no rain and a high temperature.
Eyewall
The eye is surrounded by eyewall, where there’s spiraling rising air, very strong winds, storm clouds, rain and low temperature.
Edges of the storm
The wind speed falls, the clouds become smaller, the rain becomes less intense, the temperature increases.
How climate change can affect tropical storms
The primary effects of tropical storms
Secondary effects of tropical storms
Immediate responses to tropical storm
Happen when a storm is forecast to hit an area and immediately afterwards.
Long-term responses to tropical storm
Prediction of tropical storms
Planning to reduce the impacts of tropical storms
Protection against tropical storms
Hurricanes location
In the Atlantic and Eastern Pacific Ocean.
Typhoons location
In the west of the Northen Pacific Ocean.
Cyclones location
Indian and South Pacific Ocean.
Location of tropical storms
Found in areas of low latitude, between 5 degrees and 30 degrees north and south of the Equator.
Why does not tropical storm develop along the equator?
Because the Coriolis effect is not strong enough here for the tropical storm to spin.
The hot rising air…
draws up more air and large volumes of moisture from ocean, causing strong winds.
The Coriolis effect causes the air to…..
spin upwards around a calm central eye.
As the air rises, it cools and…
condenses to form large, towering cumulonimbus clouds.
Cumulonimbus clouds generate…
torrential rainfall.
The heat is given off when the air…
cools powers the tropical storm.