7. A tropical cyclone is a
storm system
characterized by a large
low-pressure center and
numerous thunderstorms.
Tropical Cyclones:
Grounds of rotating, low-
pressure storms that form
around the equator.
8. Named according to region
where they develops:
Develop over the
Indian Ocean on worm waters
Develop over
Atlantic and eastern Pacific
Oceans
Develop over
western Pacific Oceans
All produce similar effects
Typhoon Odessa,
Philippines
Eye
15. The strongest of these
cyclones’ storms are
known in the US and
other parts of the
Atlantic ocean.
16. Progression: depression storm cyclone
Classified according to wind speeds
Tropical Depression - less than 39 m/h
Tropical Storm - between 39 m/h and 73 m/h
Tropical Cyclone - at least 74 m/h
17. Tropical cyclones are
intense, rotating, low-
pressure storms
Develop over warm,
tropical oceans
Produce strong
winds and heavy
rainfall
Can lead to immense
flooding
Destructive Winds
18. Tropical Cyclones require to basic
conditions to form: an abundant supply
of very warm ocean water and some
sort of disturbance to lift warm air and
keep it rising.
19. Warm water generates
formation of tropical cyclones
Ocean temperatures must be
at least 26.5°C which is worm
Over warm oceans moist,
humid air (water vapour)
Warm air moves along the
surface
This air converges and rises
rapidly
Intense rising of air forms low
pressure systems
20. As air rises, it cools, becomes
saturated and condenses
Water vapour condenses into
liquid droplets
Formation of thunderclouds
Condensation releases heat
stored in water vapour
This latent heat warms the
atmosphere
Air becomes lighter causing
strong updrafts
21. Air expands and diverges at higher levels
Occurs only where wind speed/direction remain constant (no wind
shear)
Air moves in at surface taking the place of rising air
This intensifies convergence
Creates wind and increases rising movement
Builds and progresses into a mature cyclone
22. Spinning of earth on its axis
produces wind deflections
(Coriolis Effect)
Causes rising air to spiral
around center (core)
Spirals with great force
Winds are now rotating,
rising and moving in to fill
spaces
Wind speeds increase and
cyclone grows
23. These conditions exist in all tropical
oceans except the south Atlantic
ocean and the pacific, west of the
South American coast ocean waters in
these areas are somewhat cooler.
24. winds are blowing counter-
clockwise around center core
winds are blowing clockwise
around center core
25. the clear, calm center of storm
Cool air descends into this center (downdrafts)
ring of thunderstorms close to eye
Eyewall produces the most devastating winds
curved groups of clouds and thunderstorms
Rainbands travel away from eye in a spiral motion
26. Occur when tropical cyclones reach land
Storm surge – raised swell of water
60 to 80 km across
Around 2 to 5 meters higher than normal tides
Created by heavy winds and cause flooding
27. Between 10 to 30° North and South of equator
Within the tropic of Cancer and Capricorn Poleward side of
the Intertropical Convergence Zone
Zone of low pressure (ITCZ)
Coriolis effect greatly reduced at equator No tropical
cyclones occur at equator
Tropical Cyclone
Appearances
ITCZ
30. November 12, 1970 The
deadliest tropical
cyclone recorded
Developed over Bay of
Bengal Gathered speed
as it moved northward
Devastated East Pakistan
(Bangladesh) and West
Bengal of India.
Storm Path
India
Bay of Bengal
31. Wind speeds
reached 115 m/h
Strength of a
category 3 hurricane
33 foot high storm
surge Massive storm
surge caused
flooding and fatalities.
Bhola Cyclone on November 11,
1970
A tropical cyclone is a powerful storm system that forms over warm ocean waters near the equator, characterized by a large low-pressure center and organized thunderstorms that rotate around it. These rotating, low-pressure storms develop due to the warm ocean waters providing the energy needed for their formation. The Earth's rotation influences the direction of their spin, with counterclockwise rotation in the Northern Hemisphere and clockwise rotation in the Southern Hemisphere. Tropical cyclones can bring strong winds, heavy rainfall, storm surges, and flooding, making them dangerous and destructive natural disasters that require preparedness and caution, especially for those living in coastal areas prone to these storms.
Cyclones, hurricanes, and typhoons are all names for tropical cyclones that develop in different regions of the world but share similar characteristics and effects. Cyclones form over the warm waters of the Indian Ocean, hurricanes develop over the Atlantic and eastern Pacific Oceans, and typhoons originate in the western Pacific Ocean. Despite their regional names, these storms are all intense low-pressure systems with rotating winds and organized thunderstorms that can bring strong winds, heavy rainfall, storm surges, and flooding. The destructive impacts of cyclones, hurricanes, and typhoons are similar, posing significant risks to coastal communities and requiring preparedness and response efforts to mitigate their effects and protect lives and property.