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A-Level AQA Geography > Hazards: Tropical Storms > Flashcards

Hazards: Tropical Storms Flashcards

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1
Q

What are the characteristics of tropical storms?

A
  • develop in the tropics
  • intense low-pressure weather systems
  • 200-700km in diameter
  • violent storms
  • last around 7-14 days
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2
Q

What are the conditions required for tropical storms?

A
  • sea temperature above 27ºC (provides a source of heat for rising air)
  • ocean depth of at least 70m
  • location of at least 5º N/S of the equator (Coriolis effect is strong enough to make them spin)
  • emergence of air in the lower atmosphere, either within the ITCZ or along the boundary between cool and warm air masses (this forces warm air to rise)
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3
Q

Describe the distribution of tropical storms?

A
  • 5º-20º north or south of the Equator (in lateral bands)
  • always form over oceans
  • in oceans with a depth of a minimum of 70m
  • never occur at the Equator
  • occur at the ITCZ
  • move westerly due to easterly winds in the tropics
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4
Q

Why do tropical storms occur 5º-20º north or south of the Equator (in lateral bands)?

A

Insolation from the Sun is the greatest at the Equator, warms the ocean and storms need enough energy in the water for evaporation and warm, moist air to rise

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5
Q

Why do tropical storms always form over oceans?

A
  • ocean provides a constant source of rising warm air
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6
Q

Why do tropical storms form in oceans with a minimum depth of 70m?

A

needs to be enough hot water to give the energy needed to drive a tropical storm

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7
Q

Why do tropical storms never occur at the equator?

A

coriolis effect is required to change individual storms into tropical storms, by spinning storms together which concentrates the energy
- coriolis effect is very weak at the equator

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8
Q

Why do tropical storms occur at the ITCZ?

A

Trade winds fuel storms with moisture, air rising will create low pressure at Earth’s surface, wind results in air moving down the pressure gradient (high to low)

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9
Q

What is the ITCZ?

A

Intertropical Convergence Zone

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10
Q

Tropical storm formation part 1

A

warm oceans cause warm moist air to rise, by convection, air pressure falls, rising air cools and condenses forming clouds

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11
Q

Tropical storm formation part 2

A
  • condensation releases latent heat
  • this warms the air and it rises, cools and condenses and releases further latent heat (forming continuous upward convection currents)
  • thick vertical clouds grow rapidly and give heavy rainfall and thunderstorms
  • this causes a further fall in air pressure at the surface
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12
Q

Tropical storm formation part 3

A
  • convergence occurs, warm moist air is drawn into the low-pressure system from different directions causing wind
  • the rising air rotates and the hurricane follows a spiral path due to the Coriolis force
  • upper atmosphere air rotation spreads away from the storm
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13
Q

Explaining the processes of a tropical storm: convection

A
  • heat energy is transferred through a substance from hot water to the cooler air above by convection
  • the air above the ocean is heated and as it warms it rises
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14
Q

Explaining the processes of a tropical storm: evaporation

A
  • water changing state from a liquid to a gas
  • hot water from the ocean evaporates to become water vapour cooling the ocean
  • this provides potential energy
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15
Q

Explaining the processes of a tropical storm: condensation

A
  • water vapour changing state into liquid water, this releases energy
  • water vapour cools as it rises in the cool upper atmosphere where it condenses and creates potential for heavy ain
  • condensation releases energy which leads to further warming of the air and air is forced to rise, adding more energy to the storm
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16
Q

What is the magnitude of tropical storms?

A

Varies due to central pressure, wind speed and strom surges

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17
Q

What is the lifespan of a tropical storm?

A

usually between 7-14 days

- however this is dependent of the magnitude, relative size and the supply of latent heat and moisture

18
Q

What does is the frequency of tropical storms?

A
  • depends on conditions in the area
  • climate change is leading to warmer ocean temperatures, greater frequency and magnitude
  • therefore in the future they could occur further than 20º N or S of the equator
19
Q

What are the primary effects (hazards) of tropical storms?

A
  • winds (can be an extreme of 250km/h)

- heavy rainfall (exceeding 200-300mm)

20
Q

What are the secondary effects (hazards) of tropical storms?

A
  • storm surges
  • landslides
  • coastal flooding
  • river flooding
21
Q

Q: Evaluate risk management designed to reduce the impacts of tropicak storms

A

Reduce the impacts gives context to the question
prediction: hurricane forecasting and modelling are the most effective
protection/preparation: moderate effectiveness
prevention: cloud seeding in the worst

22
Q

Why is land use planning one of the most effective ways to reduce impacts?

A
  • Development is prevented in vulnerable areas (e.g. in low-lying areas = storm surges
  • this dramatically decreases risk to loss of life or loss of property and normality can be restored much faster after the event
  • furthermore can help identify extremely vulnerable areas = enforcement
  • sea walls, breakwaters and flood barriers can be built
  • sea wall that was built to protect Galveston (Texas) from further flooding, after the storm surge of 1900 that killed over 6,000 people, however this was so expensive and will not be repeated elsewhere
23
Q

Why is land use planning not a very effective way to mitigate impacts?

A
  • it can only be useful in areas that have the capacity to implement that type of strategy
  • rapidly urbanised places result in many being forced into living in vulnerable spots as there is no alternative
  • for example in Tacloban some areas have over 2000Km^2, limiting options for residents forcing them to live in areas of high risk along the coast
24
Q

Why is hurricane forecasting and warning systems a effective way of managing tropical storm hazards?

A
  • data from satellites and aircrafts is compiled into supercomputers to predict path of the storm and enables for decisions of warning and evacuations
  • reduces social losses, but not property
  • individuals can empower themselves and protect themselves
  • the National Hurricane Centre in Florida gather data from stalleties in both land and sea and maintains 24/7 surveillance of tropical storms that have the potential to become hurricanes and pose threat to life in the USA
25
Q

Why is hurricane forecasting and warning systems not an effective way of managing tropical storm hazards?

A
  • lots of technology is required for monitoring to be accurate and reliable, difficult for LEDCs to fund
  • evacuation is extremely expensive, in the USA it’s been estimated that evacuation of coastal areas costs $1 million per km^2 from losses to tourism and business
  • hurricanes can follow an erratic path so it’s hard to give more than a 12-18 hour warning, if communication is poor this is insufficient
26
Q

Why is emergency action only a moderately effective management method of tropical storms?

A
  • helps minimise loss of life as services are able to support or rescue those in need
  • however it’s expensive and doesn’t reduce the number of casualties before the storm strikes, which would be more effective
  • Hurricane Katrina has 1242 deaths and despite emergency aid being delayed had less deaths than Typhoon Haiyan (6,200) as there were already other measures in place
27
Q

Why is cloud seeding the least effective management strategy?

A
  • a strategy to prevent storms from happening
  • extremely expensive, not even been proven and all research has been abandoned and never picked up again
  • will not reduce loss of life or reduce property damage
  • US military attempted trials in the 1960s that were very unsuccessful and even feared that it could make the storms worse
28
Q

What are the physical and human factors affecting vulnerability to a tropical storm?

A
  • intensity of the storm (1-5 category on Saffir-Simpson)
  • speed of movement
  • distance from the sea
  • physical geography of coastal area
  • preparations made by a community
  • warnings and community response
  • characteristics of hazard vs place
29
Q

What were the characteristics of hurricane katrina hazard?

A

280 km/h winds
Category 5
10m storm surge
380mm rainfall in 12hrs

30
Q

What were the impacts of hurricane katrina?

A 
$200bn in losses
1242 deaths (0.3% of pop of New Orleans)
1 million homeless
1 million displaced
110,000 properties destroyed
31
Q

What is the case study of a tropical storm in a place of high HDI?

A

Hurricane Katrina
New Orleans
USA 2005

32
Q

What are the environments characteristics of New Orleans?

A

Levees were not expected to break

Low lying river delta area

33
Q

What were the economic characteristics of New Orleans/USA

A

USA GDP of $19 trillion
Low tax base = low levels of maintenance of protection
Inadequate insurance protection

34
Q

What were the socio-cultural characteristics of New Orleans?

A
  • Distrust of the government due to history of neglect and slavery led to poor response of evacuation (150,000 remained by choice) and relief effort
35
Q

What were the political characteristics of New Orleans?

A
  • State of emergency not declared until 48hrs before the event struck, not enough time for a sufficient evacuation to be managed
  • emergency rescue and relief was delayed due to lack of co-ordination
  • FEMA did not act on models which predicted the disaster
36
Q

What is the case study for a tropical storm in an area of low HDI?

A

Typhoon Haiyan
Tacloban
Philippines
2013

37
Q

What were the hazard characteristics of Typhoon Haiyan?

A

250km/h wind speed
Category 5
6m storm surge
300mm rainfall in 12 hrs

38
Q

What were the impacts of Typhoon Haiyan?

A 
$3 bn in losses
6200 deaths (2.5% of population in Tacloban)
2 million left homeless
6 million displaces
ALL properties destroyed
39
Q

What were the environmental characteristics of Tacloban?

A

city based on the coast of a low-lying area

no extensive defences

40
Q

What were the economic characteristics of Tacloban?

A

Rapidly industrialising and urbanising
Speed of development hinders land use planning (poor infrastructure quality)
65% of the population in vulnerable areas due to rapid urbanisation

41
Q

What were the socio-cultural characteristics of Tacloban/Philippines?

A

1 in 3 live in poverty
Many lack education to understand how to protect themselves or respond properly
Rapidly growing population (+2000 per square km)

42
Q

What were the political characteristics of Typhoon Haiyan?

A

Insufficient hazard management
State of emergency declared but there was widespread violence
Local government collapsed as many victims were government officials

A-Level AQA Geography (13 decks)

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