Tropical storms

Key conditions for formation

Warm water (temp- 27 degrees +)

Low wind shear (difference in wind speeds) in all parts of the atmosphere

Coriolis effect

Movement of water: warm surface water evaporates and rises before condensing and releases masses of energy- creating an area of low pressure, clouds form and remain unbroken by low wind shear

Storms move to the west via trade winds (blowing eastwards)

As the storm moves over warm water it has a high amount of energy thus a strong relentless storm

As a storm moves over land or cool water then the energy supply in greatly reduced and cut-off thus decreasing the power of the storm

Features image

Eye- the area of calm, 30 miles(50km) across with little winds, precipitation and no cloud cover and high temperature, this is due to a area of very low pressure situated around a column of descending air at the centre of the storm

Eye wall- the strongest area of the storm- strong winds (approx, 160mph), high amounts of rainfall and low temperature

Surrounding clouds/edges of the storm- wind speed decreases and clouds disperse, temp increases

Effects (typhoon Haiyan)

Responses (typhoon Haiyan)

Primary

Secondary

Short-term

Long-term

Buildings/Infrastructure destroyed (1 million homes, $13million damage)

High storm surges (600,000 hectares of farmland flooded

high amounts of flooding

8,000 killed

Airports out of operation (flights grounded)

People maid homeless/jobless

Local/national economy is decreased

Diseases spread due to water contamination

Houses rebuilt

Emergency aid

shelter

food and water

electricity generators

medical aid/first aid

State of emergency declared

fishing warning (not to fish)

Dead need to be buried to prevent disease outbreak

National tourism encouraged to boost economy

Flood defences built, flood resistant homes

$300mn appealed for to help