Impacts Of Climate Change Flashcards

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1
Q

What is the melting of ice causing and give an example

A

Water stored as ice returns to the oceans

Greenland and Antarctic ice sheets

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2
Q

What does water returning to the oceans mean there is an increase of and what does it lead to
What is this called

A

Volume of the water in oceans increases
Causing sea level to rise
Eustatic sea level change

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3
Q

If all remaining ice sheets were to melt, how much would global sea level increase by

A

60-80 metres

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4
Q

What does increased global temperatures mean and what does it cause

A

Oceans get warmer and expand

Causes thermal expanse which also increases the volume of water leading to further sea level rise

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5
Q

How much could the sea levels rise for an increase in global temperature of 1degrees

A

8-80cm

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6
Q

What is global warming causing

A

Ice to melt
Permafrost to thaw
Other changes in climate

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7
Q

What are prediction of how much sea level will rise in the future like

A

Uncertain and differ a lot

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8
Q

What does IPCC stand for, who are they and what do they do

A

Intergovernmental Panel on Climate Change
Group of scientists
Look at the risks of climate change

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9
Q

What do the IPCC think

A

Sea levels could rise by 18-59cm by the end of the century

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10
Q

Any rise in sea level will have a local/regional/national/global impact
(Which one)

A

Global

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11
Q

Will the impact of sea level rise be the same everywhere

A

It will be greater in some places than others

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12
Q

Explain how sea level rise would affect Bangldesh

A

80% of land area is low lying - any sea level rise will submerge large areas
Would affect lots of people as it has a high population density (1,000 people per km2)
Would be made worse as it is an LIC - vulnerable population with low capacity to cope

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13
Q

Explain how sea level rise would affect the Maldives

A

Extremely low lying set of islands I’m Indian Ocean - rise of 0.5cm would submerge most of the country
Population not poor but economy is dependent on tourism, which would be threaded by sea level rise

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14
Q

What is permafrost

A

Ground that has been permanently frozen for two or more years - covers around 20% of the Earth’s land surface

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15
Q

What are areas of permafrost

A

Natural sinks of CO2

  • stored as organic material in the soil
  • thawing releases some of this, contributing further to global warming
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16
Q

What could thawing of permafrost lead to

A

Buildings to collapse and pipelines on it
-may also bring economic benefits though -eg easier to look for/extract natural resources (fossil fuels) in areas of unfrozen ground

17
Q

What do changes in global temperatures affect

A

Global weather patterns

  1. Increase in frequency of extreme weather events -eg increasing in ocean temperatures may mean an increased risk of tropical cyclones over a wider area
  2. Change in the distribution of climatic regions -eg colder polar regions may shrink and warmer tropical regions may advance to higher latitudes
18
Q

What does a change in global temperature and weather patterns affect

A
The ecology (distribution/abundance of organisms) - species will have to migrate to remain in a sustainable climate, if they cannot migrate they will become extinct
Agriculture -eg some areas become unsuitable for cultivation as climate factors (temperature and the timings of seasons) alter
19
Q

Example of a benefit that regional climate changes may bring to some human activities

A

Economic benefits of tourism where climate has become hotter

20
Q

What are emissions scenarios used for

A

To predict impacts of global warming

21
Q

What is the scientific consensus of what is causing global warming

A

Human factors (eg CO2 emissions)

22
Q

How do scientists try to predict the impact of climate change

A

By predicting how emissions will change in the future

23
Q

What are the emissions scenarios the IPCC have produced

A

Predictions of how human CO2 emissions will change up to 2100

24
Q

What are the scenarios

A

Emissions not increasing much more (scenario 5)
Emissions continuing to grow as they are now (‘business as usual’)
Emissions increasing a lot (scenario 1)
Emissions being controlled by sustainable management strategies

25
Q

What do the IPCC put all the different scenarios into to see how much the climate would change with each scenario eg. how much global temperature will rise

A

Global climate models

26
Q

What will the different scenarios also show other than how the climate would change

A

Different climate changes will cause different impacts eg. different levels of sea level change
Scenario 2: rise by 0.23-0.51m
Scenario 3: rise by 0.21-0.48m
Scenario 4: rise by 0.18-0.38m

27
Q

Reasons why it is difficult to predict the impact of climate change

A

So much uncertainty:
1. Do not actually know how emissions will change, ie. which emissions scenario is accurate
2. Do not know how of the emissions will be absorbed (eg. natural carbon sinks)
3. Extent of climate change due to natural causes (without human influence) is unknown
4. Do not know what climate changes each emission scenario will
cause
5. Do not know what attempts there will be to mange the impacts of climate change or how successful they will be

28
Q

What might combined impacts lead to

A

Tipping point

29
Q

What is the tipping point

A

Where a slight rise in temperature would cause catastrophic and irreversible changes to the environment, creating a much more hazardous world

30
Q

What might the tipping point occur because of

A

May happen because of the positive feedback loop - where a change in climate is speeded up by impacts already caused

31
Q

Example of positive feedback loop

A

Global warming causes melting of Arctic sea ice
As ice melts it leaves darker sea water in its place
Sea water has a lower albedo (amount a surface reflects the Suns radiations) than ice
Therefore more radiation is absorbed by the water
Warm water, then causes more ice to melt, etc

32
Q

Example of combined effect of positive feedback on several of the impacts of global warming

A

Ice melt and the destruction of CO2 sinks, may lead to a tipping point