Climate Change From The Start Of The Quaternary Period And The Consequences Of Climate Change Flashcards
What are glacials
- historic cold periods associated with the build-up of snow, ice, the growth of ice sheets and glaciers
What are inter-glacials
Historic warm periods in-between glacial periods where conditions were much the same as today
What and when was the Little Ice Age
- 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
What were the consequences of the Little ice Age (6)
- 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
What and when was the Medieval warm period
- 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
Where can we find evidence for global warming
- Global temp data
- Ice cores
- Tree rings
- Paintings and diaries
How does the Global temp data show evidence for climate change
- 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
Why might the maps produced by NASA not necessarily be accurate
- weather stations are not evenly distributed across the world and some regions (especially Africa)
- therefore the maps aren’t absolutely accurate and reliable
How can ice cores be used to show evidence for climate change
- 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
How thick and old is the Antarctic ice sheet
- 5km thick in some areas
- the eldest ice at it’s base is thought to be 800,000 yrs old
How do tree rings show evidence of climate change
- 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
How do paintings and diaries show evidence for climate change
- 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
What is the weakness with paintings and diaries for evidence of climate change
- it’s difficult to date accurately when cave paintings were drawn
- person accounts can lack objective accuracy
What are some of the natural causes of climate change
- Greenhouse effect
- Milankovitch cycles (Orbital forcing): Eccentricity, axial tilt, precession
- Volcanic activity
- solar forcing
what is the greenhouse effect is
- natural phenomenon
- maintains 15’C avg temp in lower atmosphere