Topic 1 - Hazardous Earth Flashcards

1
Q

Explain why low latitude locations receive more heat than places close to the poles?

A

The sun’s rays have to heat up a smaller surface area and travel through less atomosphere at the equator compared to the poles making the equator warmer than the poles.

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2
Q

What is high pressure?

A

As air cools it becomes more dense and it falls. This transfers heat to the ground. This leaves clear skies and little/no rainfall.

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3
Q

What is low pressure?

A

As air is heated by the ground it becomes less dense causing it to rise. It transfers heat to the atmosphere, cools and then condenses. This creates clouds and rain.

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4
Q

What are the atmospheric circulation cells called?

A

Polar Cell
Ferrel Cell
Hadley Cell

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5
Q

Where is heat moved from and to?

A
  1. The sun warms the earth at the equator creating a low pressure belt.
  2. The cool air moves out to 30° North and South to create a high pressure belt.
  3. The cool air reaches the ground surface and moves as surface winds either back to the equator or towards the poles.
  4. At 60° the warmer air meets the colder sir from the poles. The warmer air is less dense than the cold air so it rises creating low pressure.
  5. Some of the air moves back towards the equator and the rest moves back to the poles.
  6. At the poles the cool air sinks creating high pressure. The high pressure air is drawn back towards the equator as surface winds.
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6
Q

How do ocean currents move heat from the equator to the poles?

A

Surface currents are caused by winds and help transfer heat away from the Equator (e.g the Gulf Stream brings warm water from the Caribbean to Western Europe).

Deep Ocean Currents:
When water freezes at the poles the surrounding water gets saltier increasing in density. It therefore sinks causing warmer water to flow in at the surface - creating a current. This warmer water is cooled and sinks continuing the cycle. This cycle moves water in a big loop round the world (this is known as the thermohaline circulation).

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7
Q

Explain how atmospheric circulation causes high pressure areas places like Tindouf?

A

Sinking air from the Ferrel and Hadley Cells create high pressure meaning it is very arid and has a high level of solar radiation.

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8
Q

Explain how atmospheric circulation causes low pressures areas places like Singapore?

A

Rising air from the Hadley Cells meeting causes a low pressure zone meaning it has lots of rainfall but has a high level of solar radiation leaving it very humid.

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9
Q

What are the four different natural factors that have caused world climates to change over the last 400,000 years?

A

Asteroid Collisions: Asteroids hitting the Earth’s surface throw up a huge amount of dust into the atmosphere which prevent the Sun’s particles from reaching the Earth’s surface.

Solar Output Variation: The sun’s output of energy isn’t constant. Periods when solar output is reduced may cause the Earth’s climate to become cooler.

Volcanic Activity: Major volcanic eruptions eject large quantities of material into the atmosphere. These block the sun’s rays from reaching the earth’s surface so it cools.

Orbital Change.

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10
Q

Orbit, Tilt and Wobble – what are these and why do they cause variations?

A

Strech (eccentricity): the path of the Earth’s orbit around the sun changes from an almost perfect circle to an ellipse.

Tilt: the Earth’s axis is tilted at an angle as it orbits the sun.

Wobble (procession): the axis of the Earth wobbles like a spinning top.

These cycles affect the amount of solar radiation the Earth recieves.

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11
Q

What evidence do we have that tells us about previous temperatures?

A

Trees Rings: the thickness of each ring depends on the climate when the ring was formed - when its warmer the rings are thicker.

Ice Cores: Scientists drill into ice sheets to get long ice cores of ice. By analysing the gases trapped in the layers of ice they can tell what the temperature was each year.

Historical Records: Diaries and paintings, etc, can show what the climate was like in the past.

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12
Q

Give two pieces of evidence which show the earth’s climate was:
a. Warmer

A

Harvest records show that England was warm enough to grow large amounts of grapes during the Medieval Warm Period (900-1300).

Tree ring data suggests this was also the cause during Roman times when temperatures were almost 1°C warmer than today.

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13
Q

Give three pieces of evidence which show the earth’s climate was:
b. Colder

A

Paintings from the 17th Century show the London Frost Fairs which took place on a frozen River Thames during the Little Ice Age.

Historical Records talk about Arctic ice reaching as far south as Scotland.

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14
Q

How have humans enhanced the greenhouse effect (concentration of gasses)?

A

Humans are adding too many greenhouse gases into the atmosphere which means more heat is being trapped and the planet is being warmed up.

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15
Q

Give reasons how the following have caused enhanced greenhouse effect and climate change:
a. Industry

A
  • Most industry uses a lot of energy
  • Some industrial processes also release greenhouse gases
  • Industrial waste may end up in landfill sites where it decays releasing methane
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16
Q

Give two reasons how the following have caused enhanced greenhouse effect and climate change:
b. Energy Production

A

CO2 is released into the atmosphere when fossil fuels are burnt

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17
Q

Give two reasons how the following have caused enhanced greenhouse effect and climate change:
c. Transport

A

Most transport runs on fossil fuels which release greenhouse gases when burnt
Car ownership is rapidly increasing in countries which are developing, this means there are more cars on the road which increases congestion. As a result car engines are running for longer, so the amount of greenhouse gases released increases.

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18
Q

Give two reasons how the following have caused enhanced greenhouse effect and climate change:
d. Farming

A

Farming of livestock produces a lot of methane
Rice paddies have to flood fields which emits methane
Trees absorb and store CO2. When they are cleared for agriculture it stops the absorbtion of CO2 which leaves more CO2 in the atmosphere

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19
Q

Give evidence to explain how each of the factors below show that climate change is happening:
a. Sea levels

A

Glaciers are shrinking and ice sheets are melting which is adding to the sea making the sea levels rise.
Water in the oceans expands as it gets warmer. This is called thermal expansion.
Since 1901, sea levels have risen by almost 0.2m.

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20
Q

Give evidence to explain how each of the factors below show that climate change is happening:
b. Global temperatures

A

Temperstures have increased by newely 1°C since 1880
The top ten warmest years since records began have all been since the year 2000

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21
Q

Give evidence to explain how each of the factors below show that climate change is happening:
c. Arctic ice

A

The extent of arctic sea ice in winter has decreased by more than 3% each decade over the past 35 years.

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22
Q

Give evidence to explain how each of the factors below show that climate change is happening:
d. Extreme weather

A

Since 1950 that has been a higher frequency of heat waves and many areas and fewer cold weather extremes.
In the UK more rainfall records are broken in 2010 to 2020 then in any other decade on record.

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23
Q

What are emission projections? Why do we need them? What human and physical reasons affect them? Why can’t we be more certain about the future climate temperature?

A

How the climate might change and the consequences of any changes.
Physical Porcesses: e.g. the effect of volcanic eruptions on the climate
Human: e.g. the growth of industry or the development of clean energy

Predictions have to take into account population increase and economic development.
We don’t know how the natural factors will have an impact on climate change.
We don’t know what attempts there will be to manage the amount of greenhouse gases or how successful they’ll be.

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24
Q

Explain a consequence of climate change that will:
a. Make people poorer
b. Affect human health
c. Lead to overcrowding in some areas
d. Reduce food growth
e. Cause damage to houses/lost business

A

Deaths due to heat
To hot or dry to inhabit
Low-lying coastal areas lost to the sea
Migration and overcrowding
Some crops have suffered from climate change
Some farmers in higher latitudes are benefiting from the warmer conditions
Malnutrition, ill health, death from starvation
More money spent on prediction, reducing impacts and rebuilding

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25
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26
How do tropical cyclones form?
When the sea water reaches 26.5°C or above the air above begins rising and creates low pressure at the surface. Warm, moist air rises and condenses to produce cumulonimbus clouds. This provides energy from the water. The coriolis force causes rising currents of air to spiral around the centre. The air rises and cools and some of it descends to form the clear cloudless eye of the storm.
27
Why do tropical cyclones intensif in energy?
It gets larger as it moves because it has given you heat and moisture from the ocean.
28
Why is a tropical cylcone's energy sometimes lost?
Once it reaches land, the air pressure rises as the temperature falls, winds drop rainfall decreases and it dissipates.
29
Explain how tropical cyclone hazards impact on a. the people
Windspeeds can be strong enough to completely destroy buildings, which means people are left homeless. High windspeeds and floodwater can carry large amounts of debris which can kill or injure people. Damaged roads make it very difficult for aid and emergency vehicles to get through.
30
Explain how tropical cyclone hazards impact on b. the environment.
Storm surges can erode beaches and damage coastal habitats. Trees uprooted by high winds which can damage or completely destroy wooded habitats. Landslides deposit sediments in rivers and lakes which can kill fish and other wildlife.
31
How and where would be most vulnerable to the impacts of tropical cyclones?
Flat islamd nations are the most vulnerable as the cyclone will be able to cover more land as it can build back its energy as it covers water. Being flat will make it more vulnerable to flooding and high winds. Poor countries are also economically vulnerable because many people may not have insurance to cover the costs of repairing the damage healthcare is also bad in these places so they can't treat everyone and it is harder to rescue people because of poor infrastructure.
32
How can we prepare (before and after) for tropical cyclones and how do these different techniques limit the impact of cyclones?
Predicting where and when a tropical cyclone is going to happen gives people time to evacuate and protect their homes and businesses. Warning strategies are used to alert people to a tropical cyclone. An alert will give people time to leave their homes and get to a safe place. This can reduce the number of deaths and injuries. Defences can be built along the coast prevent damage from storm surges. Buildings can be made to withstand storm surge this will reduce the number of buildings destroyed.
33
How can we respond (during) a tropical cyclone and how does this limit the impact of tropical cyclones?
Quick rescue can save stranded people so less people die. Quick repair of power lines, food supplies, communication and water pumps can provide people with the supplies they need so they don't die.
34
What were the good and bad aspects of the preparation in USA?
Good The USA has a sophisticated monitoring system to predict if (and where) a hurricane will hit. 70-80% of New Orleans residents were evacuated before the hurricane reached land. Bad The Levees of New Orleans had not been maintained and the pumping stations didn't work. This caused widespread flooding (over 80% of the city was underwater). The evacuation procedures was hampered as the highways were too congested with fleeing traffic and people didn't use public transport.
35
What were the good and bad aspects of the response in the USA?
They had greater resources, wealth and communication to help the public. This allowed quick rescues and repairing of power and water supplies.
36
What were the impacts of Hurricane Katrina on people/environment?
Environment Coastal habitats such as sea turtle breeding beaches were damaged. Some coastal conservation areas were destroyed. Flooding damaged oil refineries in Louisiana, causing massive oil spills. People More than 1800 people were killed. 300 000 houses were destroyed and hundreds of thousands of people were made homeless. 3 million people were left without electricity. Roads were damaged and some bridges collapsed. 230 000 jobs were lost from damaged businesses.
37
What were the good and bad aspects of the preparation in Myanmar?
Good: Indian weather agencies warned the government of Myanmar that Cyclone Nargis was likely to hit the country 48 hours before it did. Bad: Myanmar doesn't have a dedicated monitoring centre for tropical cyclones. They didn't reach people in poor rural communities. Warnings didnt reach people in poor rural communities which meant more people were killed because they didn't know what to do or where to evacuate to. There were no emergency preparation plans, no evacuation plans and the country didn't have an early warning system. Mangrove forests protect the coast from flooding, but loads had been chopped down in the decade before Nargis hit, reducing the natural protection. Houses were made out of weak materials (wood)
38
What were the good and bad aspects of the response in Myanmar?
Aid agencies were refused access to Myanmar for a week after the disaster due to the lack of transparency in the government.
39
What were the impacts of Cyclone Nargis on people/environment?
Environment 14000km2 of land was flooded. 38000 hectares of mangrove forests were destroyed. The flooding caused erosion and salination. People More than 140 000 people were killed. 450 000 houses were destroyed and 350 000 were damaged. Around 65% of rice paddies in the Irrawaddy delta were damaged, which led to a loss of livelihoods. A lot of people suffered from diseases caused by poor sanitary conditions and contaminated water.
40
Tropical Cyclones Pressure: Rotation Direction: Structure: Location: Oceans where hurricanes occur: Oceans where typhoons occur: Oceans where tropical cyclones occur:
Pressure: Low pressure Rotation Direction: Winds rotate outwards at the top. In the southern hemisphere they rotate in a clockwise direction, while in the northern hemisphere they rotate in an anti-clockwise direction. Structure: Clear sky and no wind in the eye. Dense canopy of cirrus clouds form at the top, cloud tops can reach 12-15km high. Location: Mostly between the Tropic of Cancer and the Tropic of Capricorn Oceans where hurricanes occur: Atlantic Ocean Oceans where typhoons occur: Pacific Ocean Oceans where tropical cyclones occur: Indian Ocean
41
Core: Chemical composition Temperature Density Physical state
Chemical composition: Iron & Nickel Temperature: 4400-6000°C Density: very dense Physical state: outer liquid, inner solid
42
Mantle: Chemical composition Temperature Density Physical state
Chemical composition: silicon-based rocks Temperature: 1000-3700°C Density: 3.4-4.4 g/cm3, quite rigid Physical state: semi-molten, it can flow
43
Crust: Chemical composition Temperature Density Physical state
Chemical composition: silicon-based rocks Temperature: 900°C Density: continental - less dense, oceanic - more dense Physical state: solid
44
What is the asthenosphere and how is this important for plate movement?
The semi mountain layer above the mantle. It is important for plate movement as it is working convection currency occur which drag the plates around.
45
Where does the inner core’s heat originate from?
Radioactive decay of uranium thorium in the core and mantle.
46
How do convection currents move tectonic plates?
Lower parts of the asthenosphere heat up and rise because they become less dense. They then cool down and sink. The circular movements of semi molten rock called convection currents. Convection currents in the asthenosphere create drag on the base of the tectonic plates and this causes them to move.
47
Explain the events (earthquakes and volcanoes) at the following plate boundary: a. Divergent (constructive)
Volcanoes and small earthquakes
48
Explain the events (earthquakes and volcanoes) at the following plate boundary: b. Convergent (destructive)
Volcanoes, tsunamis, earthquakes
49
Explain the events (earthquakes and volcanoes) at the following plate boundary: c. Conservative (transform)
Earthquakes
50
Composite volcanoes: magma type/lava flows and explosiveness
magma type: andesitic lava, high silica lava flows: thick, sticky, cannot travel far explosiveness: very high
51
Shield volcanoes: magma type/lava flows and explosiveness
magma type: basaltic lava, low silica lava flows: runny, flows quickly, spreads far explosiveness: low
52
Hotspot volcanoes: magma type/lava flows and explosiveness
magma type: basaltic lava, low silica content lava flows: fast flowing, runny, travels far explosiveness: low
53
Explain which plate boundaries earthquakes are found at?
All of the plate boundaries
54
Define: focus and epicentre
Focus: the point where an earthquake starts Epicentre: the point on the Earth's surface directly above the focus
55
Explain why high magnitude, shallow focus earthquakes are most damaging?
The higher the magnitude of an earthquake the more energy is released. Shallow focus earthquakes are more damaging than deep focus earthquakes because they have less rock to travel through to reach the surface.
56
Explain how a tsunami might occur if an earthquake happens close to the sea?
Underwater earthquakes, cause the sea bed to move which displaces water. The wave spread out from the epicentre of the earthquake. When the waves reach land, they search very far in land collecting debris as they go.
57
What is a hotspot volcano?
Cross moves over a hotspot and the magma forces its way through the crust and creates a volcano. The plate moves on and takes the island with it so volcanic activity stops.
58
What is a primary impact and a secondary impact?
Primary impact: the immediate impacts of the ground shaking, e.g. buuldings collapsing Secondary impact: the impacts that happen as a result of the primary impacts, e.g. tsunamis
59
What is prediction?
Using historic and scientific data to predict when and where an earthquake will occur
60
What is prepare?
Buildings are designed to be able to withstand an earthquake
61
What is plan?
The public practice protection and response operations and emergency services trained for the response.
62
Impacts of the earthquake in Japan (2011)?
Primary: Thousands of buildings were damaged. Between 667 and 1479 deaths occurred mostly as a result of buildings collapsing Electricla power, water and sewerage systems were disrupted. Secondary: triggered a tsunami Over 17,000 deaths due to drowning in the tsunami Over 23,000 people were made homeless.
63
What was done to predict, prepare and plan for the Japanese earthquake?
Predict: The Japan Meteorological agency and local governments monitor size activity all over the country. Prepare: buildings are reinforced with steel frames, deep foundations and shock absorbers. Plan: Japan's population is educated on being prepared for earthquakes and tsunamis.
64
What was done in the short term to provide relief from the earthquake?
International aid and search teams are brought in. Power supplies transport and communications were restored.
65
What were the impacts of the Haiti earthquake (2010)?
Primary: 316,000 deaths and 300,000 injured. More than 180,000 homes were destroyed All eight hospitals collapsed or were badly damaged Secondary: cholera spread through squatter camps which killed over 8,000 people Economic losses increased because of closed factories and no tourism Looting and crime increased.
66
What was done to predict, prepare and plan for the Haiti earthquake?
They didn't have any early warning systems. They were completely unprepared for it. They had poorly built buildings.
67
What was done in the short term to provide relief from the Haiti earthquake?
International aid was sent. Supplies were sent by the USA.