Edexcel IGCSE Geography 复习笔记 3.1.2 Tropical Cyclones
Edexcel IGCSE Geography 复习笔记 3.1.2 Tropical Cyclones
Causes of Tropical Cyclone Hazards
- Low pressure areas (less than 950mb)
- Tropical Cyclones require specific conditions to form:
- Sea surface temperatures over 27°C
- Between 5° and 20° north and south of the equator
- Low wind shear
- Deep layer of humid air
Stages of Tropical Cyclone Formation
- In the right conditions a tropical cyclone can form rapidly. It follows a number of stages:
- Warm, moist air rapidly rises forming an area of low pressure
- Air from high pressure areas rushes in to take the place of the rising air
- This air then rises forming a continuous flow of rising air
- As the air rises it cools and condenses. This releases heat energy which helps to power the tropical cyclone
- Air at the top of the storm goes outwards away from the centre of the storm
- The Coriolis force causes the rising air to spiral around the centre.
- Some of the air sinks in the middle of the storm forming the cloudless, calm eye.
- The tropical cyclone moves westwards from its source
- When a tropical cyclone makes landfall or moves over an area of cold water it no longer has a supply of warm, moist air and it loses speed and temperature. Rainfall and winds decrease
Features of Tropical Cyclone
- Tropical cyclones have a number of features:
- Heavy rainfall
- High wind speeds (over 74kmph)
- Storm surges
- Calm eye
- Highest winds and heaviest rain in the wall of the eye
- Diameter up to 800km
Worked Example
Explain the formation of a tropical cyclone. (4)
- Identify the command word
- The command word is 'explain'
- The focus of the question is 'the formation of a tropical cyclone'
- Questions such as this are easiest to complete if you view them as a series of steps
Answer
- The formation of a tropical cyclone:
- Warm sea water (27°C or over) around tropics (1)
- There are high levels of evaporation and condensation of water vapour from warm water leading to cumulonimbus cloud formation (1)
- The high levels of evaporation and condensation of water vapour provides energy for strong winds (1)
- Strong Coriolis Force close to the equator make winds spin and moves them away from the equator (1)
- The tropical cyclone move westwards due to east-west winds in tropics and strengthen as they move over warm waters (1)
- The tropical cyclone dissipates when it reaches land or outside tropics as supply of warm, moist air cut off (1)
Exam Tip
Remember conditions such as warm oceans and the Coriolis Force exist at all times but tropical cyclones do not form all the time. It is the combination of all the right conditions coming together which leads to tropical cyclone formation.
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