Hazards (Storm Events) Flashcards

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1
Q

Distribution of tropical storms

A

Tropical maritime areas between 5-20 N/S but not on the equator.

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2
Q

Distribution of hurricanes

A

N Atlantic (11% of storms) and NE Pacific (17% of storms)

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3
Q

Distribution of cyclones

A

S Pacific/Indian (8% of storms). Off of Madagascar (11% of storms)

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4
Q

Distribution of typhoons

A

NW Pacific (33% of storms)

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5
Q

Distribution of willy willies

A

NW and NE of Australia (20% of storms)

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6
Q

Conditions needed to form a tropical storm

A
  • Ocean above 27C
  • Water levels at 70m below surface
  • At least 5-20 N/S of Equator for Coriolis effect
  • Low level convergence
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7
Q

Why do storms decay upon reaching land?

A
  • Lose the source of heat and moisture

- Increased frictional drag decreases speed of storm

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8
Q

Four stages of tropical storm formation

A
  • Tropical Disturbance: <23 mph
  • Tropical Depression: 23-39 mph
  • Tropical Storm: 39-73 mph
  • Hurricane: 74 mph +
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9
Q

Scale used to measure tropical storm magnitude

A

Saffir Simpson Scale

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10
Q

Four factors measured by the SS scale

A
  • Central pressure
  • Wind speed
  • Storm surges
  • Damage potential
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11
Q

Frequency of tropical storms

A
  • N Hemisphere: June-November
  • S Hemisphere: November-April
  • Frequent but few major hazards
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12
Q

Regularity of tropical storms

A

Irregular- Occur in some areas but no clear pattern

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13
Q

Predictability of tropical storms

A

Fairly predictable with satellite tracking of cloud formations.

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14
Q

Primary hazards of tropical storms

A
  • Strong winds
  • Heavy rainfall
  • Storm surges
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15
Q

Secondary hazards

A
  • Flooding

- Landslides

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16
Q

Formation process of tropical storms

A
  • Solar radiation heats the ocean to 27C. ITCZ is usually overhead
  • Warm air rises and creates an area of low pressure
  • This air cools as it rises and condenses. Forms cumulonimbus clouds and heavy rainfall
  • Coriolis effect causes the air to spin upwards around a central eye
  • Air rushes in from high pressure areas, replacing rising air and creating strong winds
  • Cold air sinks in the eye of the storm
  • Carried across the ocean by prevailing winds, building with evaporated water
  • When it meets land it’s no longer powered by moisture and slows from friction with the land.
17
Q

Storm surges

A

Rising air creates low barometric pressure, and therefore an area of localised sea level rise. Winds create larger onshore waves and push a surge of water inland.

18
Q

Factors increasing severity of storm surges

A
  • Low relief of coastal areas
  • Funnelled coasts
  • Storm track
  • Intensity of storm
  • High tide
19
Q

Short term responses to storms

A

Search & Rescue. Evacuation.

20
Q

Long term responses to storms

A

Mitigating the impacts of future storms. E.g. prevention, protection, prediction and preparedness

21
Q

Methods of prediction for storms

A
  • Geostationary satellites
  • Land and Sea based monitoring (NOAA)
  • Aircraft reconnaissance
22
Q

Method of prevention of storms

A

Cloud seeding

23
Q

Methods of protection for storms

A
  • Strengthening homes e.g. barricades
  • Cyclone/hurricane drills
  • Land use planning to reduce access to high risk areas
  • Sea walls and flood defences to reduce storm surge risk
  • Emergency service drills
  • Insurance