Tropical Cyclone Formation (Cambridge (CIE) IGCSE Environmental Management): Revision Note
Exam code: 0680
What conditions are needed for tropical cyclone formation?
Tropical cyclones are among the most powerful natural hazards on Earth
Understanding how they form, how they affect people, and how we can manage their impacts is important
What's the difference between hurricanes, cyclones, and typhoons?
They all describe the same type of storm, but the name varies by region
They are known as:
Typhoons in the South China Sea and the western Pacific Ocean
Hurricanes in the Gulf of Mexico, the Caribbean Sea and the west coast of Mexico
Cyclones in the Bay of Bengal, the Indian Ocean and northern Australia

Development of tropical cyclones
Tropical cyclones are rotating, intense low-pressure systems (below 950mb)
They need specific conditions to form
Form between 5° and 30° latitude north or south of the Equator
Cyclones require the Coriolis effect to spin, which is too weak at the Equator
Therefore, they form away from the Equator, usually between 5° and 30° latitude
They do not form at higher latitudes because the water is too cold
Ocean temperature of at least 27 °C
Warm water is essential because it provides the heat energy needed to drive the storm
Ocean temperatures must be in excess of 27°C
Warm water evaporates rapidly, adding heat and moisture to the rising air
This fuels towering cumulonimbus clouds and intense rainfall
Warm water = more evaporation = more latent heat = stronger cyclone
Ocean depth of at least 60 m
Warm water must extend to at least 60 metres in depth
Deep warmth ensures the storm continues to gain energy without mixing with cooler water from below
Shallow warm layers are quickly disrupted by strong winds
Tropical cyclones begin when tropical oceans are at their warmest, which is usually late summer (Nov-April in the southern hemisphere and June-Nov in the northern hemisphere)
The Pacific Ocean sees the largest number of tropical storms, followed by the Indian Ocean, and lastly, the Atlantic
Tropical storms in the western Pacific are the strongest
Impacts of tropical cyclones
Cyclones affect large areas because they combine high winds, intense rainfall, storm surges, and flooding
Damage to buildings and infrastructure
Roofs ripped off; buildings collapse
Power lines, roads, bridges and communication networks are destroyed
Loss of crops
Crops flattened by wind or drowned by floodwater
Saltwater storm surges ruin farmland
Loss of livestock and habitats
Animals drowned or injured
Forests uprooted; coastal ecosystems damaged
Evacuation of people and livestock
Millions may be moved to safer areas
Displacement disrupts daily life and livelihoods
Flooding
Torrential rain, overflowing rivers and storm surges cause widespread flooding
Urban drainage may be overwhelmed
Landslides
Heavy rainfall saturates slopes, triggering landslides
Buries homes, roads and farmland
Contamination of drinking-water supplies
Floodwater mixes sewage with clean water
Saline intrusion from storm surges pollutes wells and aquifers
Water-related disease
Outbreaks of cholera, dysentery, giardia and other infections
Standing water encourages mosquito breeding
Financial losses
Huge repair costs for transport networks, homes, utilities and businesses
Loss of agricultural production and tourism
Long-term economic disruption
Human health
Injuries and deaths from collapsing structures and debris
Psychological stress and trauma after disaster
Poor shelter conditions increase sickness
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