2.1 - The Causes Of Climate Change Flashcards

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1
Q

Define adaption

A

Initiatives and measures to reduce the vulnerability of human and natural systems to climate change

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2
Q

Define albeado

A

The amount of incoming solar energy reflected back into the atmosphere by the earths surface

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3
Q

Define anthropogenic

A

Human relate processes and impacts

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4
Q

Define the enhanced greenhouse effect

A

The increasing amount of greenhouse gases in the atmosphere, as a result of human activities and their impact on atmosphere is systems, including global warming

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5
Q

Define global warming

A

The increase in temperatures around the world that hace been noticed since the 1960s, and particular in the 1980s

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6
Q

Define the greenhouse effect

A

The process by which certain gases (water vapour, carbon dioxide, methane and chlorofluorocarbons (CFCs)] allow short-wave radiation from the sun to pass through the atmosphere and heat up the Earth, but trap an increasing proportion of long-wave radiation from the Earth. This radiation leads to a warming of the atmosphere.

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7
Q

Define mitigation

A

Attempts to reduce the causes of climate change.

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8
Q

Define resilience

A

The ability of a population or a human or natural system to absorb change without having to make a fundamental change.

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9
Q

Define vulnerability

A

The degree to which a human or natural system is susceptible to, and unable to cope with, the adverse impacts of climate

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10
Q

What is the atmosphere

A

The atmosphere is an envelope of mixed gases which is held in place by gravitational attraction

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11
Q

What makes up the atmosphere

A

It consists of nitrogen (78%), oxygen (21%), and 1% trace gases

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12
Q

What are the 4 layers of the atmosphere

A
  1. Thermopylae
  2. Mesopause
  3. Stratopause
  4. Tropopause
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13
Q

What is the atmospheric layers

A

The atmosphere is 10,000 km in height
But gravity compresses 99% of the atmosphere to within 40 km of the Earth’s surface
50% of the atmosphere is in the first 5.6 km

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14
Q

What is the atmosphere heat budget

A

The Sun is Earth’s primary source of energy
It provides more energy in an hour than humans use in a year
Energy is received as short-wave radiation - insolation

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15
Q

What does the atmospheric heat budget depend on

A

The balance between isolation and outgoing long wave radiation

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16
Q

Where is energy lost when its passing through the atmosphere

A

Some energy is lost passing through the atmosphere, but there is an overall net gain of energy at the surface

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17
Q

Do polar regions have a net gain or deficit of energy and what causes it

A

Polar regions have a net deficit (they receive about 24% of insolation) due to absorption, reflection and scattering – albedo effect

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18
Q

Does the overall atmosphere have a net deficit or gain of energy

A

The atmosphere itself has an overall net deficit of energy

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19
Q

What is the neutral greenhouse affect and how does it reflect the atmospheres net deficit of energy

A

To compensate, heat is moved from the surface to the atmosphere by radiation, conduction and release of latent heat – the natural greenhouse effect

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20
Q

Define climate chnage

A

Any long term trend or movement in climate detected by a sustained shift in the average value for any climatic element (for example: rainfall, drought, hurricanes, temperature etc…)

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21
Q

What are the 2 main reasons for climate chnage

A
  • changing concentrations of green house gases
  • various kinds of external forces
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22
Q

Define green house gases

A

The atmospheric gases that absorb infrared radiation and cause world temperatures to be higher than they would otherwise be.

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23
Q

Define external forces

A

A term used to describe the Earth’s climate system, which originate from outside of the climate system itself, such as variations in solar output.

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24
Q

What are the 6 stages of the natural greenhouse effect

A

1.Incoming solar radiation (insolation) comes in through the Earth’s atmosphere in short-wave radiation.
2. As this short-wave energy passes through the atmosphere it might hit dust particles or water droplets and be scattered or reflected.
3. Only a little short-wave radiation is absorbed in the atmosphere.
4. Solar energy hits the Earth’s surface ,which then absorbs the short-wave radiation and re-emits
long-wave radiation into the atmosphere.
5. Long wave radiation is quite easily absorbed by naturally occurring greenhouse gases in the
atmosphere. Of these, carbon dioxide is by far the most abundant.
6. Some long wave radiation escapes in to space

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25
Q

What is the human enhanced greenhouse effect

A

This is the negative aspect of the greenhouse effect which is the cause of climate change. It is caused by an increased amount of greenhouse gases in the atmosphere which mean that the Earth’s atmosphere absorbs increasingly more heat.

26
Q

What are the mian causes of the enhanced human greenhouse effect

A

Some main causes include the burning of fossil fuels, intensive farming, deforestation and the release of methane from permafrost. There are many severe effects linked to this phenomenon, including increasing natural disasters, changing ocean currents and sea levels and rising temperatures.

27
Q

What country’s contribute most to the human enhanced greenhouse effect

A
  • Countries that are in an industrial stage of development, tend to produce more emissions.
  • More developed countries tend to have a decrease in levels of emissions as they import
    many of their products.
28
Q

What does IPCC stand for

A

Intergovernmental Panel on Climate Change. Dedicated to providing our world with an objective to fight Climate change.

29
Q

What does the IPCC report of 2013 state about the human enhanced greenhouse effect

A
  • It is ‘virtually certain’ that humans are to blame for ‘unequivocal’ global warming.
  • Atmospheric concentrations of greenhouse gases (GHGs) carbon dioxide, methane and nitrous
    oxide are at levels ‘unprecedented in the last 800’000 years’.
30
Q

What is ÉPICA core

A

The European Project for Ice Coring in Antarctica. It is a multinational European for deep ice core drilling in Antarctica. Its main goal is to obtain full documentation climatic and atmospheric record archived in Antarctic ice by drilling and analyzing two ice cores and comparing these with their Greenland counterparts.

31
Q

How far back are we able to collect data of climate change

A

800’000 years of climate evidence: 800’000 years, is how far back we are able to collect data and analyse the climate of our planet. This is doable due to Antarctic ice-core, capturing the CO2 between layers that date back to 800’000 years ago.

32
Q

What is the structure of the atmosphere

A
  • Up to a height of around 80 km, the atmosphere consists of nitrogen (78 per cent), oxygen (21 per cent), argon (0.9 per cent) and a variety of other trace gases such as carbon dioxide, helium and ozone.
  • In addition, there is water vapour and solids (in the form of aerosols) such as dust, ash and soot.
33
Q

What is the ozone layer

A

A layer of Ozone (O3) found mostly in the stratosphere, that absorbs harmful UV rays. CFCs unfortunately react with the ozone layer and can create ‘holes’. These CFCs last in the atmosphere for 100+ years. They were previously used in sprays but are now banned, the only current use of CFCs is in refrigerators and freezers. CFCs also act as a greenhouse gas.

34
Q

What is the slip, slap, slop campaign

A

The campaign used when there was a hole in the ozone layer over Australian and the government wanted more people to be aware and put on sunscreen. This is where you slip on a shirt slop on some sunscreen and slap on a hat. This was used to raise awareness for skin cancer. It was absorbed well by the Australian public.

35
Q

What is global dimming

A

Suspended particulate matter in the atmosphere can reflect solar energy back into space and so have a net cooling effect.

36
Q

How does a volcano eruption create global dimming

A

When a volcano erupts, a large amount of ash can be released into the atmosphere. This ash in the atmosphere blocks energy from the sun and therefore cools the Earth’s lower atmosphere.
○ Mount Tambora erupted in 1815 and ejected 160km2 of ejecta into the atmosphere. This caused what was known as “the year without summer” in 1816.
○ The more orange a sunset, the ‘dirtier’ the atmosphere. After a volcanic eruption it is likely there will be some beautiful sunsets.
This can also be caused by human pollution and is one of the possibilities being considered for geo-engineering.

37
Q

What is a sun spot

A
  • Sunspots are dark areas on the sun where intense magnetic storms are happening, these increase solar output and hence provide greater energy to the earth and heat the atmosphere more.
38
Q

When is there usually an increase in sun spots

A

Every 11 years

39
Q

What is the Maunder minimum

A

A long period of time with almost no sun spots, lasting
from 1645 to 1715. It led to extremely cold conditions where the river Thames was frozen over. → Some people believe it may happen again and it has the potential to cause mass famine as there are many more people living on Earth now compared to Medieval times.

40
Q

What is the Milankovitch cycle

A
  • There are known cycles of the Earth’s orbit around the Sun which affect warming and cooling over long periods of time as incoming levels of solar radiation change.
  • Every 100’000 years the Earth’s orbit changes from spherical to elliptical (approximately), changing the solar input.
  • Over a 41’000 year cycle the Earth’s axis is tilted between 22 and 24.5 degrees, also affecting solar input.
  • Earth’s axis wobbles, changing over a 22’000 year period.
  • When these factors align, leading to less insolation in the northern hemisphere, an ice age can be started (This is estimated to be a cause of alignment between the 22’000 year and 41’000 year cycle rather than the 100’000 year cycle).
  • Ice ages occur approximately once every 100’000 years.
41
Q

What is a cosmic collisions

A

Large asteroids colliding with the Earth may have caused dramatic, though short-lived, climate change in the past. The mass extinction of dinosaurs is thought to have been caused by a large meteor strike 65 million years ago. It’s explosive impact would have thrown up an enormous volume of debris which caused global dimming to such extreme levels that plants would not have been able to photosynthesise for up to 10 years.

42
Q

What is methane

A
  • Methane is a highly powerful greenhouse gas, estimated to be 30x more potent than carbon dioxide.
  • Enormous volumes of methane gas are stored in the Earth’s permafrost regions → The are of which accounts for approximately 1⁄4 of the Earth’s surface.
43
Q

What is permafrost

A

Ground (soil or rock and included ice) that remains at or below 0oC for at least two consecutive years. The thickness of permafrost varies from less than 1m to more than 1.5km.

44
Q

How does the rise in temperature affect the atmosphere in regards to permafrost

A

Unfortunately due to rising temperatures, more of these permafrost areas are melting and hence releasing more methane.
○ One estimate shows that the tundra climate zone has shrunk by about 20% since 1980.
○ According to scientists at NASA, temperatures in Newtok, Alaska, have risen by 4oC
since the 1960’s and by as much as 10oC in winter months.
- This melting can be shown by a positive feedback loop.

45
Q

What is a positive feedback loop

A

Knock on effects in natural systems, which act to accelerate and amplify any changes that have already started to occur. When one element of a system changes, it upsets the overall equilibrium, or state of balance, thereby leading to changes in other elements that reinforce what is happening.

46
Q

What is the albedo effect

A

Lighter colours reflect insolation better than dark colours. This effect helps to keep the earth cool. As the atmosphere warms up, the ice in the poles melts, which means that less sunlight will be reflected, more heat will be absorbed and therefore the ice will melt more. This is an example of a positive feedback loop.

47
Q

What is a terrestrial albedo

A

A measure of the earths albedo, ideally we want high values for this

48
Q

What is the negative feedback loop in terms of the albedo affect

A

When a system adjusts itself in ways that lessen or counteract as the effects of the originals chnage. In this case, feedback has triggered changes in other elements, which act in the oposite directs from the initial chnage. As a result, equilibrium or balance is restored

49
Q

Who are the highest polluters in terms of carbon

A

The highest polluters in terms of carbon output are high and middle-income countries with large populations, including China, the USA, India, Russia, Japan and Germany.

50
Q

Who has the highest data for per capita carbon footprint

A

Data showing per capita carbon footprints reveal a very different pattern, with the highest figures belonging to oil-rich Middle Eastern States, including Qatar and Kuwait.

51
Q

What does the data show about the anthropogenic carbon flow and stock

A

Current data showing the
anthropogenic carbon flow vastly
differs from the anthropogenic carbon stock already in the atmosphere. Germany, for example, may be to blame for 6.9% of all anthropogenic carbon stock, however only accounted for 2.3% of current carbon flow in 2015.

52
Q

How does globalisations and trade need to be considered when talking about carbon emisiones

A

Globalization and trade needs to be considered, many HIC’s claim to have reduced their carbon emissions in recent years, however, falling domestic emissions mask the fact that many developed countries now import much of their food and consumer goods from other countries since deindustrialization and globalization took place. → Some people believe Globalization and trade needs to be considered, many HIC’s claim to have reduced their carbon emissions in recent years, however, falling domestic emissions mask the fact that many developed countries now import much of their food and consumer goods from other countries since deindustrialization and globalization took place. → Some people believe

53
Q

What are Japan’s and germanys carbon emisiones

A

Japan’s emissions have increased significantly as a result of a substantial increase in the use of fossil fuels in power generation following the 2011 Fukushima nuclear disaster. Germany is also phasing out nuclear power but aims to restrict emission rises by adopting renewable energy sources.

54
Q

What is the USAs carbon emisiones

A

The world’s second biggest emitter, generating just under 1⁄5 of all anthropogenic GHGs, despite the population size being less than 5% of the global total. On a per capita basis, the USA still has a carbon footprint 5x higher than China.

55
Q

What are chinas carbon emissions

A

The world’s largest carbon emitter on account of widespread industrialization since the 1970s. A massive programme of poverty alleviation (requiring more, not less, energy) remains the country’s priority. → However China’s leaders want to reduce the rate at which their carbon emissions rise and have made a (non-binding) pledge to reduce the carbon intensity of the country’s growth by adopting more renewable energy into the mix.

56
Q

What is anthropogenic carbon flows

A

The current amount of carbon emission released annually by a country, produced in each nation.

57
Q

What is anthropogenic carbon stock

A

The total size of the store of anthropogenic carbon emissions released into the atmosphere since industrialization began around 1750.

58
Q

What is deindustrilization

A

The loss of traditional manufacturing industries in some high-income countries due to their closure or relocation elsewhere. Since the 1960s, many industries have all but vanished from Europe and North America. Instead they thrive in Asia, South America and, increasingly, Africa.

59
Q

What is a wicked problem

A

A wicked problem is a challenge that cannot be dealt with easily, owing to its scale and/or complexity. Wicked problems arise from the interactions of many different places, people, things, ideas and perspectives within complex and interconnected systems.

60
Q

How does climate chnage present us with a wicked problem

A

Climate change presents us with a wicked problem which - because of its complexity - defies attempts to establish exactly what its effects would be. Unfortunately, this uncertainty is siezed upon by climate change skeptics as a reason to avoid taking any action to reduce GHG emissions.

61
Q

What factors bring greater complexity into climate chnage models

A
  • Other factors can also bring greater complexity to climate chane models, such as ENSO (El Nino Southern Oscillation) and the North Atlantic Oscillation (NAO). → These are independent phenomena that operate naturally on shorter scale, decade-long timeframes. Both phenomena can temporarily bring colder conditions to places that are predicted to get warmer on account of long-term climate change.
62
Q

LOOK AT THE NEGATIVE FEEBACK IN GREENLAND

A