Weather Hazards Flashcards

1
Q

Define the atmosphere

A

the complex mass of gases, liquids and solids surrounding the earth

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2
Q

Define weather

A

day to day conditions of temperature, cloud, precipitation, fog/visibility, wind + sunshine

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3
Q

What causes wind?

A

Air moves from an area of high pressure to low pressure. The low pressure means that air is rising, there is less air

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4
Q

Order of Cells from Equator up in the global atmospheric circulation

A

Hadley Cell, Ferrel Cell, Polar cell.

between Hadley and Ferrel = High pressure descending air

between ferrel and polar = low pressure rising air

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5
Q

Describe the global atmospheric circulation

A

Sinking air creates high pressure, and rising air creates low pressure.

Surface winds move from high to low pressure, transferring heat and moisture from one to another.

These winds curve due to the earth’s rotation and change seasonally as the tilt and rotation of the earth causes relative changes in the position of the overhead sun.

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6
Q

How does global circulation affect the world’s weather?

A

Cloudy and wet in the UK – we are 60o north and this is close to where cold polar air from the north meets the warm subtropical air from the south. So since the boundary is unstable, the rising air cools and condenses forming clouds and rain.

Hot and dry in the desert – there they are 30o north or south of the equator, where the sinking air means that there is high pressure, little rain, hot daytime temperatures and very cold nights. Since no air is rising there are no clouds forming and therefore little rain.

Hot and sweaty at the equator – there the air is rising and there is another pressure belt called the equatorial low. It’s much hotter here since the sun is directly overhead, so it is often cloudy with high rainfall. This is where tropical rainforests are often found.

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7
Q

Define Tropical Storms

A

a huge storm that developed in the tropics, they can be called hurricanes (US and Caribbean), cyclones (south-east Asia, Australia) and typhoons (japan and Philippines).

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8
Q

How do Tropical Storms form?

A
  1. Rising air draws evaporated water vapour up from the warm ocean surface which cools and condenses to form towering thunderstorm clouds.
  2. The condensing releases heat which powers the storm and only draws up more water vapour.
  3. Multiple thunderstorms join to form a giant rotating storm.
  4. The Earth’s rotation spin the cloud an over 120 km/h creating a vast cloud spiral with a central, calm eye of rapidly descending air.
  5. Prevailing winds drift the storm over the ocean surfaces like a spinning top, gathering energy and strength.
  6. On reaching land the energy supply of evaporated water is cut off and the storm will weaken.
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9
Q

Conditions for Tropical Storms

A
  • mainly formed in Summer and Autumn
  • Warm oceans supply the energy
  • Need to be at least 26.5degreesCelsius
  • Oceans take months towarm up
  • Around 5-15o north or south of the equator as there the Coriolis effect (the effect of the earth’s rotation) is stronger.
  • Intense heat and humidity in the tropics makes the air unstable
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10
Q

Structure and feature of Tropical Storms

A
  • 500-2000km long
  • height = about 12km
  • Eye = clearly visible, small area where relatively cold air sinks towards the ground and warms up
    = no clouds and conditions are calm.
  • Eye wall = bank of cloud; strong in excess of 120km/h; heavy torrential rain; thunder and lightning
  • Beyond the eye wall there are further banks of clouds with thunderstorms and occasional tornadoes
    = strong gusty winds
    = heavy rain
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11
Q

Description of the Hadley Cell

A

Since it is at the equator, the sun is directly overhead, there are vast quantities of warm, moist air. This rises to about 30degrees north or south where it is cooled down again and goes back towards the equator where it is heated up again with the concentrated sun rays.

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12
Q

Conditions near the equator

A
  • very humid
  • hot
  • wet
  • high rainfall
  • Tropical Rainforest
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13
Q

General direction of Tropical storms

A
  • overall most go from east to west
  • never cross the quator
  • Northern Hemisphere go up north
  • Southern Hemisphere go down south
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14
Q

How do the tropical storms move thousands of miles

A
  • the prevailing wind pushes the storm along as wells as ocean currents
  • the Earth’s rotation from east to west.
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15
Q

Under what conditions do tropical storms lose or gain intensity?

A

Lose intensity:

  • cooler ocean
  • moving on land

Gain intensity

  • warmer ocean
  • not over land
  • Time = takes days to build
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16
Q

How will climate change affect tropical storms?

A

 Distribution
The sea surface temps have increased by 0.25 – 0.5o in the tropics so it is easier for them to form and affect the distribution. Therefore, areas which are now outside the hazard zone may become affected. The storms can also become more powerful.

 Frequency
Six of the ten most active years in the north Atlantic since the 1950 have happened since the mid-1990s.

 Intensity
In the last 20 years, hurricane intensity has increased, this is linked with sea surface temperatures.

17
Q

Locational detail of the Philippines

A
  • South East Asia
  • Archipelago
  • Pacific Ocean to the East
    South China sea to the west
  • Population: 99.9 million
18
Q

Overview of Typhoon Haiyan

A

It was one of the strongest category 5 storms ever recorded. There was very low air pressure which caused a 5m storm surge which was swept on shore by winds of up to 275km/h. coastal devastation included 90% of Tacloban destroyed by the storm surge.

19
Q

Primary Effects of the Typhoon Haiyan

A

 About 6300 killed, most in storm surge.
 Over 600 000 displaces and 40 000 homes damaged or flattened.
 Over 400mm of rain caused widespread flooding.
 30 000 fishing boats destroyed.
 Airport terminal badly damaged.
 Wind damage to buildings, power lines and crops.

20
Q

Secondary Effects of Typhoon Haiyan

A

 14 million affected including 6 million lost jobs.
 Landslides and blocked roads due to flooding.
 Power supplies cut off for a month in certain areas.
 Shortages of power, water, food and shelter, leading to outbreaks of disease.
 Looting and violence in Tacloban.

21
Q

Immediate Responses of Typhoon Haiyan

A

 Rapid overseas aid.
 US aircraft carrier ‘George Washington’ assisted with the search and rescue and delivery of aid.
 Over 1200 evacuation centres set up.
 Field hospitals helped injured.

22
Q

Long Term Responses of Typhoon Haiyan

A

 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.

23
Q

Tropical Storms : Monitoring and Prediction

A

Tropical storms can’t be prevented, but they can be monitored and their tracks can be predicted so warnings can be given out and people can prepare and know what to expect.
- computer models

e.g. National Hurricane center in Miami warns people.

24
Q

Tropical Storms : Protection

A
  • Cyclone shelters = very expensive but highly effective
  • Storm drains = preventing flooding, cheaper option
  • Sea walls to protect key properties from storm surge
  • Houses on stilts = if made with strong material (expensive) but can be very effective.
25
Q

Tropical Storms: Planning

A

It is unrealistic to stop the tens of millions of people living and working in coastal areas that are at risk, so instead it can be made safer. This means to educate the communities so that they understand the dangers and how to respond to them.

26
Q

UK Weather Hazards: Thunderstorms

A

they follow hot weather bringing lightning and torrential rain linked with ‘flash’ flooding.

27
Q

UK Weather Hazards: Prolonged Rainfall

A

this over a long time leads to river floods, such as the wet winter of 2013/14. This is common in the winter when snow melt adds to the issue.

28
Q

UK Weather Hazards: Drought and extreme heat

A

this causes rivers to dry up and reservoirs to run dangerously low. The record-breaking 2003 heatwave killed 20,000 all over Europe – mostly children or the elderly.

29
Q

UK Weather Hazards: Heavy snow and extreme cold

A

they are less common nowadays but can still cause hardships to those in the north. Dec 2010 was the coldest in a century.

  • usually coming in from the east
30
Q

UK Weather Hazards: Strong winds

A

such as Feb 2014, cause disruption to power supplies, damage from fallen trees and coastal battering from large waves.

31
Q

Somerset levels: Overview

A

they were caused by a sequence of south-westerly depressions which brought record rainfall in Jan and Feb. The high tides and storm surges swept water up the rivers from the Bristol Channel preventing normal flow and rivers, clogged with sediment, had not been dredged for 20 years.

  • Somerset located in SW of UK
32
Q

Social Impact of the Somerset Levels

A
  • over 600 houses flooded
  • 16 farms evacuated
  • some residents evacuated to temporary accommodation for several months
  • Many people had power supplies cut off
  • Villages such as Moorland and Mulchelny cut off. This affected people’s daily lives e.g. attending school, shopping etc
33
Q

Economic Impacts of the Somerset Levels

A
  • Somerset County Council estimated the cost of flood damage to be more than £10 million
  • over 14, 000 ha of agricultural land under water for 3-4 weeks
  • over 1000 livestock evacuated
  • Local roads cut off by floods
  • Bristol to Tauton railway line closed at Bridge water
34
Q

Environmental Impact of the Somerset Levels

A
  • Floodwaters were heavily contaminated with sewage and other pollutants including oil and chemicals
  • A huge amount of debris had to be cleared
  • Stagnant water had collected for months had to be reoxygenated before being pumped back to rivers.
35
Q

Immediate Response of Somerset Levels

A

 Huge media interest was generated.
 Boats were used as transport for cut-off villages.
 Community groups and volunteers gave individual support.

36
Q

Long-Term Responses of Somerset Levels

A

 £20 million flood action plan launched by Somerset county council and Environmental Agency to reduce future risk.
 8km of rivers Tone and Parrett dredged.
 Road levels raised in lowest dips.
 Vulnerable communities will have flood defences.
 River banks raised and strengthened, and more pumping stations built.

37
Q

Examples of Extreme weather in the UK

A

2003 – heatwave – highest ever temp of 38.5oC recorded in Kent. Over 2000 died, railways buckled and roads melted.

2007 – floods – several deaths and many left homeless in the summer floods.

2009 – snow – heavy snow in the south including 20cm in London.

2015/16 – floods – December 2015 wettest and warmest ever recorded.

38
Q

Causes of Extreme weather

A

These recent cases of extreme weather could be because of climate change and global warming as they lead to more energy in the atmosphere, which could lead to more intense storms, and it probably affects the atmospheric circulation, bringing floods to normally dry areas and heatwaves to normally cooler areas.