Tropical Cyclone Formation (Cambridge (CIE) IGCSE Environmental Management): Revision Note

Exam code: 0680

Jacque Cartwright

Written by: Jacque Cartwright

Reviewed by: Alistair Marjot

Updated on

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

World map showing global storm development areas and tropical cyclone pathways. Arrows highlight hurricanes, cyclones, and typhoons in specific regions. Key included.
Distribution of tropical storms

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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Jacque Cartwright

Author: Jacque Cartwright

Expertise: Geography Content Creator

Jacque graduated from the Open University with a BSc in Environmental Science and Geography before doing her PGCE with the University of St David’s, Swansea. Teaching is her passion and has taught across a wide range of specifications – GCSE/IGCSE and IB but particularly loves teaching the A-level Geography. For the past 5 years Jacque has been teaching online for international schools, and she knows what is needed to get the top scores on those pesky geography exams.

Alistair Marjot

Reviewer: Alistair Marjot

Expertise: Environmental Systems and Societies & Biology Content Creator

Alistair graduated from Oxford University with a degree in Biological Sciences. He has taught GCSE/IGCSE Biology, as well as Biology and Environmental Systems & Societies for the International Baccalaureate Diploma Programme. While teaching in Oxford, Alistair completed his MA Education as Head of Department for Environmental Systems & Societies. Alistair has continued to pursue his interests in ecology and environmental science, recently gaining an MSc in Wildlife Biology & Conservation with Edinburgh Napier University.