Storm Hazards Flashcards
The nature of tropical storms
They are huge spinning storms with tropical winds and torrential rain.
They require warm water (27 degrees to a depth of at least 70 metres).
As warm, moist air rises, it releases energy that increases wind speed.
Conditions needed for tropical storms to form
A disturbance, such as an area of low pressure that triggers the storm
A convergence of air in the lower atmosphere - either within the inter-tropical convergence zone or along the boundary between warm and cool air masses. This forces warm air to rise.
How tropical storms form
They form in the tropics and move westwards due to easterly winds.
They occur at least 5 degrees from the equator.
They cannot form any closer because the coriolos effect isn’t strong enough to make them spin.
They also move away from the equator because of this
They lose strength as they move over land because their supply of warm, moist air is cut off.
The Coriolos effect
The rotation of the earth which deflects objects and air (to the right in the northern hemisphere) along the earths surface.
Latent heat
The energy that is the driver of tropical storms, while the presence of moisture allows low frictional drag with the surface of the ocean.
Circular storms
There is a low pressure point at the centre, called the eye.
In the eye wall there are rising air spirals that cause strong winds.
Near the top of the storm, there is an outflow of moisture - laden air so cloud cover extends for a long distance either side of the eye.
Measuring storms
Storm magnitude is measured in the Saffir-Simpson scale.
It measures wind speed from 1 (weakest winds of 120-150kmh) to 5 (strongest winds of over 250kmh)
It also measures damage done from 1 (limited) to 5 (catastrophic)
Frequency
Tropical storms are quite frequent with around 100 occurring each year.
Some never reach land so don’t develop into hazards.
Predictability
Storms are more frequent in the Northern hemisphere between June and November, and the Southern Hemisphere between November and April.
They can be predicted using satellite imagery to identify cloud formations.
The storm can then be predicted using satellite imagery and models, helping scientists to work out when it will hit.
Predictions are usually accurate however storms are largely irregular due to the number of factors affecting when one will form.
Winds
Wind speeds on the ground can reach more than 300km/h.
They can destroy buildings, uproot trees and carry debris long distances before smashing them into other objects.
Storm surges
A large rise in sea level caused by high winds pushing water towards the coast, and by the low pressure of the storm.
They account for around 90% of tropical storm deaths.
Waves can reach 10m high if a surge coincides with high tide, devastating coastal communities by destroying buildings, roads and contaminating agricultural land with salt from sea water.
Heavy rain
Warm moist air rises, cools, condenses and then falls as torrential rain. This can lead to secondary hazards such as flooding and landslides. During tropical storms, there tends to be around 100mm of rainfall a day.
E.g. Storm Denise 1966, over 1000mm of rain fell in 12 hours
Standing water + warm temperatures = breeding ground for mosquitos, leading to malaria.
Flooding
Heavy down pours cause river discharge to increase suddenly, causing rivers to overtop their banks and flood the surrounding area.
Heaving rain and storm surges can also cause flooding in coastal areas.
Landslides
Water infiltrates soil and rock, adding weight and making it less stable, increasing the risk of landslides.
Social impacts
People may drown, be injured or killed by debris that’s blown around or carried by water.
People left homeless
Electricity cables damaged, so supplies are cut off
Flooding = sewage overflow = contaminated water = disease
Food shortages due to damage to agricultural land