Hazards: Storm Hazards Flashcards
What is a tropical storm?
is a low pressure, spinning storm with high winds and torrential rain.
Why is temperature a cause for a tropical storm to develop?
Ocean temperatures must be around at least 26 - 27°C and at least 50 metres deep. Warm water provides the storm with energy
Why is air pressure a cause of a tropical storm?
Must be in areas of unstable air pressure - usually where areas of high pressure and low pressure meet (convergence) - so that warm air rises more readily and clouds can form (this air must also be humid for cloud formation). Warm air rises because it is less dense than cold air.
Why is wind shear a cause of tropical storms?
Winds must be present for the swirling motion to form, but not too strong or the storm system will be ripped apart in the early stages.
Why is rotation a cause of tropical storms?
Tropical storms only form around the equator, but no less than 5° on either side. The Coriolis Effect is the effect of the Earth’s rotation on weather events. The storm spins because the Earth is spinning; but there is no Coriolis Effect at the equator, hence why these storms will only form a certain distance away from it.
Why can a trigger also be a cause of a tropical storm?
a pre-existing thunderstorm, a spot of very high sea surface temperature, an area of low pressure and many other factors can act as a trigger for a storm to develop, which will only further develop when the other conditions are present
What’s the development of a tropical storm?
- Warm, moist air rises, leaving an area of low pressure below. This causes warm air from surrounding areas of higher pressure to move into this low pressure area and rise too. Overall, warm air is constantly rising and accumulating in the atmosphere.
- warm air rises, cools, and condenses into thunderstorm clouds and heavy rain, releasing latent heat to further drive uplift and the storm
- The whole system is spinning due to the Coriolis effect. In southern hemi, storms spin clockwise; northern, anticlockwise.
- constant additions of energy from the warm air causes storm to spin faster and generate higher wind speeds. At 39mph the storm can be classed a tropical storm.
How does the tropical storm then mature?
- swirling winds create a central eye (diameter of 30-50km) - an area of subsiding air, light winds, clear skies and high temps. The more intense the storm, the clearer the eye.
- this descending air increases instability by warming as falls.
- Surrounding the eye is the eyewall, the most intense and powerful area of the storm. Warm, moist air rapidly rises here, with extremely high winds and torrential rain. When winds reach 74 mph, it becomes a hurricane/cyclone/typhoon.
- wind speeds of 100-150mph are not uncommon
What happens when a storm reaches the coast?
- the low pressure and high winds will cause a large amount of sea water taken into the system and then released as a high wave called a storm surge.
- When the storm reaches land, it no longer has a supply of energy (warm, moist air from the sea) and the eye eventually collapses. Heavy rain can persist for days.
- increased frictional drag also slows the storm
- continued movement away from the tropics over the sea bring contact with cooler waters, meaning less energy and a reduction in pressure differences
What is the average life span of a tropical storm?
7-14 days
What is the global distribution of tropical storm hazards?
- hurricanes usually develop west/southwest of the Atlantic Ocean and the east pacific (around Mexico and the Caribbean Sea) between the equator and the Tropic of Cancer (slight above this though in the Atlantic)- Aug-Oct
- cyclones usually developed within the two tropics north of the Indian Ocean and West of the pacific ocean - June-Dec
- typhoons are west of the pacific ocean between the equator and Tropic of Cancer, although sometimes above it, heading towards Japan - June-Dec
How is the magnitude measured for tropical storms?
Measured on the Saffir-Simpson Scale (A scale of 1-5) based on maximum sustained wind speed and thus power of the storm.
1: 74-95mph - winds produce some damage
2: 96-110mph - extensive damage
3: 111-129mph - devastating damage
4: 130-156mph - catastrophic damage
5: 157mph+ - even more catastrophic damage
What is the frequency of tropical storms?
Tropical storms form in the Northern Hemisphere from June-November, and the Southern Hemisphere from November-April. The majority of tropical storms do not develop into strong storms and do not reach land. Tropical storms that are higher magnitude and reaching land are thought to be increasing in frequency.
- year with the highest amount of hurricanes in the North Atlantic is 2005 - approx halve being major
- in 1964, all hurricanes that occurred were major
- 1982 was the year with the lowest occurring hurricanes
- the frequency fluctuates, yet the average occurring has increased more recently
What is the regularity of tropical storms?
Tropical storms are irregular because although they occur in the same areas, their path does not follow a set route - the route taken is dependent on the storm and the climatic conditions.
— they mostly occur from late summer into autumn - over a long period of time there is a degree of symmetry, although this does not mean that in any one year the pattern will be reflective of this
What is the predictability of tropical storms?
Tropical storms are fairly predictable, particularly in their geographical locations (restricted in the tropics, yet not close to the equator itself)
- advances in weather prediction computer models means forecasting the initial development of tropical cyclones has improved in recent years
—> each year NOAA publishes a prediction of hurricane activity for the coming season. Uses a number of indicators, such as sea-surface temps, atmospheric conditions and short-term climatic cycles.
How are strong winds a storm hazard?
- tropical storms have average wind speeds of over 75mph. In extreme cases, at the eye wall, gusts reach 155mph.
- These can tear off roofs, break windows or damage communication networks
- flying debris (which can also block road networks).
- If power lines fall, result in power cuts and potential electrical fires.
—> e.g. lots of damage caused by strong winds from Cyclone Winston, Fiji, 2016
Why are storm surges a storm hazard?
TSs cause a surge of high water caused by intense low atmospheric pressure (which allows seawater to rise vertically), combined with powerful surface winds (which whip up waves).
- result in coastal flooding as storm surges typically 3-5m higher than normal high tides
—> extreme coastal erosion (with potential to undermine man-made structures), flooding of low-lying land with seawater and/or debris and damage to property. It extreme cases, loss of life.
—> e.g. Hurricanes Katrina, USA 2005, recorded a storm surge of 7.6m, one of the largest ever recorded