2.1 - The Causes Of Climate Change Flashcards
Define adaption
Initiatives and measures to reduce the vulnerability of human and natural systems to climate change
Define albeado
The amount of incoming solar energy reflected back into the atmosphere by the earths surface
Define anthropogenic
Human relate processes and impacts
Define the enhanced greenhouse effect
The increasing amount of greenhouse gases in the atmosphere, as a result of human activities and their impact on atmosphere is systems, including global warming
Define global warming
The increase in temperatures around the world that hace been noticed since the 1960s, and particular in the 1980s
Define the greenhouse effect
The process by which certain gases (water vapour, carbon dioxide, methane and chlorofluorocarbons (CFCs)] allow short-wave radiation from the sun to pass through the atmosphere and heat up the Earth, but trap an increasing proportion of long-wave radiation from the Earth. This radiation leads to a warming of the atmosphere.
Define mitigation
Attempts to reduce the causes of climate change.
Define resilience
The ability of a population or a human or natural system to absorb change without having to make a fundamental change.
Define vulnerability
The degree to which a human or natural system is susceptible to, and unable to cope with, the adverse impacts of climate
What is the atmosphere
The atmosphere is an envelope of mixed gases which is held in place by gravitational attraction
What makes up the atmosphere
It consists of nitrogen (78%), oxygen (21%), and 1% trace gases
What are the 4 layers of the atmosphere
- Thermopylae
- Mesopause
- Stratopause
- Tropopause
What is the atmospheric layers
The atmosphere is 10,000 km in height
But gravity compresses 99% of the atmosphere to within 40 km of the Earth’s surface
50% of the atmosphere is in the first 5.6 km
What is the atmosphere heat budget
The Sun is Earth’s primary source of energy
It provides more energy in an hour than humans use in a year
Energy is received as short-wave radiation - insolation
What does the atmospheric heat budget depend on
The balance between isolation and outgoing long wave radiation
Where is energy lost when its passing through the atmosphere
Some energy is lost passing through the atmosphere, but there is an overall net gain of energy at the surface
Do polar regions have a net gain or deficit of energy and what causes it
Polar regions have a net deficit (they receive about 24% of insolation) due to absorption, reflection and scattering – albedo effect
Does the overall atmosphere have a net deficit or gain of energy
The atmosphere itself has an overall net deficit of energy
What is the neutral greenhouse affect and how does it reflect the atmospheres net deficit of energy
To compensate, heat is moved from the surface to the atmosphere by radiation, conduction and release of latent heat – the natural greenhouse effect
Define climate chnage
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, temperature etc…)
What are the 2 main reasons for climate chnage
- changing concentrations of green house gases
- various kinds of external forces
Define green house gases
The atmospheric gases that absorb infrared radiation and cause world temperatures to be higher than they would otherwise be.
Define external forces
A term used to describe the Earth’s climate system, which originate from outside of the climate system itself, such as variations in solar output.
What are the 6 stages of the natural greenhouse effect
1.Incoming solar radiation (insolation) comes in through the Earth’s atmosphere in short-wave radiation.
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 absorbed in the atmosphere.
4. Solar energy hits the Earth’s surface ,which then absorbs the short-wave radiation and re-emits
long-wave radiation into the atmosphere.
5. Long wave radiation is quite easily absorbed by naturally occurring greenhouse gases in the
atmosphere. Of these, carbon dioxide is by far the most abundant.
6. Some long wave radiation escapes in to space