weather hazards

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  • Created by: Iona112
  • Created on: 05-04-22 09:32
Global atmospheric circulation
- sinking air creates high pressure, rising air creates low pressure
- surface winds move from high to low pressure, transferring heat and moisture
- winds curve due to the earths rotation and change seasonally as the tilt and rotation of earth changes t
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How does global atmospheric affect the UK's weather
- UK's weather is wet and cloud
- close to where cold polar air from the north meets warm subtropical air from the south
- these surface winds from the south- west usually bring warm wet weather, as rising air cools and condenses forming clouds and rain
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atmospheric cells
interconnected circular air movements
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how does global circulation affect the weather in the deserts
- deserts are hot and dry
- found at about 30 north and south where sinking air means high pressure, little rain, hot day time temps and very cold nights
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how does global circulation affect the weather at the equator
- hot and sweaty at the equator
- low pressure marks where the sun is directly over head
- hot, humid air rises, cools and condenses causing heavy rain
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tropical storms
huge storms called hurricanes cyclones and typhoons in different parts of the world
form 5-15 degrees north and south of the Equator
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what are the requirements needed for a tropical storm to form
- 5-15 degrees north and south of the equator in summer and Autumn where:
- ocean temp are highest (above 27C)
- the spinning effect (Coriolis) of the earths rotation is very high
- intense heat and humidity makes the air unstable
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how will climate change affect tropical storms
affect the frequency, intensity and distribution
- over last few decades sea surface temp has risen by 0.25-0.5C
- tropical storms may extend into South Atlantic and parts of the sub-tropics
- In the North Atlantic hurricane intensity has risen in the las
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Typhoon Haiyan
November 2013
- One of the strongest Category 5 storms ever recorded
- Hit the Philippines
- Very low air pressure caused 5m storm surge swept on shore by winds up to 275km/h
- Coastal devastation included 90% of Tacloban destroyed by storm surge
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typhoon Haiyan primary effects
- 6300 killed- most in storm surge
- Over 600,000 displaced
- 40,000 homes destroyed or damaged
- Wind damage to buildings, power lines and crops
- Over 400mm of rain caused widespread flooding
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typhoon Haiyan secondary effects
- 14 million affected including 6 million jobs lost
- Flooding caused landslides- blocking roads and restricting access for aid workers
- Shortages of power, water food and shelter, leading to outbreaks of disease
- Infrastructure including schools destro
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Typhoon Haiyan immediate response
- Rapid overseas aid included NGOs
- US helicopters assisted search and rescue, and delivery of aid
- Field hospitals helped injured
- Over 1200 evacuation
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Typhoon Haiyan immediate response
- UN and international financial aid, supplies and medical support
- Rebuilding of infrastructure
- Rice farming and fishing quickly re-established
- Homes rebuilt in safer areas
- More cyclone shelters built
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Monitoring and prediction
storms can be monitored and their tracks predicted
this allows warnings to be issued and preparations made
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protection
-reinforced walls, roofs, window shutters
- storm drains
- saw walls
- cyclone shelters in Bangladesh are used as community centres schools or medical centres for the most of the time
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planning
- education and media campaigns to raise individual and community awareness
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What are the UK's weather hazards
- thunderstorms
- prolonged rainfall
- drought and extreme heat
- heavy snow and extreme cold
- strong winds
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thunderstorms
follow hot weather bringing lighting and torrential rain
linked with flash flooding
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prolonged rainfall
prolonged rainfall over a long period leads to river floods
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drought and extreme heat
causes rivers to dry up and reservoirs to run dangerously low
the 2003 heatwave killed 20,000
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heavy snow and extreme cold
less common nowadays
can cause great hardship to people in the north of the UK
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Strong Winds
cause disruption to power supplies, damage from fallen trees and coastal battering from large waves
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Somerset levels
extensive area of low-lying land in South-west England
severly flooded in 2014
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causes
- sequence of South- Westerly depression brought record rainfall in January and February
- High tides & storm surges swept water up the rivers from the Bristol channel preventing normal flow
- Rivers, clogged with sediment, had not been dredged in 20 yrs
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immediate responses
- Huge media interest
- Cut off villagers used boats for transport
- Community groups and volunteers gave support
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long term responses
- £20 million Flood Action plan launched to reduce future risk
- 8km of rivers Tone and Parrett dredged
- Road levels raised
- Vulnerable communities have flood defences
- Riverbanks raised and strengthened
- Possible tidal barrage at Bridgwater by 2024
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social impacts
- 600 houses flooded
- 16 farms evacuated
- Residents evacuated to temporary accommodation for several months
- Villages cut off
- Many cut off to power supplies
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economic impacts
- estimated cost of flood damage is more than £10 million
- over 14000 ha of agricultural land under water for 3-4 weeks
- 1000 livestock evacuated
- Local roads cut by floods
- Bristol to Taunton railway line closed at Bridgewater
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environmental impacts
- Floodwaters were heavily contaminated with sewage, oil, and chemicals
- Huge amounts of debris
- Stagnant water that had collected for months had to be reoxygenated
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evidence that UK weather is becoming more extreme
- 2003 heatwave, highest temp ever recorded
- 2007, 2008 and 2009 floods
- 2009 heavy snow in the south
- 2010 heavy snow, record low temps in N Ireland
- 2013/2014 floods, Englands wettest winter in 250 years
- December 2015, wettest and warmest ever rec
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why might extreme weather evens be on the increase
climate change:
- leads to more energy in the atmosphere which could lead to more intense storms
- possibly affects atmospheric circulation, bringing floods to normally dry areas and heatwaves to normally cooler ones
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Other cards in this set

Card 2

Front

How does global atmospheric affect the UK's weather

Back

- UK's weather is wet and cloud
- close to where cold polar air from the north meets warm subtropical air from the south
- these surface winds from the south- west usually bring warm wet weather, as rising air cools and condenses forming clouds and rain

Card 3

Front

atmospheric cells

Back

Preview of the front of card 3

Card 4

Front

how does global circulation affect the weather in the deserts

Back

Preview of the front of card 4

Card 5

Front

how does global circulation affect the weather at the equator

Back

Preview of the front of card 5
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