Tropica Storms Flashcards
The nature and cause of tropical storms ?
Formation
This means that the sea surface is warmer (above 27 degrees). This causes warm moist warm to rise (convection)
Secondly, the rising air cools and condenses which creates clouds
Condensation release latent heat, this further warms the air and it rises,cools and condenses and releases further latent heat-forms continuous upwards convection currents
As the storm develops, warm moist air is drawn into the low-pressure system over the arm ocean, providing more fuel for convergence
The rising air rotates due to the Coriolis force, forming convection currents into one tropical storm
Upper atmosphere air rotation spreads air outwards and away from the storm
(the 4 C’s)
The distribution of storm events ….
Such storms occur between 5 and 20 degrees north and south of the equator
- Highest sun concentration
- Ocean warmed and hot air rises convection
- - Falls (10-20) north and south
- Therefore hurricanes occur in these paces
Concentration near Central America, East Asia and the subcontinents
- Secondary characteristics of distribution is due to the concentration of warm water at depths greater than 70m
Storms move from the equator north (if north of the equator) and south (if south of the equator)
- Secondary characteristics of the distribution is due to the influence of the coriolis effect
The magnitude and frequency of storm events …..
tropical revolving storms are measured on the Saffir Simpson Scale, a 5 point scale based solely upon wind speed
The average lifespan of a tropical storm is around 7-14 days (although it is believed that they may last longer due to climate change)
Every year 80-100 storms develop, 80% become tropical revolving storms
Primary effects ….
the immediate effects of a tropical storm is strong winds (often exceed 150km/h)
Heavy rainfall (often exceeding 200-300mm)
Storm surges
Secondary effects ….
storm surges can cause structural damage to buildings, roads and bridges
Heavy rainfall can lead to severe flooding, landslides and mudslides
Storm surges often devastate low lying land such as river deltas and often cause the majority of deaths.
Environmental effects ……
Political effects ……
Social effects
Economic effects ….
Explain the physical and human factors affecting the vulnerability of a population to a tropical storm?
the intensity
Warnings and community response
Preparedness made by a community
The geography of the coastal area
Distance from the sea
Speed of movement (length of time over an area)
What are the impacts of climate change on tropical storms?
increase in the intensity
Decrease in the number of tropical storms, but an intense increase in the frequency of the most intense ones
Slow moving tropical storms will become more common
(This is because of the increase in temperatures of the polar regions. Less temperature difference between the tropics and the polar regions)
Response for tropical storms
Name high HDI
Hurricane Katrina, USA, 2005
Katrina Facts:
- characteristics of place / hazard
- primary / secondary events
- risk / vulnerable
- short / long term response
Characteristics of place:
- low lying river delta
- were not prepared for the levees to break (low tax base led to low levels of maintenace)
- one of the poorest cities in America
- distrust of government due to history neglect / slavery led to poor response response to evacuation order and relief effort
Characterics of the hazard:
- wind speed 280kmh
- Saffir Simpson: 5
- storm surge: 10 m
- 380mm in 12hrs of rainfall
Primary:
- heavy rainfall
- storm surge 10m
- high wind speeds
Secondary:
- losses of 200 billion
- 1234 deaths
- 1 million homeless
- 100,000 properties destroyed
Risks/ vulnerable
- were not prepared for the levees to break.
- poorer area, and low tax led to poor manintance of levees
Long term Management
- media backlash led to an extensive rehabilitation and reconstruction
- built Great Wall of Louisiana - new levee
Short Term Responses
- 10.5 billion in aid in month after storm
- national guard was mobilised and a state of emergency was declared (however a delayed response due to looting and homlessness)
Low HDI case study
Typhoon Haiyan, Phillipines 2013