Tropical storms Flashcards
What is the basis for storms forming?
Develop over warm water. As warm, moist air rises and condenses, it releases energy that increases wind speed.
What conditions do tropical storms need?
- Disturbance near the sea-surface that triggers storm (area of low pressure)
- Warm sea water (27degrees + 50m below surface) - evaporation
- Convergence of air in lower atmos. - within ITCZ or along boundary between warm and cold masses - air rises
- At least 5 degrees from Equator - don’t form either side because Coriolis force is not strong enough
What is the Coriolis effect?
Force caused by earths rotation. Deflects the path of winds but is weak near the equator.
What are the characteristics of tropical storms?
AKA cyclones, hurricanes and typhoons. Can extent to 500km in diameter and cause extensive damage and loss of life in many coastal regions on the tropics. Must have av. wind speeds over 75mph.
The eye wall, bank of cloud that rings the central eye, is the most powerful and damaging part. Cloud and rain extend in a series of waves that extend beyond the eye wall. Tornados form within storms
Highly localised = difficult to predict and highly destructive.
What is the distribution of tropical storms?
Vast majority form in the tropics close to the Equator on either side.
They do extend to other places like China, Japan and eastern seaboard of USA.
What are the factors that can effect distribution?
- Oceans
- High temperatures
- Atmospheric instability
- Rotation of the earth
- Uniform wind directions at all levels
What happens as storms form?
- It develops a clear and distinct rotation.
- Warm moist air rises rapidly in its centre to be replaced by air drawn in at the surface.
- A central cortex develops as more and more air is drawn in and rises. The eye often characterised by column of dry sinking air.
- Air cools as it rises - condensation and towering cumulonimbus clouds form. Sometimes a no. of isolated storms will join to form 1 large one.
What happens when condensation forms in a storm?
Latent heat is released. This effectively powers the storm.
When do tropical storms begin to die down?
Continue to grow and dev. as they are driven by prevailing winds across ocean.
When it reaches land and supply of energy and moisture is cut off storms die down. Back over ocean - reinvigorated.
What are the storm hazards?
- High winds
- Coastal flooding
- Storm surges
- River flooding
- Landslides
Storm hazards: strong winds
Average wind speeds of 75 mph (120 km/h). Speeds of up to 250km/h have been recorded at the eye wall.
Capable of significant damage - tearing off roofs, breaking windows, uproot trees, carry debris and damage communication networks.
Debris form flying missiles, strewn on roads = transport disruption.
Damaged power lines - electricity cuts and occasionally fires.
Storm hazards: Storm surges
Surge of water 3m high inland flooding low-lying areas. Caused by intense low atmos. pressure of TS w/ powerful driving surface winds.
Major cause of widespread devastation and loss of life. Inundate agricultural land w/ saltwater and debris, pollute freshwater supplies and destroy housing and infrastructure. Enhanced coastal erosion = undermining of buildings and highways.
Storm hazards: Coastal and river flooding
Warm humid air can generate torrential rainfall, over 200mm in a few hrs. Flash flooding at the coast, urban areas where surface water overwhelms drainage. Urbanisation increases flood hazard.
As moves inland, weakens as moisture supply is cut off. Still may result in sig. flooding due to intensity and quantity of rain falling on river basin.
What is an example of flooding due to a tropical storm?
August 2011, Hurricane Irene caused widespread flooding throughout New Jersey resulting in evacuation of over 1 mil ppl and over $1 bil in damage.
Storm hazards: Landslides
Up to 90% of landslides a yr caused by heavy rainfall and many triggered by TS. Intense rainfall increases pore water pressure, weakens cohesion and triggers slope failure. Additional weight of water exacerbates problem.
Possible that load release caused by TS-induced landslides may trigger earthquakes in tectonically stressed regions.