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hazards - Coggle Diagram
hazards
wildfires
nature
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surface fires sweep over the ground - consumes plant litter, trees and grass
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nature of the fire depends on:
- types of plants
- topography of the area
- strength of winds
- behaviour of the fire itself
once vegetation has dried out, the fire depends largely on the wind
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causes
ignition source
with natural fires, lightning is the most common source of the fire
most often, they are a result of human intervention - especially in areas of human settlement
usually started by discarded cigarettes, falling power lines, children playing with matches, campfires or controlled burning (agricultural)
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danger of fires have increased in areas of the us and australia as a result of allowing tourists in wild areas
fuel
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dry climates can increase the frequency of fires - during droughts, vegetation has the opportunity to accumulate and dry out
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3 ideal conditions
fuel
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combustable materials - vegetation (trees, shrubs, grass etc.)
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heat/ignition source
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these include lightning, cigarettes, matches, campfires etc.
impacts
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environmental
loss of crops, timber and livestock
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secondary impacts
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increased flood risk
loss of vegetation leads to less interception - when it rains there will be an increase in overland flow and therefore flooding
responses
preparedness
modelling - studying computer simulations of fire behaviour to prepare for any fire fighting methods
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education - make people in at risk areas aware of the impacts of wildfires and what to do in the situation
warning systems
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tourist areas should have warning signs and notice boards making people aware that they are in an at risk area
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being well insured - especially in wealthier countries, property such as housing is insured against fire damage to lessen economic impacts
mitigation
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managing built environment - increasing the gap between houses and vegetation so the fire cannot jump as easily
using more fire resistant materials - e.g. stone and brick rather than wood, spark arrestors on chimneys (device that prevents emission of flammable debris)
case study - victoria wildfire, australia (February 2009)
nature
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40°c heatwave in the months leading up to the bushfires - provided dry fuel (vegetation) which lead to widespread fires
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impacts
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3,500 properties lost - 2,000 homes and 1,500 farm buildings
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loss of livestock (12,000 head including cattle and sheep)
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over 60,000 residents had electrical disruptions
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seismic hazards
nature
when pressure is released after a build up of stress in the rocks, parts of the surface experiences an intense shaking - this is an earthquake
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vast majority occur along plate margins - the most severe associated with destructive (convergent) margins
at conservative plate margins, the boundary is shown in a fault line - e.g. san andreas fault, california
others that do not occur along plate margin boundaries are associated w/ the reactivation of old fault lines
magnitude and frequency
magnitude measured on the richter scale, however it is more usual for earthquakes to be measured on the moment magnitude scale (mms) which identifies energy release
seismic records allow earthquakes to be observed and can provide support for management of future events in specific areas
impacts
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secondary
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tsunamis - giant sea waves generated by the uplift of the seabed (shallow focus underwater earthquakes)
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responses
short term
aid - providing medical centres, food and water, accessible sanitation, temporary shelter
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long term
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improving building regulations - possibly inputting earthquake proof buildings (swaying, steel frames, shock absorbers etc.)
restoring utilities - i.e. water, sanitation, electricity, gas
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reducing impacts
prediction
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attempts to predict events through monitoring groundwater levels, unusual animal behaviour and release of radon gas
fault lines monitored
sometimes can predict where the next earthquake may occur - existence of a 'seismic gap' along the san andreas fault
protection
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in the usa, FEMA programme set to meet certain aims:
- promote understanding of earthquakes and effects
- to better identify earthquake risk
- to improve building design and construction techniques
- encourage use of earthquake-safe policies and planning practices
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storm hazards
nature
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is a tropical depression if it reaches 38mph (or less) - therefore becomes a tropical storm if wind speed reaches 39-73mph
conditions
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ocean depth of 70km - moisture provides latent heat (rising air causes moisture to be released by condensation which drives the whole system
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formation
- usually occur 5° and 20° north/south of the equator, where the temps reach over 27°c, and where the sea is 70km deep - where the convergence of air occurs at a low level
- the warm air rises and then cools, forming clouds, resulting in low pressure which draws in the hot water up to form the body of the storm
- the storm begins to spin due to the coriolis effect - the high pressure air near the top of the storm travels in towards the eye, however because the earth turns on its axis, the air is deflected from the centre of the storm
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- the weather system generates heat, which further powers the storm and allows it to sustain itself
- the storm usually dies out when it reaches land due to lack of moisture
characteristics
distribution
occur between 5° and 20° north/south of the equator (this is because coriolis effect cannot take place at the equator)
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hurricanes - caribbean sea/gulf of mexico (11%),, western side of central america (17%)
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magnitude
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once reaching land, storm starts to weaken - as there is no longer moist air to draw upon
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impacts
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major impacts caused by winds, heavy rainfall and storm surges
winds:
- strong winds (150-250km/h) can cause structural damage to buildings
- roads and bridges can collapse
- bring down electricity lines
- damage agricultural areas
- debris is thrown around and pose threat to people's lives
heavy rainfall:
- can exceed 200-300mm and can cause excessive flooding
- can cause landslides and mudflows
- high relief near coastal area can cause rainfall to increase to 500mm/day
storm surges:
- rise in sea level as a result of tropical storms
- wind-driven waves pile up and ocean heaves upwards as a result of the low atmospheric pressure
- can have a devastating effect on low-lying coastal areas,, especially in river deltas where flooding can reach far inland
- storm surges is the main cause of death in such events
- can cause severe long-term damage to agricultural areas (soil contaminated by the sea water)
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secondary effects
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road and rail networks blocked by debris - aid takes longer/cannot reach the people who need it the most
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