Hazards Flashcards

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1
Q

What is a hazard?

A

“A hazard is a perceived natural event which has the potential to threaten both life and property.”

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2
Q

What is a disaster?

A

“A serious disruption of the functioning of a community or a society involving widespread human, material, economic or environmental losses and impacts, which exceeds the ability of the affected community or society to cope using its own resources.”

Simple explanation : a hazard that has enormous impacts on people and property

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3
Q

List some examples of hazards

A

Earthquake, tsunami, floods, acid rain, volcanoes, hurricane/cyclone/typhoon, mudslide (lahars), storm (tropical/snow/sand), sink hole, pandemics, lightning, tornado, wildfires, heatwaves, mud volcanoes, rockfall, climate change, avalanches, geyser etc.

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4
Q

What are the three classifications of hazards?

A
  • Geophysical -> driven by Earth’s internal energy sources e.g. volcanoes
  • Atmospheric -> driven by processes in the atmosphere e.g. wildfires
  • Hydrological -> driven by water bodies, mainly oceans e.g. floods
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5
Q

What are the common characteristics of natural hazards?

A
  • Little or no warning
  • Clear origin or distinctive effects
  • Exposure to risk
  • Scale and impact requires emergency response
  • Most damage and loss of life occurs shortly after the hazard but impacts may last into the future
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6
Q

How can impacts of hazards be classified?

A

They can be classified as primary or secondary:

Primary -> direct result of the hazard - they are immediate e.g. ground shaking in an earthquake (seismic activity)

Secondary -> occur after the event has occurred or as a result of the primary hazard e.g. collapsed buildings

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7
Q

What are the responses to natural hazards?

A

1. Fatalism - people believe they cannot influence the outcome of the event and so do nothing to prevent/manage it
2. Adaptation - attempts of the communities/people to live with the hazard events (adjustments to living conditions)
3. Fear

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8
Q

What is risk sharing?

A

​A form of ​community preparedness​, whereby the community ​shares the risk ​posed by a natural hazard and ​invests collectively to mitigate the impacts of ​future hazards

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9
Q

State the Disaster Risk Equation

A

RISK = HAZARD x VULNERABILITY
——————————
MANAGEMENT

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10
Q

What factors may lead to vulnerability?

A

Physical (age, disability),
Social (carer, family),
Economic (job),
and Environmental (level of land).

Potentially cultural and political factors as well as knowledge.

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11
Q

What factors influence hazard perception?

A
  • Socio-economic status
  • Level of education
  • Employment status
  • Religion, cultural background
  • Family situation
  • Past experience
  • Personal values and personality
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12
Q

What is magnitude?

A

The size of the hazard.

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13
Q

What is intensity?

A

The power of a hazard i.e how strong it is and how damaging the effects are.

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14
Q

What is The Park Model?(RRR)

A

It is a model that shows the steps carried out in the recovery of a hazard, giving indication of time frame.
The steepness of the curve shows how quickly an area deteriorates and recovers.
The depth of the curve shows the scale of the disaster (the lower the curve, the lower the QoL)

Stage 1 - Relief (hours, days)
Immediate local response
Appeal for foreign aid

Stage 2 - Rehabilitation (days, weeks, sometimes months)
Services begin to be restored
Temporary shelters and hospitals
Food and water distributed
Foreign aid

Stage 3 - Reconstruction (weeks, years)
Infrastructure rebuilt
Area back to normal
Same or better QoL

Photo of the diagram

Evaluation
✓ Shows link between Quality of Life and hazardous events
☓ Very generalised with no quantitative data
✓ Focuses on relief, rehab and reconstruction which helps understanding recovery
✓ Good for comparing different events and responses
☓ Does not examine that some countries need more help than others from outside
☓ Doesn’t address level of development/wealth

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15
Q

What is The Hazard Management Cycle?(PPRR)

A

The Hazard Management Cycle outlines the stages of responding to events.

  1. Prevention and Mitigation - strategies to lessen the effects of another hazard e.g. barriers, warning signals, risk assesment, planning
  2. Preparation - being ready for an event to occur e.g. public awareness, education, training
  3. Response - immediate action taken after event e.g. evacuation, medical assistance, rescue
  4. Recovery - long-term responses e.g. reconstruction, restoration of infrastructure & services

Photo of the diagram

Evaluation
☓ Too generic and unquantifiable
✓ Easy to remember four-stage sequence
✓ Centered around 4 Ps: prediction, prevention, protection and preparedness
☓ Not as much detail as Park Model
✓ Place detail can be inserted into the model

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16
Q

What is Continental Drift and who proposed it?

A

It was first proposed by Alfred Wegener in 1915.
It states that the Earth’s crust is divided into continental and oceanic areas. The proportion of continental areas has increased through geological time and so have the positions of them and the oceans.

The evidence for continental drift is as follows:
- Jigsaw fit
- Tectonic fit
- Geological fit
- Glacial deposits
- Palaeo-climates and lithologies
- Fossil distributions
- Palaeo-magnetism

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17
Q

How is the Earth structured?

A

It has a layered structure…
- The outer layer of crust/lithosphere
- The asthenosphere
- The mantle
- Outer core
- Inner core at the centre of the Earth

Diagram

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18
Q

What are convection currents?

A

They occur within the molten rock in the mantle. Liquid rock close to the core is heated and rises as it is less dense. When it reaches the crust it is forced sideways as it often cannot pass through the crust. The friction between the convection current and the crust causes the tectonic plate to move. The liquid rock then sinks back towards the core as it cools and the process repeats.

Diagram

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19
Q

What is the Earth’s crust made of?

A

Continental Crust
- Thick (10-70km)
- Buoyant (less dense than oceanic crust)
- Mostly old

Oceanic Crust
- Thin (~7km)
- Dense (sinks under continental crust)
- Young

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20
Q

What happens at constructive boundaries?

A

The plates move apart leading to new material erupting to fill the gap in the form of a shield volcano.

Diagram and further explanation

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21
Q

What happens at destructive boundaries?

A

The plates move towards each other. This usually involves a continental plate and an oceanic plate. The oceanic plate is denser than the continental plate. As they move together, the oceanic plate is forced underneath the continental plate. This is called a subduction zone.

Diagram and further explanation

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22
Q

What happens at conservative boundaries?

A

The plates move parallel to each other. As the plates move, friction occurs and plates become stuck. Pressure builds up because the plates are still trying to move. When the pressure is released, it sends out huge amounts of energy, causing an earthquake. The earthquakes at a conservative plate boundary can be very destructive as they occur close to the Earth’s surface. There are no volcanoes at a conservative plate margin.

Diagram and further explanation

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23
Q

What volcanoes form at constructive plate boundaries and what are their eruptions like?

A

Shield volcanoes
- Basaltic lava which is high in temperature
- Low silica and gas content
- Non-acidic
- Runny lava
- Less viscous lava (sticky)
- Less violent eruption
- Shorter periods between eruptions

Fissure volcanoes
- Low viscousity

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24
Q

What volcanoes form at destructive plate boundaries and what are their eruptions like?

A

Composite volcanoes
- Violent eruptions
- Highly viscous lava (sticky)
- Acidic
- Longer periods between eruptions
- Andesitic lava which is lower in temperature and has more silica

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25
Q

What are trenches?

A

Trenches are long, narrow depressions on the seafloor that form at the boundary of tectonic plates where one subducts under the other (destructive plate boundaries) e.g. the Mariana Trench

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26
Q

How are volcanic hotspots formed?

A

Volcanic hotspots are formed by a localised plume of rising, hot mantle which partially melts the overlying plate due to the reduction in pressure.
Because magma is less dense than solid lithosphere it rises up and erupts onto the surface, cooling as it hits the ocean which creates active volcanic islands.
As the plate moves over the plume the volcanic island is carried away, becoming extinct due to it being removed from its magma source. A new volcanic island is formed above the hotspot to fill the gap and the process repeats, forming a chain of volcanic islands. The old islands subside as they are carried away, those under the sea forming guyots. An example of a volcanic hotspot is the Hawaiian Islands.

Diagram

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27
Q

How is the magnitude of a volcano measured?

A

It is measured using Volcanic Explosivity Index (VEI).

28
Q

What are the hazards associated with volcanoes?

A
  • Lava flows
  • Lahars (rainwater flowing with ash mixed in, similar to mudflow)
  • Glacial floods (jökulhlaups)
  • Tephra (rock ejected by a volcano)
  • Acid rain
  • Toxic gases
  • Pyroclastic flows
29
Q

CASE STUDY
Eyjafjallajökull - 2010 eruptions

A

General
Eyjafjallajökull lies in the south of Iceland and is 1660m high. Eyjafjallajökull achieved a VEI (Volcanic Explosivity Index) of 4 when its ash plume was blown almost 10km into the atmosphere. Seismographs were registering swarms of shallow earthquakes, suggesting rising magma before the eruption. Eyjafjallajökull erupted in the years 920, 1612, 1821, and 2010.

Causes
The volcano was overlain by an ice cap and as the magma rose to the surface, the lava that was emitted passed through the ice and melted it. The mix of water and lava increased the explosivity and helped eject ash high into the atmosphere where it caused the most serious impacts of the eruption. Much of the ash emitted was very fine so the percentage of ash being transmitted over long distances was very high. Eyjafjallajökull is on a constructive plate margin and so it is expected to be less explosive than those on destructive ones.

Impacts

Local:

  • Livestock taken inside to escape ash. Also, fluoride was deposited from the volcano on grazing land.
  • The local population was evacuated.
  • Local flooding as the glacier melts. A main road route had to be breached to let the surplus water flow safely to the sea rather than allowing the rush of water to destroy an important bridge.
  • Fresh fish exports, a major local industry, were badly affected with loss of income.

Global:

  • All flights cancelled from some airports on some days.
  • The Channel Tunnel and the cross-Channel ferries did a lot of extra business whilst this ash eruption lasted.
  • The eruption occurred at the end of the Easter break so many people were stuck abroad.
  • Huge reduction in aircraft noise around major airports. Improved quality of life temporarily.
  • Due to reduction of air traffic, 2.8 million tonnes less of carbon dioxide was emitted during the period.

Response

  • About 700 people from this rural area were evacuated.
  • Thousands of flights were cancelled across Europe. Airports closed in western Scotland and the south of England, including Heathrow.
  • Scientists are investigating how the two volcanoes are linked subterraneanly to try to predict when and why Katla might next erupt as it is more dangerous.
30
Q

CASE STUDY
Montserrat 1995-present eruption

A

General
1995-present. Montserrat is situated within the northern part of the lesser Antilles. This is an island arc formed where the South American tectonic plate subducts beneath the Caribbean. It is a strato volcano with dacite lava (sticky and explosive). Montserrat is a LIC and a small island, only stretching around 20km.

Causes
Lava domes were created as a result of viscious, silica-rich laval building up at the top of the volcanoes. When the lava eventually becomes too heavy, the domes collapse, resulting in andesitic lava and pyroclastiic flows. Chances Peak catostrophically erupted, sending 5 million cubic metres of hot rock and gases down its sides.

Impacts

Primary:

  • The South of the island, including Plymouth (the capital), was covered by these pyroclastic flows of hot ash, rocks, boulders and lahars.
  • Fires associated with the pyroclastic flows killed 19 people. 2/3 of all houess were buried by ash or flattened by rocks.
  • Down to 3 clinics due to the eruption.

Secondary:

  • South remains an exclusion zone to this day.
  • Tourism is now one of the islands main sources of income due to the eruption with some tourist trips to the South of the island.
  • Half of population forced to migrate

Reponses

  • Temporary schools set up and medical support and food
  • 2 emergency clinics set up by other countries, lacking staff but not supplies
  • Temporary port set up
  • Evacuated citizens from South
  • 3-year development program for infrastructure funded by UK
31
Q

How are earthquakes formed?

A

When two plates move side by side, friction builds up and pressure increases; this pressure is stored as potential energy, it cannot move so it just builds up. When the pressure becomes too much, the plates eventually move. All of the energy that has been built up must go somewhere, so it is transferred into kinetic energy, which is released and vibrates throughout the ground. The further away from the focus, the weaker the shockwaves, as the energy is transferred into the surroundings. They manifest themselves by a shaking or displacement of the ground and sometimes tsunamis. Lead to loss of life/destruction of property.

32
Q

What are intraplate earthquakes?

A

The are earthquakes that occur within the interior of a tectonic plate, away from plate boundaries in areas that are not typically associated with seismic activity.

33
Q

What are the two main types of seismic waves and what can they travel through?

A
  • Body waves, travel through the earth’s inner layers
  • Surface waves, can only move along the surface of the planet like ripples on water
34
Q

What are examples of body waves?

A
  • P waves (primary waves). P waves are the fastest kind of seismic wave. They move through solid rock + fluids. Pushes and pulls rock and moves through like sound waves. Longitudinal
  • S waves (secondary waves). Only through solid rock. Slower. Up and down or side-to-side. Transverse
35
Q

What are examples of surface waves?

A
  • Love waves. Fastest surface waves. Moves ground from side to side. Transverse
  • Rayleigh waves. Rolls along the ground like a wave, rolls across a lake or ocean. Moves the ground up and down and side-to-side in the same direction the wave is moving. Much larger than other waves and causes the most shaking
36
Q

What is the focus of an earthquake?

A

The focus is the point underground where the earthquake originates from.

37
Q

What is the epicentre?

A

The epicentre is the
area above ground that is directly above the focus

38
Q

How does the Richter Scale measure earthquakes?

A

Ranks earthquakes based on the amount the ground shakes 100km from epicentre. A well known example of a magnitude (M) scale. Measured from 2-9.

Image

39
Q

How does the Mercalli Scale measure earthquakes?

A

Measures the intensity of shaking occurring at a given point on the Earth’s surface. Uses 1-XII using Roman numerals. Subjective meaning there is a risk of bias.

Image

40
Q

What is liquefaction?

A

When soil is saturated, the vibrations of an earthquake cause it to act like a liquid. Soil becomes weaker and more likely to subside when it has large weight on it. Liquid emerges from the ground.

41
Q

What are the hazards associated with seismic events?

A
  • Shockwaves (seismic waves)
  • Tsunamis
  • Liquefaction
  • Landslides/avalanches
  • Building collapse
42
Q

How do tsunamis occur?

A

When an oceanic crust is jolted during an earthquake, all of the water above this plate is displaced. The water travels fast but with a low amplitude (height). As it gets closer to the coast, the sea level decreases so there is friction between the sea bed and the waves. This causes the waves to slow down and gain height, creating a wall of water that is on average 3m high, but can reach 30m.

43
Q

CASE STUDY
Haiti 2010 earthquake

A

General
Haiti is located in the Caribbean Sea and is located on the western one-third of the island of Hispaniola in the Caribbean Sea, Haiti shares the island with the Dominican Republic. The earthquake occurred on January 12, 2010, with a magnitude of 7.0. The epicentre was near the town of Léogâne, 16 miles away from the capital of Haiti, Port-au-Prince. Haiti is a LIC that fAqaces limited access to basic services and a high poverty rate, the majority of the population relying on agriculture for their livelihoods. It is estimated that 230,000 people lost their lives in the earthquake. Deforestation in the country is high due to it being used to obtain charcoal leading to landslides occurring more easily.

Causes
The earthquake was caused by a movement along the Enriquillo-Plantain Garden fault zone which runs through the Southern part of Haiti. The fault exists due to tectonic activity between the Caribbean and North American plates. The plates are moving apart, the release of accumulated stress along the fault causing the sudden shaking of the Earth’s crust which resulted land movement of 1.8 metres and the destruction of 60% of the capital city.

Impacts

Primary:

  • Collapse and destruction of buildings and infrastructure
  • Loss of life, injuries
  • Displacement of people

Secondary:

  • Disruption of essential services like transport or healthcare
  • Spread of diseases due to inadequate sanitation
  • Economic setbacks/jobs lost

Response

Short term:

  • Emergency services
  • International efforts to provide shelter, food and clean water
  • Search and rescue operations
  • Temporary schools

Long term:

  • Attempts to attract foreign investment via offering tax incentives and providing support for investment projects
  • Improvements to infrastructure by investing in various sectors such as tourism, transport, energy, water, telecommunications and upgrading roads
  • Constructing new homes
  • More sustainable programs implemented
44
Q

CASE STUDY
Sendai 2011 megaquake

A

General
Sendai is located in the northeastern part of Japan, specifically in the Tohoku region. It is located on the coast, facing the Pacific Ocean. On March 11th, 2011, a magnitude 9.0 earthquake struck at 2:46 PM. The epicentre was located some 130 km east of the city of Sendai. Hundreds of aftershocks, dozens of magnitudes 6.0 or greater and two of magnitude 7.0 or greater, followed in the days and weeks after the main quake. The tsunami wave measured 10m and there was estimated to be 28,000 casualties.

Causes
The earthquake was caused by the rupture of a stretch of the subduction zone associated with the Japan Trench, which separates the Eurasian Plate from the subducting Pacific Plate. The earthquake sent a large burst of energy up the ocean, displacing a large quantity of water. The upward motion sends a series of waves in all directions.

Impacts

Primary:

  • Death and injury – Some 15,894 people died, and 26,152 people were injured. 130,927 people were displaced, and 2,562 remain missing.
  • Damage – 332,395 buildings, 2,126 roads, 56 bridges and 26 railways were destroyed or damaged. 300 hospitals were damaged, and 11 were destroyed.
  • Blackouts – Over 4.4 million households were left without electricity in North-East Japan.
  • Transport – Japan’s transport network suffered huge disruptions.
  • Liquefaction occurred in many of the parts of Tokyo built on reclaimed land. 1,046 buildings were damaged.

Secondary:

  • Economy – The earthquake was the most expensive natural disaster in history, with an economic cost of US$235 billion.
  • Tsunami – Waves up to 40 m in high devastated entire coastal areas and resulted in the loss of thousands of lives. This caused a lot of damage and pollution up to 6 miles inland.
  • Nuclear power – Seven reactors at the Fukushima nuclear power station experienced a meltdown. Levels of radiation were over eight times the normal levels.
  • Transport – Rural areas remained isolated for a long time because the tsunami destroyed major roads and local trains and buses. Sections of the Tohoku Expressway were damaged. Railway lines were damaged, and some trains were derailed.

Response

Short term:

  • The Japan Meteorological Agency issued tsunami warnings three minutes after the earthquake.
  • Rescue workers and around 100,000 members of the Japan Self-Defence Force were dispatched to help with search and rescue operations within hours of the tsunami hitting the coast.
  • The government declared a 20 km evacuation zone around the Fukushima nuclear power plant.
  • Japan received international help from the US military, and search and rescue teams were sent from New Zealand, India, South Korea, China, and Australia.
  • Hundreds of thousands of people who had lost their homes were evacuated to temporary shelters in schools and other public buildings or relocated to other areas.

Long term:

  • Incentives to attract investment, both in terms of business and reconstruction, into the Tohoku region.
  • The central government decided on a coastal protection policy, such as seawalls and breakwaters
  • The March 11th earthquake wiped 5–10% off the value of Japanese stock markets. The priority for Japan’s long-term response is to rebuild the infrastructure in the affected regions and restore and improve the economy’s health as a whole.
  • As of November 2011, 96% of the electricity supply had been restored, 98% of the water supply and 99% of the landline network.
45
Q

**

What is a tropical storm?

A

A tropical storm is a low pressure weather system with high winds and torrential rain.

46
Q

What is the Coriolis effect?

A

Because the Earth rotates on its axis, circulating air is deflected toward the right in the Northern Hemisphere and toward the left in the Southern Hemisphere.

47
Q

How do hurricanes form?

A
  1. Warm, moist air rises, leaving an area of low pressure below. This causes warm air from surrounding areas of higher pressure to move into this low pressure area and rise too. Overall, warm air is constantly rising and accumulating in the atmosphere.
  2. When the warm air rises, it cools, condensing into thunderstorm clouds.
  3. The whole system is spinning due to the Coriolis effect. In the southern hemisphere, the storms spin clockwise; in the northern, anticlockwise.
  4. The constant additions of energy from the warm air causes the storm to spin faster and generate higher wind speeds. At 39 mph the storm can be classed as a tropical storm.
  5. The eye of the storm is in the centre. This is an area spanning around 30 miles wide that is of extremely low pressure (can be 15% lower pressure than areas outside of the storm). Cool, dry air (cool from the higher altitudes and the moisture has been transferred into the system) descends in the eye, causing the weather to be relatively calm and cloud free. The more intense the storm, the clearer the eye.
  6. Surrounding the eye is the eyewall, the most intense and powerful area of the storm. Warm, moist air rapidly rises here, with extremely high winds and torrential rain. When winds reach 74 mph, it becomes a hurricane/cyclone/typhoon.
  7. When the tropical storm reaches a coast, the low pressure and high winds will cause a large amount of sea water to be taken into the system and then released as a high wave called a storm surge.
  8. When the storm reaches land, it no longer has a supply of energy (warm, moist air from the sea) and the eye eventually collapses. Heavy rain can persist for days.
48
Q

How is the magnitude of tropical storms measured?

A

Measured on the Saffir-Simpson Scale (A scale of 1-5) based on wind speed and thus power of the storm.

Diagram

49
Q

What hazards are caused by tropical storms?

A

High winds - over 300km/h and therefore very strong. Hurricane winds are strong enough to blow a house down, and also blow heavy debris at high speeds, which can obviously cause damage and injure anyone who comes into contact.
Flooding - coastal/river flooding from storm surges and heavy rain.
Landslides - due to soil becoming heavy when wet with high levels of rain
Storm surges - Large rise in sea levels caused by low pressure and high winds, pushing water towards the coast

50
Q

At what point in the year are tropical storms frequent?

A

Tropical storms form in the Northern Hemisphere from June-November, and the Southern Hemisphere from November-April

51
Q

CASE STUDY
Hurricane Katrina 2005

A

General
Hurricane Katrina is the costliest natural disaster in the history of the United States. New Orleans has always been vulnerable to flooding as it sits by Lake Pontchartrain and the Mississippi river. The wetlands of the Mississippi delta that used to protect New Orleans have diminished in size because they have been drained and because they are starved of sediment as the Mississippi river is so heavily embanked against flooding it stops erosion upstream which prevents deposition downstream. New Orleans is also sinking because the drained soft sediments it is built upon has compacted under the weight of the buildings. The levees, both earthen and flood walls, were only ever designed to cope with a category 3 storm, not enough to cope with the strength of the storm surge of Katrina, a category 5 storm.

Causes
Hurricane Katrina began as a very low pressure weather system, which strengthened to become a tropical storm and eventually a hurricane as it moved west and neared the Florida coast on the evening of 25 August 2005. After crossing southern Florida - where it left some 100,000 homes without power - it strengthened further before veering inland towards Louisiana, eventually making landfall at Grand Isle, approximately 90km south of New Orleans, at 10am local time on 29 August.

Impacts

Primary:

  • Social - More than 1,800 deaths in the state of Louisiana, Mississippi and Florida. And thousands of homes and businesses were destroyed.
  • Environmental - The strongest winds were over the coastal areas of Louisiana and Florida. Although the wind did not directly kill many people it was responsible for the storm surge which led to the floods.
  • Economical -. Thousands of jobs lost and millions of dollars in lost tax incomes.

Secondary:

  • Social - Estimated 1.2 million people evacuated the New Orleans region. And flooding delayed rescue efforts and aid for days.
  • Environmental - The storm surge pushed water levels up around the city. The levees were overwhelmed by the extra water and many collapsed. With 80% of the city being flooded to depths of six meters.
  • Economical - Katrina is the costliest hurricane with estimated damage of over $81 billion and costs of over $160 billion.
  • Political - The government was criticized for its mismanagement and lack of preparation in the relief efforts in response to hurricane katrina. President Bush only signed a relief package and ordered 7,200 troops to assist 10 days after the hurricane first struck New Orleans, this left many without help for over a week.

Response

Short term:

  • 5.6 million meals were served with 178 feeding units mobilised
  • Salvation Army raised nearly $400 million
  • More than 50,000 National Guard Troops were called to duty from various states
  • 1.7 million people were evacuated before the storm struck
  • Louisiana’s National Guard asked for more than 700 buses to evacuate people however only a 100 were sent
  • More than 35,000 people were rescued by the coastguard in New Orleans

Long term:

  • US Congress allocated $62 billion to be spent in aid helping feed and re-house survivors
  • $20 billion spent rebuilding New Orleans’ flood defence systems (220 miles of floodwalls and levees)
  • Waters that flooded New Orleans were pumped into Lake Pontchartrain (took over a month)
  • Relief on electric rates for over 30,000 people affected by the hurricane
  • All oil, gas, and energy facilities that were damaged have been restored or rebuilt
  • Public hurricane related broadcasting stations have been improved
52
Q

What is a wildfire?

A

Uncontrolled fires that occur in natural areas such as forests and grasslands

53
Q

What are the conditions that favour wildfires?

A
  1. Fuel in the form of dry vegetation - some plants like Eucalyptus contain volatile oils that promote fire. Forests fires can be worse than grassland
  2. Ignition source (natural and human) - quasi-natural hazard
  3. Favourable climatic conditions - heatwaves, droughts, el nino (warm phase), areas with dry seasons
54
Q

What is a quasi-natural hazard?

A

Quasi-natural hazard refers to those hazards that occur due to the interaction between the activities done by the humans and the various types of natural processes that take places on the surface of the earth

55
Q

What factors affect the behaviour of a wildfire?

A
  • Fuel (dry vegetation)
  • Ignition source
  • Climatic conditions
  • Topography
  • Wind speed/direction
56
Q

How can wildfires be beneficial?

A

They can disperse seed, remove dead or decaying matter, harmful insects and diseased plants. Some species of plants require fire for seed germination such as Douglas fir

57
Q

How do wildfires spread?

A

Processes like convection heat up the vegetation ahead of the flames, preparing them for ignition and enable the fire to spread fast.
These processes hear the material above the fire most effectively causing a vertical advance on the fire front. Because of this they tent to advance more rapdily up slope than on level ground. 20 degress = 4x faster.
Firebrands (burning fragments of vegetation can be carries ahead of the fire by convection currents and strong winds igniting isolated spot fires. This makes them random and therefore a significant hazard. Firebrands can also roll downhill because of gravity and start fires there.

58
Q

What are the causes of wildfires?

A
  • Natural causes e.g. lightning strikes (the biggest cause), volcanoes or spontaneous
  • Human causes e.g. lit cigarettes, barbeques, agriculture, train lines
59
Q

What are the three types of wildfires?

A
  1. Surface
  2. Ground
  3. Crown
60
Q

Describe surface fires

A

Surface fires burn only the surface litter and duff. They are the easiest fires to put out and cause the least amount of damage to the forests.

61
Q

Describe ground fires

A

Ground fires burn very slowly beneath the ground in layers of dry organic peat and humus. Difficult to fully put out. They have been known to smoulder all winter underground and then emerge at the surface again in Spring.

62
Q

Describe crown fires

A

Crown fires burn the entire tree from bottom to top , which is classed as the most dangerous, intense and destructive type of fire as they spread through the canopy and affect forests

63
Q

What is the ladder effect?

A

The ladder effect describes the process of fires from the forest floor spreading to the tree canopy

64
Q

How can people be prepared for a wildfire?

A

People can be prepared by having evacuation plans, emergency services training and drills, and a
personal emergency plan (with food supplies, water, a place to stay etc.)

Warning systems are also a good way for people to be
prepared. Broadcasted weather warnings (or ‘Red Flag
Warnings’ as they are commonly referred to as) warn people when the perfect conditions for wildfires are occurring - e.g. hot, dry, upcoming lightning storms. This means people may wish to evacuate and campfire bans can be put in place.
Thermal infrared satellite imagery shows where wildfires are occurring so that people can stay away from these areas. Therefore, evacuation zones can be set up for areas in high risk, and people can be evacuated

65
Q

CASE STUDY
New South Wales, Australia Wildfires

A

General
NSW has the highest population of any state in Australia, with 8,153,000 residents as of 30 June 2022. Nearly a third of all Australians live in NSW, with most living in the Greater Sydney region. More than 275 different languages are spoken and 144 religions are practiced in NSW. NSW has the largest labour force in Australia with almost 4.5 million people either employed or seeking employment. At almost 700 billion dollars, NSW is Australia’s largest state economy. The state has a diversified, service driven economy.

Causes
According to the Victorian Country Fire Authority (CFA) and the NSW RFS, the majority of the 2019–20 fires in Victoria and NSW were caused by lightning. Drought, soil moisture, wind speed, relative humidity, heat waves, fuel moisture, and certain land cover types all contributed to the fires

Impacts

Primary:

  • Burnt through 2.7 million hectares of land
  • Destroyed over 3,000 buildings (including 2,779 homes), and killed at least 34 people
  • Large areas of forest burnt out of control

Secondary:

  • Choking skies and terrible air quality afflicting Sydney
  • Bushfire smoke was responsible for more than 400 deaths
  • Economists estimated the bushfires – Australia’s costliest natural disaster in history – may have cost over A$78–88 billion in property damage and economic losses
  • Satellite data estimated the carbon emissions from the fires to be around 715 million tons, surpassing Australia’s normal annual bushfire and fossil fuel emissions by around 80%
  • Thousands of farms affected by significant losses of livestock, placing further strain on a sector already suffering wide-spread effects of drought.

Response

Short term:

  • Emergency services
  • Many countries have offered assistance, including firefighters, helicopters, troops and money.
  • The New South Wales Rural Fire Service is the lead agency for bush fires in New South Wales and formed the bulk of the primary response to the fires, mobilising thousands of firefighters and several hundred firefighting vehicles
  • Firefighters as of January 2020 managed to save over 16,000 structures from direct fire impact in addition to countless lives

Long term:

  • A wide range of disaster assistance payments and allowances were made available through joint Commonwealth-State arrangements to assist individuals, primary producers, businesses, non-profit organisations and local governments that had been impacted by the bushfires
  • 6 January 2020 the Australian Government committed $2 billion to the National Bushfire Recovery Fund to provide further assistance to individuals and communities impacted by the fires, bringing total government assistance available to almost $2.65 billion
  • On 20 February 2020 the Royal Commission into National Natural Disaster Arrangements was established
66
Q

What is slab pull?

A
67
Q

What is ridge push?

A