Meteological Hazards Flashcards
(41 cards)
Define Meteorological Hazard
Hazards related to atmospheric patterns or conditions, and are generally caused by weather factors such as precipitation temperature, wind speed and humidity
State the 5 ways of classifying Hazards
- Scale
- Frequency
- Nature of Hazard
- Scale of Intensity
- By wind speed
Using the 5 methods of classification, classify a Tropical Storm
Scale=Regional Frequency= July-September N.Hemisphere, Jan-March S.Hemisphere Nature of Hazard=Winds and Flooding Scale of Intensity=Saffir Simpson Wind Speed=119-251km/h
Using the 5 methods of classification, classify a Tornado
Scale=Local Frequency=Any time Nature of Hazard=Wind Scale of Intensity=Fujita Wind Speed=100-320km/h
Using the 5 methods of classification, classify a Drought
Scale=Local/regional
Frequency=All year round, peak time is summer months
Hazard=Lack of precipitation and extreme temperature
Using the 5 methods of classification, classify a Flood
- Local
- All year round
- Precipitation
Using the 5 methods of classification, classify Fog
- Local
- All year round
- Precipitation, temperature, Visibility
Using the 5 methods of classification, classify Photochemical Smog
-Local (cities)
-All year round, peak time summer months
-Visibility
Emissions of chemicals- health problems
Describe the distribution of tropical storms
- Generally found of east coast of continents
- Track away from the equator in a curve due to the Coriolis effect
What is a tropical storm
A localised, very intense low pressure wind system, forming over tropical oceans and with winds of up to 39mph
What is a cyclone
A hurricane, cyclone or typhoon is a developed tropical storm, wind speeds reach at least 74mph.
Define Global Energy Budget
The balance between the incoming solar radiation, the outgoing terrestrial radiation and the redistribution of the sun’s energy
What are the 4 vertical transfers of energy
Conduction, Convection, Radiation, Latent Heat
What are the 3 horizontal transfers of heat
Atmospheric circulation (tri-cellular model), ocean currents and jet streams
Define Conduction
Vertical transfer of heat through direct contact between particles of a substance without moving the particles to a new location
Define Convection
Vertical transfer of heat though movement of particles from one location to another, generally occurs in fluids
Describe the role of the Coriolis force
- Without the Coriolis force, winds would run North to South or South to North in each of the cells
- The force drags the wind giving them an east or west component
- It describes the pattern of deflection taken by objects not firmly connected to the ground as travel long distances around the world
Describe the structure of a tropical storm/cyclone
- It has a central eye that is 30-60km wide. It has calm conditions
- An eyewall is the boundary between the stronger and calmer conditions
- The eye is surrounded by rain bands
Describe the formation of tropical storms/cyclones
- As sea temperatures rise there is an increase in evaporation and the rising of air and water in thermals
- As these thermals rise their temperatures drops, causing the water vapour to condense leading to the formation of clouds
- Latent heat is released during the condensation fuelling the storm
- The water droplets in the clouds collide with each other causing them to become bigger and fall as rain
- Because the air at the centre of the storm has risen, an area of low pressure forms at the surface
- The global energy budget act to balance at this pressure difference, as air moves from surrounding high pressure areas to the centre of the storm, this creates high winds.
- The whole storm migrates across the ocean towards the land, the Coriolis force causes the whole system to rotate about a calmer point which is the eye
- As they move across the land, they lose their source of energy and die out
What sea conditions does a tropical storm require to form, and how does this effect when they occur
Sea temperatures above 26.5C, this process takes a long time as the ocean is constantly moving and redistributing heat. Therefore hurricanes tend to form in late summer
Describe the Bernoulli Effect
- Velocity and Pressure are inversely proportional, so low pressure of hurricanes causes an increase in wind speed
- When wind blows at high speeds, a low pressure system is created above the building, so the pressure inside the building is greater than outside the building
- Therefore the roof of a building is blown up towards the wind, rather than being pushed down by the wind as objects move from high pressure regions to low pressure regions
How does the Coriolis force cause cyclones to rotate
- At the centre of a cyclone there is low pressure, this means the high pressure surrounding the eye is constantly rushing towards the centre
- But the Coriolis effect the high pressure is deflected off course.
- In the N.Hemisphere the winds are deflected slightly to the right, causing the whole cyclone to rotate in an anti-clockwise direction.
How is the pattern of intensity for tropical storms changing
-Hurricanes are becoming more devastating than in the past because they have a lower velocity resulting in the impacts being amplified and dragged out over larger areas
How is the pattern of periodicity for tropical storms changing
The number of tropical storms doesn’t seem to be changing, but the number reaching hurricane status is increasing