9.3 Hazards resulting from atmospheric distrubances Flashcards

1
Q

define risk and vulnerability - differences

A

risk: probability hazard event causing harmful consequences

vulnerability: susceptibility to a hazard

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2
Q

factors determining risk

A

location
wealth
time
type of hazard

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3
Q

factors determining risk perception

A
  • the subjective judgement that people make about the characteristics and severity of a risk
  • Experience: make you more or less
  • material well being
  • personality
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4
Q

similarities and differences between hurricanes and tornadoes

A

Similarities:
- strong winds
- high energy environment
- rotating motion
- eye
- cause damage

Differences:
- wind speed (strongest tornado has stronger winds than hurricane, but generally hurricanes stronger)
- hurricanes have a greater diameter (size)
- hurricanes form above water
- easier to predict/track a hurricane
- other hazards associated with hurricanes (storm surge)
- location: hurricanes only in tropical/subtropical areas but tornadoes can form anywhere
- tornado local/short lived; cyclones longer duration
- tornado touches ground, hurricanes remain in atmosphere

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5
Q

global distribution of hurricanes and tornadoes

A

hurricanes:
- around equator largely with category 5 concentrated on south east coast of Asia: western pacific most intense
- tropical region not equator itself: 5-30 degrees above/below
- more in northern hemisphere than southern

tornadoes:
- mainly north America but can occur anywhere
- everywhere but Antarctica

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6
Q

area most at risk from hurricanes

A
  • south east Asia:
  • high population density
  • wealth inequality: informal settlements won’t withstand strong winds
  • rely on aid to recover
  • frequency of hazards high
  • islands: hard to be evacuated/receive help
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7
Q

formation of a hurricane

A
  • warm sea surface heats air above it which causes it to rise (forming low pressure) and then cools/condenses to form rain - much more rain due to quick rising air by warm sea surface
  • as water changes state, latent heat transfer fuels rising of air even more
  • low pressure can lift up the water
  • as air rises, more air rushes in to replace the air that rises upwards - generating strong winds
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8
Q

conditions needed for a tropical storm to form

A
  • cluster of thunderstorms over warm ocean
  • high levels of moisture
  • low wind shear: winds are at same speeds/low hurricane can form
  • 26.5 degrees
  • strong winds - 74mph
  • unstable air pressure: high levels of moisture, usually where areas of high/low pressure meet (convergence)
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9
Q

when do tropical storms form

A
  • between may and november in northern hemisphere and november and may in southern hemisphere
  • as when the noonday sun is high and so long period of intense heating to warm sea temps
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10
Q

where do tropical storms form according to latitude

A
  • 5to 30 degrees north and south as do not form nearer the equator because coriolis effect needed to deflect the converging rising air into a spin and effect of earths rotation not strong enough near equator
  • in higher latitudes sea not warm enough for their formation and there are no strong upper atmosphere winds in these latitudes so air can rise to tropopause
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11
Q

importance of latent heat in the formation of hurricanes

A
  • as rising air cools to below dew point, condensation releases latent heat
  • this causes the air to rise even faster, low pressure to lower even more and the moisture-laden wind to rush into the low pressure centre even faster
  • lower the pressure, the more air is drawn into it and greater its power
  • very heavy rain falls from thick cumulonimbus clouds produced by the uplift
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12
Q

conditions of the eye wall

A
  • very dense circular band of cumulonimbus cloud
  • most powerful winds and deepest convection with towering rain clouds that above the rest of the cyclone due to vast amounts of latent heat released from them
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13
Q

factors that affect the impacts of hurricanes

A

population density
politics
warnings
level development
size/category/nature of the storm
risk perception
track of the storm
frequency of the hazard

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14
Q

how does frequency of hazard affect the impacts of hurricanes

A
  • higher frequency = less time to recover and so put in reinforcements if very close together
  • e.g Katrina first of three high category storms to hit central Gulf in quick succession
  • although higher frequency = more aware of severity/know what to expect and so likely to have more plans in place
  • e.g hurricane sandy was the 18th named storm to hit USA that season
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15
Q

how does track of the storm affect impacts of hurricanes

A
  • impact on warning:
  • e.g path of Hurricane sandy affected by unusual atmospheric condition and moved west instead of east and hit New York
  • only 2 day forecast
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16
Q

how does risk perception affect impacts of hurricanes

A
  • lower levels of wealth likely to be more afraid as whole livelihood ; higher levels of wealth who have secure infrastructure/able to evacuate/insurance less worried
  • links to frequency: more frequent may be more aware of severity but also then may choose to stay if previous experience bad when leaving
17
Q

how does size/category/nature affect impacts of hurricanes

A
  • physical factors that aren’t affected bu development e.g location/size:
  • harder to evacuate/receive aid if an island`
  • storm surge very difficult to protect against = high damage: e.g hurricane katrina: 80% of New Orleans below sea level/only protected by levees which could not withstand surge causing 8m deep flooding
  • larger size = more areas affected e.g Hurricane Sandy 1800km in diamter despite only category 2
18
Q

how does level of development affect impacts of hurricanes

A
  • lower=higher population density/more likely to live by coast (more exposed), more primary industry and so reliant on agriculture - loss of land - detrimental impact economically: e.g 70% of Honduras economic output lost and took longer to recover as mainly primary compared to New York*
  • more developed = stronger/better infrastructure to withstand storm, but may result in higher cost of damage if unable to withstand storm
  • less developed: less knowledge on how to prepare/communicate with authorities
19
Q

how do warnings affect impacts of hurricanes

A
  • higher wealth = higher level of tech to predict/communicate with people: higher education = understand whats happening/know what to do
  • length of warning = more time to prepare/evacuate: 2 day forecast in New York for Hurricane sandy not long enough
  • errors made in warnings e.g hurricane sandy: no warnings in New Jersey so not aware of severity as not expected to hit
  • if certain hazards not expected then not prepared in correct way, e.g constant rain in Hurricane Mitch unexpected: most damage caused by floods and mudslides
20
Q

how does politics affect impacts of hurricanes

A
  • dictatorships may prevent aid from being received or even warnings: e.gBurmese people received no warning of hurricane
  • limit successes of aid e.g Cyclone Nargis, military junta prevented aid arriving: lack of response cost 1 million lives
  • in contrast hurricane sandy: Obama signed emergency declarations for states expected to be impacted by Sandy allowing them to request federal aid/prepare.
21
Q

How does population density affect impacts of hurricanes?

A
  • urban vs rural, more populated = more impacted in one area: e.g Hurricane Mitch large areas of informal housing hit as often on marginal land - prone to landslides