2.1 Causes of climate change Flashcards
Define climate change
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).
What are greenhouse gases?
Atmospheric gases that absorb infrared radiation and cause world temperatures to be warmer than they would otherwise be.
Define external forcing
A term used to describe processes that impact Earth’s climate system, which originate from outside of the climate system itself, such as variations in solar output.
What are the two reasons why climate change can occur?
-Changing concentrations of greenhouse gases
-External forcing
Explain how changing concentrations of greenhouse gases can lead to climate change
-Changing concentrations of greenhouse gases (carbon dioxide, methane and nitrous oxide) affect temperature.
-These greenhouse gases (GHGs) allow sunlight to pass through Earth’s atmosphere but trap the heat that is radiated back towards space (short-wave sunlight is absorbed when it hits the ground, or water, and is later re-emitted as long-wave infrared heat radiation).
-If the concentration of GHG rises above its naturally occurring level, this is the climatic equivalent of putting extra blankets on a bed.
-More heat is retained, resulting in a warmer, more energetic and less predictable climate system.
What would the Earth’s temperature be without GHGs?
-18°C (too cold for life to have evolved)
Explain how external forcing can lead to climate change
-Various kinds of external forcing may occur.
-This means the amount of sunlight reaching Earth is reduced or increased.
-This may be because of changes in the Sun’s activity or Earth’s distance from the Sun, for instance.
-Any such change in the global energy balance results in a fall or rise in global mean surface temperature (GMST).
Diagram showing the greenhouse effect
Explain the greenhouse effect (take from other deck?)
1) Solar energy enters the atmosphere.
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 abosrbed in the atmosphere.
4) Solar energy heats the Earth’s surface, which then radiates long-wave (heat) energy into the atmosphere.
5) Long-wave energy is quite easily absorbed by naturally-occuring greenhouse gases in the atmosphere. Of these, carbon dioxide is by far the most abundant.
6) Some long-wave energy escapes into space.
What are the different pieces of evidence of naturally-occuring climate change over time?
-Fossil and geological records
-Landscape evidence
-Tree rings
-Agricultural records
Explain how fossil and geological records can give evidence about naturally-occuring climate change
-Fossils, sedimentary rocks and sediments (containing pollen grains) offer clues about environmental changes over time.
-The geologically recent appearance and later disappearance of woolly mammoths in what is now Europe indicates that periods of cooling and warming occurred in the past.
Explain how landscape evidence can give evidence about naturally-occuring climate change
Evidence for past sea-level changes is provided by raised beaches (landforms which show sea level used to be higher than it is today) and drowned valleys called rias and fjords. From these, we surmise that Earth’s ice caps have changed size, along with the volume of water stored in oceans.
Explain how tree rings can give evidence about naturally-occuring climate change
-Trees produce one new ring of growth per year, during the growing season.
-A warmer year results in a wider ring.
-Patterns of slower and faster growth can be observed that allow us to estimate temperatures in the past.
Explain how agricultural records can give evidence about naturally-occuring climate change
-Historical grape harvest dates have been used to reconstruct summer temperatures in Paris, France, from 1370 to 1879.
-These contribute to our understanding of the so-called ‘Little Ice Age’ (a relatively cold phase from around 1300 to 1850) and the ‘medieval warm period’ (900–1300) that preceded it.
In addition to explaining why world temperatures have sometimes risen or fallen, ___ help determine the strength and duration of any changes.
Positive and negative feedback processes
What are positive feedback loops?
-They are 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.
What are negative feedback loops?
-These occurs when a system adjusts itself in ways that lessen or cancel out the effect of the original change.
-In this case, feedback has triggered changes in other elements, which act in the opposite direction from the initial change.
-As a result, equilibrium or balance is restored.
Diagram of a positive feedback loop showing a possible way the climate system could respond to more carbon dioxide being added to the atmosphere (for example, as a result of fossil fuel use).
The first scenario suggests accelerated warming as various system changes take place, which strengthen one another.
Diagram of a negative feedback loop showing a possible way the climate system could respond to more carbon dioxide being added to the atmosphere (for example, as a result of fossil fuel use).
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Which is more concerning for scientists: positive or negative feedback loops?
-There is widespread concern among the world’s climate scientists that positive feedback effects associated with human emission of carbon dioxide will be far greater than negative feedback effects in the coming decades.
-As a result, there is a significant risk of a high rise in GMST (of 4–6°C) occurring by 2100.
What are the different reasons for variations in solar radiation?
-Volcanic emissions and global dimming
-Changes in solar output
-Changes in the Earth’s orbit
-Cosmic collisions
Explain how volcanic emissions and global dimming can be a reason for variations in solar radiation
-Major past volcanic eruptions have led to a short-lived period of global cooling lasting for one or two years only.
-This is because of ash and dust particles being ejected high into the atmosphere, blanketing Earth and reducing incoming insolation.
-Mount Pinatubo’s 1991 eruptions caused global temperatures to drop temporarily by about 0.5°C.
Explain how changes in solar output can be a reason for variations in solar radiation
-A variety of output cycles have been detected in the amount of energy emitted by the Sun.
-The most obvious of these is an 11-year sunspot activity cycle.
-Sunspots are dark areas where intense magnetic storms are happening, which increase solar output.
-A long period with almost no sunspots lasting from 1645 to 1715 is called the Maunder Minimum.
-It has been linked to the cooler conditions that existed during the Little Ice Age.
Explain how changes in the Earth’s orbit can be a reason for variations in solar radiation
-Three known cycles occur in Earth’s orbit around the Sun, resulting in warming and cooling over long periods of time as incoming levels of solar radiation change.
-Firstly, every 100,000 years, Earth’s orbit changes from spherical to elliptical, changing the solar input.
-Secondly, Earth’s axis is tilted at 23.5 degrees, but this changes over a 41,000-year cycle by between 22 and 24.5 degrees, also affecting solar input.
-Thirdly, Earth’s axis wobbles, changing over 22,000 years, bringing further climate change.
-These orbital cycles are usually termed Milankovitch cycles (the theory of astronomical climate forcing was developed by Milutin Milankovitch).
Explain how cosmic collisions can be a reason for variations in solar radiation
-Large asteroids colliding with Earth may have caused dramatic, though short-lived, climate change in the past.
-The mass extinction of the dinosaurs is thought to have been caused by a large meteor strike 65 million years ago.
-Its explosive impact would have thrown up an enormous volume of debris.
-A vast dust cloud may have blocked sunlight and prevented photosynthesis for up to 10 years.
-This would have been long enough for the food chains that sustained the dinosaurs to collapse entirely.
Define global dimming
-Suspended particulate matter in the atmosphere can reflect solar energy back into space and so have a net cooling effect.
-This phenomenon can occur naturally because of volcanic emissions but can also be caused by human pollution too – meaning that fossil fuel burning may be both warming and cooling the planet at the same time.
Graph showing the ineratction between the three Milankovitch cycles
Explain the albedo effect
-During periods when Earth has grown warmer in the past, temperature changes may have accelerated because of the loss of ice cover.
-Ice has a high albedo of around 80 percent, which means it reflects four-fifths of all incoming solar radiation.
-If some white-colored sea ice melts in the Arctic, for instance, darker-colored water will be revealed.
-The water has a lower albedo because of its dark color and, consequently, it absorbs more heat.
-As it warms, the water becomes more likely to melt any remaining sea ice.
-This results in the opening up of more areas of the open ocean, and so the process repeats.
-When the water grows warmer, so too do the air masses that are in contact with it.
-The result is accelerated warming of the atmosphere.
Define albedo
-How much solar radiation a surface reflects.
-White surfaces have the highest albedo, or reflectivity.
How can a positive feedback loop exacerbate the albedo effect?
-This positive feedback process means that even a small change in sea ice coverage can have a significant impact on global climate potentially.
-In theory, even a small reduction in sea ice cover could lead eventually to an ice-free Arctic.