Climate Change From The Start Of The Quaternary Period And The Consequences Of Climate Change Flashcards

1
Q

What are glacials

A
  • historic cold periods associated with the build-up of snow, ice, the growth of ice sheets and glaciers
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2
Q

What are inter-glacials

A

Historic warm periods in-between glacial periods where conditions were much the same as today

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3
Q

What and when was the Little Ice Age

A
  • 1300-1870
  • a period of time when parts of Europe and Northern America experienced much colder winters than today
  • coldest periods being 15th and 17th
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4
Q

What were the consequences of the Little ice Age (6)

A
  • The price of grain increased and vineyards in Europe became unproductive
  • Ice land surrounded by sea ice = prevented ships landing and crops were failing = almost half the population left (emigrated)
  • The sea froze around parts of UK
  • regular winter ‘Frost Fairs’ were held on frozen river Thames
  • In Northern Europe, rivers froze and food supplies became limited = famine
  • effects lingered until beginning of 19th century
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5
Q

What and when was the Medieval warm period

A
  • it was associated with an unusual temp rise roughly between 750 and 1350 AD
  • available evidence suggests that at times, som regions experienced temps exceeding those recorded during the period between 1960 and 1990
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6
Q

Where can we find evidence for global warming

A
  • Global temp data
  • Ice cores
  • Tree rings
  • Paintings and diaries
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7
Q

How does the Global temp data show evidence for climate change

A
  • maps produced by NASA by using data collected over 1000 ground weather stations + satellite info
  • there’s a warming trend for most of the world
  • the warming is consistent with earlier maps produced over several decades
  • avg global temps has increased by 0.6’C since 1950 and 0.85’C since 1880
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8
Q

Why might the maps produced by NASA not necessarily be accurate

A
  • weather stations are not evenly distributed across the world and some regions (especially Africa)
  • therefore the maps aren’t absolutely accurate and reliable
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9
Q

How can ice cores be used to show evidence for climate change

A
  • extracted from Antarctic and Greenland
  • when snow falls in polar environments, it builds up slowly, year by year
  • buried layers of snow are compressed and gradually turned into ice
  • scientists can drill to deep ice and extract cylindrical cores from ice, and then dated accurately
  • they date them by analysing the trapped water molecules, then calculating the temp of the atmosphere when the snow fell
  • this info can be used to create graphs from the past 400,000 years —> which show fluctuating temps
  • this indicates past glacial and inter-glacial periods
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10
Q

How thick and old is the Antarctic ice sheet

A
  • 5km thick in some areas
  • the eldest ice at it’s base is thought to be 800,000 yrs old
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11
Q

How do tree rings show evidence of climate change

A
  • every year, the growth of a tree is shown by a single ring
  • if the ring is narrow it indicates a cooler drier year
  • if it’s thicker it means the temp was warmer and wetter
  • these patterns of growth are used to produce tree ring timescales, which give accurate climate info
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12
Q

How do paintings and diaries show evidence for climate change

A
  • Ancient cave paintings of animals in France and Spain depict nature as it was between 40, 000 and 11, 000 years ago, a period of time when the climate change significantly.
  • most evidence from little Ice Age comes from diaries and observations made at the time
  • paintings and drawings of ice fairs and markets on the river Thames when it froze —> indicate Little Ice Age
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13
Q

What is the weakness with paintings and diaries for evidence of climate change

A
  • it’s difficult to date accurately when cave paintings were drawn
  • person accounts can lack objective accuracy
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14
Q

What are some of the natural causes of climate change

A
  • Greenhouse effect
  • Milankovitch cycles (Orbital forcing): Eccentricity, axial tilt, precession
  • Volcanic activity
  • solar forcing
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15
Q

what is the greenhouse effect is

A
  • natural phenomenon
  • maintains 15’C avg temp in lower atmosphere
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16
Q

Explain how the greenhouse effect works

A
  • sun emits short wavelength radiation, greenhouse gases can’t absorb it
  • the earth reflects these wavelengths as long wavelength radiation which the greenhouse gases can absorb
  • They then re-radiate it in all directions-including back towards earth
  • The long wave radiation is thermal radiation, so it results in warming of the surface of the Earth. This is the greenhouse effect
17
Q

Explain how the Milankovitch cycles influence the Earth’s climate

A

—> Eccentricity:
- the Earths orbit
- when it’s more elliptical shaped = warmer periods
- when it’s more circular shaped = cooler periods
- a complete cycle take 100 000 years

—> Axial Tilt
- some parts get more intense solar radiation then others
- A greater degree of tilt = high avg. temp
- tilt of Earth moves back and forth over a period of 41, 000 years

—> Precession
- the Earth’s wobble
- 1 complete wobble takes 26, 000 years
- can cause very long days and very long nights

18
Q

How does volcanic activity influence climate change

A
  • produces Ash and SO2
  • Ash: ash clouds go high into atmosphere = block solar radiation = leading to worldwide cooling for up to 2 yrs
  • SO2: SO2 gas turns into sulphuric acid particles in atmosphere = reflects sun’s rays = reducing solar radiation
19
Q

How does solar forcing influence climate change

A
  • sun spots: dark patches on sun’s surface = indicate higher solar out put
  • sun’s energy output isn’t constant
  • periods when the sun’s activity is high correlates to warm climatic periods
  • periods when the sun’s activity is low correlates to cooler climatic periods
20
Q

What were the causes of the Medieval warming Period

A
  • increase in solar radiation and decrease in volcanic eruptions
  • The increase in solar radiation modified the atmospheric pressure system over the North Atlantic Ocean,
  • which brought warmer and wetter conditions over Northern Europe and most of north-eastern part of North American continent (including Greenland).
21
Q

What were the cause of the Little Ice age

A
  • The weak sun in the 17th Ventura ray coincided with the little Ice Age
  • Throughout the Little Ice Age, the world also experienced heightened Volcanic activity
22
Q

What are the sources of Carbon dioxide

A
  • burning of fossil fuels
  • Deforestation (burning wood)
  • Industrial processes (e.g. making cement)
23
Q

What are the sources of Methane, CH4

A
  • emitted from livestock and rice cultivation
  • decay of organic waste in landfill sites
24
Q

What are the sources of Nitrous oxides, NOx

A
  • vehicle exhausts
  • agriculture and industrial processes
25
Q

What are the social consequences of climate change

A
  • 600 million people live in coastal areas that are less than 10m above sea level
  • people living in vulnerable areas may have to move home or even move to different countries. Some small islands states such as Tuvalu and Vanuatu are particularly at risk
  • people may suffer from increased flooding and storm damage
  • people may lose their jobs, e.g. fishing or tourism, so will have to learn new skills
  • No. of environmental refugees will increase
26
Q

What are the economic consequences of climate change (6)

A
  • Cities like London, New York, Venice may be affected by flooding
  • valuable agricultural land may be lost to sea/polluted by sea water (in areas like India or China)
  • harbours and ports may be affected —> impact on fishing and trade
  • transport systems, such as railways, roads and airports might be damaged or destroyed
  • valuable land and property will need expensive coastal protection measurements
  • countries that depend on coastal tourism as main source of income may have beaches eroded or flooded —> forcing hotels to close and reducing tourism
27
Q

What are the environmental consequences of climate change

A
  • fresh water sources might be contaminated by salty seawater: salinisation
  • damage could occur to coastal ecosystems such as mangrove swamps, which form natural barriers to storms
  • damage to coral reefs by storms and powerful waves will affect fish breeding grounds and ecosystems
  • The IPCC estimates that up to 33% of coastal land and wetlands could be lost in the next 100 yrs
  • Harbours may become blocked by sediment due to increased rates of coastal erosion