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Hazard
potential threat to human life and property caused by an event
Only becomes a hazard when it is a threat to people
Geophysical hazard
caused by land processes
Normally tectonic
Atmospheric hazard
caused by atmospheric processes and the conditions created by
Eg weather systems causing wildfires
Hydrological hazard
caused by water bodies and movement eg floods
Hazard perception
people have different viewpoints of how dangerous hazards and what risks they pose
Dependent of lifestyle factors including economic and cultural elements Including:
Wealth
Experience
Education
Religion and beliefs
Mobility
Fatalism
viewpoint that hazards are uncontrollable and any losses should be accepted as there is nothing that can be done to stop them
Prediction
using scientific research and past events in order to know when a hazard will take place So that warnings may be delivered and impacts of the hazard can be reduced
Adaptation
Attempting to live with hazards by adjusting lifestyle choices so that vulnerability to the hazard is lessened
Mitigation
Strategies carried out to lessen the severity of a hazard
Management
Coordinated strategies to reduce a hazards effects
Includes prediction, adaptation, and mitigation
Risk sharing
form of community preparedness where they invest collectively to mitigate the impacts of future hazards
Incidence and human response
frequency of a hazard
Low incidence hazards are harder to predict and have less management strategies put in place
Low incidence usually more intense than high incidence hazards
Distribution and human response
where hazards occur geographically
Areas of high hazard distribution are likely to have a lot of management strategies
Those living there will be adapted to the hazardous landscape
Magnitude and human response
High magnitude/intensity hazards will have worse effects meaning they require more management
Level of development and human response
economic development will effect how a place can respond to a hazard
An area with lower development is less likely to have effective mitigation strategies therefore the effects of a hazard will be more catastrophic
The park model
graphical representation of human responses to hazards
Steepness shows how quickly an area deteriorates and recovers
Depth shows the scale of the disaster (lower curve=lower quality of life)
Works as a control line to compare hazards
Stage 1 of the park model - relief
hours-days
Immediate local response: medical aid, search and rescue
Immediate appeal for foreign aid
Stage 2 of the park model - rehabilitation
days - weeks
Services begin to be restored
Temporary shelters and hospitals set up
Food and water distributed
Coordinated foreign aid eg peacekeeping forces
Stage 3 of the park model
weeks - years
Restoring the area to same or better quality of lie
Area back to normal - ecosystem restored, crops regrown
Infrastructure rebuilt
Mitigation efforts for future event
Hazard management cycle
outlines the stages of responding to events
Preparedness - (EVENT) - response - recovery - mitigation
Evaluating the ffectiveness of models
can it be applied to every hazard?
Does it take into account aspects of hazards eg levels of development?
Is there a timeframe?
How does timeframe change?
Does it present hazards currently? Effect fo climate change?
Inner/outer core
inner: very hot due to pressure and radioactive decay. This heat is responsible for earths internal energy
Outer: semi molten
Mantle
mainly solid rocks
Very top later of the mantle is semi-molten magma, known as the asthenosphere
The lithosphere rests on top
Astenosphere
semi-molten layer constantly moves due to flows of heat called convection currents
Movements are powered by the heat from core
Lithosphere
broken up into plates
Majority of the lithosphere is within the mantle
Top of the lithosphere is the crust
Crust
thin top of the lithosphere
Oceanic crust is dense and destroyed by plate movement, continental crust is less dense and not destroyed
Hotspots
areas of volcanic activity that are not related to plate boundaries
Hot magma plumes from the mantle rise and burn through weaker parts of the crust
This can create volcanoes and islands
The plume stays in the same place but the plate continues to move, which sometimes causes a chain of islands eg Hawaii
Volcanic hazards
lava flows: speed depends on viscosity
Lahars (mudflows): usually caused by melting ice at high latitudes
Tephra: any type of rock that is ejected by a volcano
Toxic gases: released during some eruptions (even CO2can be toxic as it can replace oxygen as it is heavier)
Acid rain: caused when gases such as sulfur dioxide are released into the atmosphere
Pyroclastic flows/Nuees Ardentes: clouds of burning hot ash and gas that collapses down a volcano at high speeds. 60-430mph
Spacial distribution of volcanoes
along constructive or destructive boundaries or on hotspots
Ring of fire is an area of high volcanic and earthquake activity located in the pacific
Majority of volcanoes occur here
Primary effects of volcanoes
ecosystems damaged
Wildlife killed
Businesses and industry destroyed/disrupted
People killed
Homes destroyed
Secondary impacts of volcanic hazards
water acidified by acid rain
Volcanic gases contribute to greenhouse effect
Jobs lost
Potential profit from tourism industry
Fred may start
Mudflows or foods
Homelessness
Conflicts concerning government response, food shortages, or insurance
Prevention of volcanic hazards
cannot be prevented
Only risk to people can be prevented by not allowing people near active volcanoes
Preparedness of volcanic hazards
monitoring increases notice of volcanic eruptions, allowing for warnings
Education of volcanoes in areas of risk
Evacuation procedures planned
Training response teams
Mitigation of volcanic hazards
direct intervention eg concrete blocks to steer lava from areas of risk
Evacuation zones
Mitigating effects on health by having emergency aid and rescue
Adaptation to volcanic hazards
moving away from high risk areas
Capitalising on opportunities eg encouraging tourism
Seismic hazards
at all boundaries, plates can become stuck due to friction between plates
When plates are stuck, convection currents in the asthenosphere continue to push, building pressure
Eventually the plates give way and release pressure in a sudden movement, causing a jolting motion in the plates
This is responsible for seismic movement spreading through the ground in the form of seismic waves
The focus is the point underground where the earthquake originates from
Epicentre is the point directly above the focus on ground
Spacial distribution of earthquakes
occur along all boundaries
Ring of fire accounts for 90% of the worlds earthquakes
Hazards caused by seismic events
shockwaves: potential enegry transferred into kinetic energy and is released and vibrates throughout the ground. Strongest closest to the focus
Tsunamis
Liquefaction: 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
Landslides and avalanches: movement in soil or snow will cause it to become unstable
Primary impacts of seismic hazards
can cause fault lines which damage the environment
Liquefaction
Businesses destroyed
Buildings collapsing which threatens life
Secondary impacts of seismic hazards
radioactive material leaked from power plants
Saltwater from tsunamis flooding freshwater ecosystems
Soil salinisation
Economic decline
High cost of rebuilding and insurance payout
Gas pipe ruptures may cause fires
Water supplies contaminated spreading disease
Tsunamis causing flooding
Political unrest
Borrowing money for international aid
Prevention of seismic hazards
majority cannot be prevented
Liquefaction can be prevented though soil stabilisation
Avalanches can be prevented through controlled explosions
Preparedness of seismic hazards
extensive awareness strategies eg in Japan
Tsunami warnings following earthquake event
Evacuation plans and training
Mitigation of seismic events
search and rescue, immediate emergency aid, and evacuation
Demolishing older unsafe buildings
Tsunamis wave breaks and sea walls to prevent flooding
Adaptation to seismic hazards
moving away from areas of risk
Insuring homes and businesses
Building earthquake proof buildings
Tropical storm
low pressure spinning storm with high winds and torrential rain
Conditions needed for a tropical storm
ocean temperatures of 27 degrees and 50m deep
Area of unstable air pressure (eg where high and low pressure areas converge)
Wind needed for swirling motion
Around the equator not on due to coriolis effect
Formation of tropical storms
Over land: rapidly rising warm air forming thunderstorms. No shear wind to destroy the storm
Easterly winds move the storm. Sea surface temperature over 26 and 50m deep. Rising warm air fuels the storm
Storm moves away from the equator due to the coriolis effect and begins to spin anti clockwise. Rising warm air continues to enlarge the storm
Increased speed and energy makes the thunderstorm a tropical storm. Bands of cloud with rising warm air through the clouds and cooler air sinking between the bands. Storm rotates around the eye
Once the storm reaches land, the warm rising air is stoped, removing the fuel of the storm. The storm dissipates.
Spacial distribution of tropical storms
between 5 and 1 degrees latitude
Likely to form in the ITCZ where the two limbs of the hadley cell converge to form low pressure
Cyclones: Indian Ocean
Hurricanes: Atlantic Ocean
Typhoon: Pacific Ocean (most common)
Hazards caused by tropical storms
high winds over 300km/h
Flooding from storm surges and heavy rain
Landslides due to oil becoming more saturated
Primary impacts of storm hazards
beaches eroded and sand displaced
Coastal habitats eg coral reefs destroyed
Agricultural land damaged
Drowning
Debris carried by high winds
Building destroyed
Secondary impacts of storm hazards
river flooding/salt water contamination
Water sources changing course from blockages
Rebuilding costs
Economic decline
Homelessness
Polluted water supplies
Food shortages
Pressure for government to do more about global warming
Prevention of storm hazards
cannot be prevented
Strategies to mitigate climate change could prevent higher category storms
Preparedness of storm hazards
awareness though education
Evacuation plans and training
Satellite image tracking
Storm warning systems and television broadcasting
Mitigation of storm hazards
search and rescue, immediate emergency aid, evacuation
Strengthening buildings and homes
Clearing loose debris before storm
Adaptation to storm hazards
move away from high risk areas
Design buldings to withstand high winds and flood damage
Flood defences eg houses on stilts and sea walls
Wildfires
large, uncontrolled fire that spreads quickly through vegetation
Conditions favouring wildfires
densely packed vegetation allows fires to spread quickly and easily
Vegetation with flammable oils eg eucalyptus
Dry vegetation
Climates that have enough rainfall for sufficient plant growth but considerable dry spells and droughts eg California
Wind causes fire to spread quicker
Impact of temperature rise on incidence of wildfires
increases incidence and length of wildfire seasons
“Forest fires in the US occur 5x more since the 70s and 80s, burning 6x area of land, an lasting 5x longer”
Fire behaviour
spread quickly on hills are the heat rises
May jump across rivers and into areas due o lit debris which causes it to spread
Crown/surface/ground fires
crown: burn the entire tree from bottom to top. Most dangerous and destructive
Surface fires: only burn leaf litter making them easy to extinguish
Ground fires: burn dry peat or vegetation beneath the surface, and move slowly through the dried underground. Difficult to put out and can continue to burn throughout the year if weather conditions allow it
Causes of wildfires
can be natural or human
Normally caused by human activity (accidentally or by arson)
Natural causes include lightning and volcanoes
Human causes can be lit cigarettes, bbqs, agriculture and more
Primary impacts of wildfires
air pollution from ash
Water pollution
Habitats destroyed
Toxic gases
Agricultural land destroyed
Cost of firefighting
Deaths
Homes destroyed
Secondary impacts of wildfires
Migration patterns of animals effected
Increased CO2 release contributes to greenhouse effect
High cost of rebuilding
Discourages tourism
Cancelled air travel
Homeslessness
Food shortages
Health problems eg smoke inhalation causing asthma
Government pressure to tackle climate change
Prevention and preparedness of wildfire hazards
wildfire will not be eradicated entirely due to current climate
Public awareness can prevent ignition of wildfires and prepare people
Eg SMOKEY BEAR US mascot who provides information on preventing wildfires
Evacuation plans, emergency services training, personal emergency plans
Warning systems eg Rd flag warnings
Evacuation zones setup
Mitigation of wildfire hazards
mainly concerned with protecting those directly at risk and extinguishing the fire
Firefighters dispatched on ground
Water and flame retardants sprayed onto large areas using aircrafts
Long term mitigation strategies work to reduce impacts before they occur, eg controlled burning which remove flammable materials so less fuel is available
Fire breaks created to limit spread
People living at risk of wildfires can ensure their homes do not contribute to wildfire spread by following campaigns such as Smokey bear
Homes can be built using materials that do not release harmful substances when burnt
Adaptation of wildfire hazards
insurance and clean up of homes
Staying educated
Globally adaptations to lifestyle to stop contributions to atmospheric CO2 levels