Storm hazards Flashcards
What is a tropical storm?
Tropical storms are intense low pressure systems (below 950mb)
What are the different names of storms?
Cyclones - Indian oceand and the South Pacific
Hurricanes - North Alantic
Typhoons - Western Pacific and South East Asia
Where do tropicla storms form?
- Form over tropical waters between the tropics of cancer and the capricorn but not directly over the equator (5-20 degrees N and S)
- Sea temperatures of 26.5 degrees
- Typically occur between the months of June to November in northen hemisphere and november to april in southern hemisphere
- Natural events excabertaed by climate change
- Key purpose is to redistribute heat from tropics towards the poles and without them global climate change would be very different
- On average kil around 10,000 people a year mostly in coastal areas
What are the characteristics of tropical storms?
- Revolving
- 500km in diameter on average and can cause extensive damage and loss of life
- Must exceed average wind speeds of 120km p/h
- Contains a central eye wind speed reduced here
- Most powerful part of the storm is the eye wall with strong winds
- Clouds and tall and wide cumlonimbus
- Rising moist air above oceans combine with cooling dry air from stratosphere
- Torndaedoes may occur within tropical storm
- High rainfall
- Lasts 7-14 days on average
- Path known as track
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What is the spatial distribution?
- Vast majority in the tropics e.g. china,Japan, eastern seaboard of USA
Factors that affect the spatial distribution?
Oceans
Ocean temperatures
Atmospheric instability
Corolis effect
wind shear at high altitudes
Ocean temperatures
- A sea surface temp in excess of 26 degrees is required for tropical storm formation
- Formed in low altitudes during summer when temps arent at their highest
- Provide energy to the storm through high rates of evaporation and condensation
Atmosphereic instability
- Tropical storms most likley to form here where warm air is being forced to rise
- The ITCZ where two limbs of the hadley cell converge to form low pressure on the ground perfect for tropical storms
Coriolis effect
- The rotation of the air causes the air to move around the centre of the eye in cicurlar or rotating motion
- This increases with distance away from equator - n-s 5-20 degrees
Wind shear
- Winds from diff altitudes prevent tropical storm from attaining heigh and intensity - vertical development ‘sheared off; by multi directional winds
The formation of Tropical storms
- Warm moist air rises to be replaced by air drawn in at the surface
- Central vortex as more air is drawn in and rises
- Very centre of the storm (eye) characterised by a column of dry,sinking air
- As air rises rapidly cools condensation and formation of towering cumulonimbus clouds
- Sometimes no of isolated thunderstorms will coalese to form a single giant storm
- Latent heat during condensation powers the storm
- Continues to grow +develop as driven by prevailing winda across oceans when reaches land - supply of energy and water is cut off strom decays and moves back over oceans it reinvigorates
What hazards are associated with tropical storms?
Strong winds
Storm surges
Coastal and river flooding
Landslides
Strong winds
- Average wind speeds in excesss of 120km p/h (75mph) gusts over 25km p/h in the eye wall
- Strong winds are capable of causing significant damage and disrutpion - teraing off roofs, breaking windows, damaging communication networks
- Debris form flying missiles whisked up by the wind
- Widespread electricity cuts (power outrages) - fires
- Debris over roads can cause major transport disruptions
Storm surges
- Surge of high water, typically about 3m in heigh sweep inlanf from sea flooding low lying areas
- Caused by the intense low atmosphereic presssure of the storm (enables sea level to rise vertically) together with powerful driving surface winds
- Storm surges account for 90% of tropical storm deaths
- 1mb drop in air pressure = 1cm rise in water levels
- Inundate agricultural land with saltwater and debris, pollute freshwater supplies and destroy housing and infrastructure
- Contaminated flooding - chlorea
- Enhanced coastal erosion - undermiing buildings and highways
- Looting of shops
- Silting
- Salinisation
- Storm tide
Coastal and river flooding
- Warms humid air generates torrential rainfall often in excess of 200mm in a few hours - triggers flash flooding at the coast (in urban areas where surface water can overwhelm the drainage system
- Urbanisation (drains, high density of buildings) exacerbates the flood hazard by encouraging rapid overland flow and causing flash flooding
- As ts moves inland gradually weakens as moisture and energy supply is cut off may still have significant river flooding due to intensity and sheer quantity of rain on the river basin
Landslides
- 90% each year caused by heavy rainfall - triggered by tropical storms
- Intense rainfall increases pore water pressure (hydrostic pressure within a slope) which weakens coheison and triggers slope failturw
- Additional weight of water exacerbates problem - 1998 hurricane
- Load release caused by tropical storm induced landslides may tigger eqs in tectonically stressed regions