Ingredients for a Hurricane
- Warm ocean water — at least 26°C to a depth of 50 metres
- Atmospheric instability — warm, moist air rising rapidly
- Low wind shear — consistent winds at different altitudes so the storm structure is not torn apart
- Distance from the equator — at least 5° latitude so the Coriolis effect can start rotation
The Formation Process
Stage 1: Tropical Disturbance — A cluster of thunderstorms organises over warm water, often starting as an African easterly wave crossing the Atlantic.
Stage 2: Tropical Depression — Sustained winds reach 62 km/h. The system develops a closed circulation. It gets a number.
Stage 3: Tropical Storm — Winds reach 63-118 km/h. The storm gets a name. Rain bands spiral outward.
Stage 4: Hurricane — Winds exceed 119 km/h. An eye forms at the centre — a calm, clear column surrounded by the most intense winds (the eyewall).
The Saffir-Simpson Scale
| Category | Wind Speed | Damage |
|---|---|---|
| 1 | 119-153 km/h | Minimal — roof tiles, tree branches |
| 2 | 154-177 km/h | Moderate — roofs, small trees |
| 3 | 178-208 km/h | Extensive — structural damage |
| 4 | 209-251 km/h | Extreme — severe structural damage |
| 5 | 252+ km/h | Catastrophic — total destruction |
Why Hurricanes Weaken
Hurricanes lose power when they move over cool water, encounter wind shear, or make landfall (cut off from their warm-water fuel source).
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