How warm seas contribute to hurricane

frequency and strength

3

Cool air

Eye

Eyewall

4

5

2

1

1. Sea surface temperatures rise above 26.5°C

2. Water evaporates and warm, humid air rises

3. Rising air cools, causing moisture to condense into clouds. Droplets form, releasing even more heat to power the storm. Low pressure over the sea draws more air upwards

4. The system spins as air rushes to the centre to fill the low pressure void

5. Once sustained winds reach 74mph, it is classified as a hurricane

How warm seas contribute to hurricane frequency

and strength

3

Cool air

Eye

Eyewall

4

5

2

1

1. Sea surface temperatures rise above 26.5°C

2. Water evaporates and warm, humid air rises

3. Rising air cools, causing moisture to condense into clouds. Droplets form, releasing even more heat to power the storm. Low pressure over the sea draws more air upwards

4. The system spins as air rushes to the centre to fill the low pressure void

5. Once sustained winds reach 74mph, it is classified as a hurricane

How warm seas contribute to hurricane frequency

and strength

3

Cool air

Eye

Eyewall

4

2

5

1

1. Sea surface temperatures rise above 26.5°C

2. Water evaporates and warm, humid air rises

3. Rising air cools, causing moisture to condense into clouds. Droplets form, releasing even more heat to power the storm. Low pressure over the sea draws more air upwards

4. The system spins as air rushes to the centre to fill the low pressure void

5. Once sustained winds reach 74mph, it is classified as a hurricane

How warm seas

contribute to hurricane

frequency and strength

Rising air cools, causing moisture to condense into clouds. Droplets form, releasing even more heat to power the storm. Low pressure over the sea draws more air upwards

Cool air

Eye

Eyewall

The system spins

as air rushes to the centre to fill the low pressure void

Once sustained

winds reach 74mph, it is classified as a hurricane

Water

evaporates and

warm, humid air rises

Sea surface temperatures

rise above 26.5°C

How warm seas

contribute to hurricane

frequency and strength

Rising air cools, causing moisture to

condense into clouds. Droplets form, releasing even more heat to power the storm. Low pressure over the sea draws more air upwards

Cool air

The system spins

as air rushes to the centre to fill the low pressure void

Once sustained

winds reach 74mph, it is classified as a hurricane

Eye

Eyewall

Water

evaporates and

warm, humid air rises

Sea surface temperatures

rise above 26.5°C