Climate Change Flashcards
(36 cards)
Evidence for Climate Change: Ice Cores
Scientists take long samples of ice out of ice sheet + analyse gases that are in there by inspecting bubbles, deeper ice in ice sheet, older it is, trapped air contains record of carbon dioxide + methane levels at time, more carbon dioxide there is, then warmer it was + vice versa
Evidence for Climate Change: Tree Rings
Scientists look at tree rings to determine what climate was like before, small rings means growth was slow + vice versa, counting rings determines age of tree, trees grow wider rings when season is long + vice versa
Evidence for Climate Change: Fossils
Palaeontologists can identify similarities between fossil remains + animals that are living today, if fossils found are different to animals that live today, then it’s likely that climate was different in past
Evidence for Climate Change: Old Paintings and Diary Entries
Old Paintings can visually show us what climate was like + diary entries can describe what climate was like
Evidence for Climate Change: Yearly Events ‘Natures Calendar’
Seasonal shift, when season lasts for either shorter or longer than it should have is evidence of climate change
Evidence for Climate Change: Landforms
Depending on landscape, landforms are created e.g valley means that there was river there before, glaciers that existed in very cold climates also carve out landscapes, leaving behind U-shaped valleys
Natural causes of climate change: Milankovitch Cycles
Eccentricity, Obliquity + Precession
Eccentricity
Describes path of Earth as it orbits Sun - not fixed, every 100,000 years it changes to either circle or oval shape of orbit
Obliquity
Tilt of Earth, Earth spins on its axis, causing night + day, angle changes every 41,000 years, tilt axis is between 24.5º - 22.5º, average angle is 23.5º, larger angle, more Northern Hemisphere is turned towards sun + vice versa
Precession
Describes natural ‘wobble’ rather than spinning top, accounts for certain regions of world e.g Northern Hemisphere, experiencing very long days + very long nights at certain times of year, happens every 26,000 years
Natural causes of climate change: Sunspots
Dark patch that appears from time to time on surface of Sun, ‘Sunspot Cycle’, when sunspot activity is at its maximum, Sun gives off more heat, large explosions occur on surface of Sun, resulting in solar flares, when sunspot activity is at its minimum, solar output is reduced, leading to lower temperatures
Sunspot Cycle
Number of sunspots increase from minimum to maximum over 11 years
Natural causes of climate change: Volcanic Activity
Violent volcanic eruptions blast huge quantities of ash, gases + liquids into atmosphere, volcanic ash can block out Sun, reducing temperatures on Earth, normally short-term impact, fine droplets that from from conversion of sulphur dioxide to sulphuric acid act like tiny mirrors reflecting radiation from Sun, last lot longer + can affect climate for many years
Volcanic Winter
Cooling of lower atmosphere + reduction of surface temperatures
Human causes of Climate change: Greenhouse effect
Atmosphere allows most of heat from Sun (short-wave radiation) to pass straight through it to warm up Earth’s surface, when Earth gives off heat in form of long-wave radiation, some gases e.g CO2 + methane are also able to absorb it, keeps Earth warm, without this ‘blanketing’ effect it would be far too cold for life to exist on Earth
Greenhouse gas
Gas that is able to absorb long-wave radiation e.g carbon dioxide or methane
Human causes of Climate change: Carbon Dioxide
Accounts for estimated 60% of enhanced greenhouse effect, sources: deforestation + burning wood, burning fossil fuels in industry + power stations to produce electricity e.g oil, coal + gas, car exhausts,
Human causes of Climate change: Methane
Very effective in absorbing heat, accounts for 20% of enhanced greenhouse effect, sources: rice farming, burning biomass for energy, farm livestock e.g cows, decaying organic matter in landfill sites + compost tips
Human causes of Climate change: Nitrous Oxides
Very small concentrations in atmosphere, but are up to 300 times more effective in capturing heat than carbon dioxide, sources: sewage treatment, power stations producing electricity, car exhausts, agricultural fertilisers
Greenhouse Effect
When atmosphere traps heat from Sun, which keeps Earth warm, more heat leaves atmosphere than in enhanced greenhouse effect
Enhanced Greenhouse Effect
Same as greenhouse effect just more heat is trapped in atmosphere as there are more greenhouse gases produced by humans in atmosphere, so less of Sun’s energy is leaving Earth’s atmosphere, increasing average atmospheric temperature, caused by humans
Climate Change
Long-term change in Earth’s climate, especially change due to increase in average atmosphere temperature, causes natural events to be more extreme
Changes in agricultural systems: Low-latitudes (Adaptation)
Scientists think that greatest change to agriculture will occur in low-latitudes, Southern Africa’s maize crop could fall by 30% by 2030 + production of rice in South Asia could fall by 10%
Changes in agricultural systems: Mid-latitudes (Adaptation)
Warmer climate in Europe + North America could lead to increase in production of certain crops e.g wheat, in UK, Mediterranean crops e.g vines + olives may thrive in future