Natural hazards Flashcards
(138 cards)
What are the greenhouse gases?
- carbon dioxide (CO2)
- methane (CH4)
- nitrogen oxides (NOx)
- water vapour (H2O)
Greenhouse gases allow
our atmosphere to trap heat near to the planet
All of the heat on the surface of our planet comes from
solar radiation
Infra-red radiation
It warms our planet
The natural greenhouse effect
- Infra-red radiation
- When it gets closer to our planet, some of it goes to space.
- When infra-red radiation hits a surface of our planet, there is heat.
- Some of the infra-red radiation can get back out into our atmosphere and off into space but greenhouse gases trap heat near to the surface of our planet - keeps some of our heat in.
- It is why our planet stays warm
- It is a natural effect.
- The greenhouse effect keeps the Earth naturally warm anough to support life. It works like a glass greenhouse by:
- greenhouse gases (eg: water vapour, carbon dioxide, methane and nitrous oxides) trapping heat that would otherwise escape into space
- allowing short-wave radiation (light) from the Sun through to the Earth.
- Trapping some of the longer wavelength radiation (heat) that would otherwise be radiated back into the atmosphere.
Human causes of climate change
- power generation
- factories
- transport
-farming practices/ agriculture (methane) - manufacturing
- domestic reasons
- We are artificially changing the composition of the earthโs atmosphere.
To do this, you have to burn fossil fuels- coal, oil or natural gas.
Our climate
Our climate is changing quite rapidly because our planet is getting warmer
By how much has the temperature of earth risen?
1 degrees Celsius
Climate change
Our climate has become more unpredictable.
the enhanced greenhouse effect
- we are adding more greenhouse gases into the atmosphere. The atmosphereโs composition is changing.
- Atmosphere is better at trapping heat, struggled to let some of the infra-red radiation out. Creates heat for a lot longer. Planetโs temperature will very slowly and gently rise.
- In recent years the amounts of greenhouse gases in the atmosphere have increased. Scientists believe that this enhanced greenhouse effect is due to human activities.
natural causes of climate change
- solar activity (sunspots)
- volcanic activity
- Milankovitch Cycles
Solar activity
- The sun goes through different stages in its lifespan
- parts of the surface of the sun have sunspots- about 2000 degrees colder than the normal temperature of the sun.3500 degrees. If the earth passes in front of one of these sunspots, there may be a small period in which the earth was colder- lowers solar activity-less energy/ infra-red radiation from sun.
- The surface of the Sun has dark patches called sunspots which mark short-term regions of reduced surface temperature. They are usually accompanied by explosive, high-energy solar flares increasing heat output. Over a period of around 11 years, sunspots increase from a minimum to a maximum, and back again.
volcanic activity
- volcanic eruptions can cause the earth to get warmer or colder
- volcanoes release ash. If ash gets up into the atmosphere- blocks infra-red radiation coming towards our planet- cooling effect on overall temperature by 2 or 3 degrees- short-term impact.
- can release lots of carbon dioxide. Carbon dioxide has a warming effect
- Sulphur dioxide is also blasted out which converts to droplets of sulphuric acid, and acts like mirrors to reflect solar radiation back into space. This longer-term impact (over many years) also reduces temperatures.
Milankovitch cycles
- 3 ideas about the way the earth goes around the sun. Interesting ways that the earth changes its orbit around the sun.
1, Eccentricity- the earth doesnโt always orbit the sun in a circular shape.
2, Precession- the wobble of the tilt around the core
3, Obliquity/ tilt-
It is not always the same distance from the sun.
Evidence for climate change
- if glaciers/sea ice are melting back further and further
- rising sea levels - warmer
- icicle drilling- drill deep down into ice sheets in antarctica- tiny bubbles to see the composition of the atmosphere thousands of years ago- ice cores
- paintings/writing from hundreds/ thousands of years ago
- Tree rings - how well they were growing- to see what the climate was like
definition of climate change
It refers to the long-term shifts in temperature and weather patterns, mainly caused by human activities, especially the burning of fossil fuels.
Milankovitch cycles are
Three distinct cycles which increase (cooling) or decrease (warming) the distance from the sun.
Eccentricity
Every 100,000 years or so the orbit changes from almost circular, mildly eliptical (oval and back again). This can lead to changes in the Earthโs temperature.(This causes changes in our season or long-term climate).
Axial tilt/ obliquity
Every 41000 years the tilt of the Earthโs axis moves back and forth between 21.5 degrees and 24.5 degrees. The difference in angle (normally 23.5 degrees) affects temperature on the planet.
Glycoscopic precession
Over a period of around 26000 years the axis wobbles from one extreme to the other.
Carbon dioxide (enhanced greenhouse effect)
- Carbon dioxide is the most important, contributing approximately 60% to the net warming by greenhouse gases
- Most carbon dioxide comes from burning fossil fuels in industry and power stations. Transport and farming also contribute
- Deforestation of tropical rainforests by burning is another major source.
Methane (enhanced greenhouse effect)
- CH4 emissions from ever- increasing numbers of farm livestock, rice farming, sewage treatment, and emissions from landfill sites, coal mines and natural gas pipelines are growing even faster than CO2.
Alternative energy
- eg: Lesotho Highland Water project
- not really done in LICs
- HICs it is done
- The UK aims to produce half of itโs electricity from renewable sources
- The burning of fossil fuels accounts for 87% of all carbon dioxide emissions.
- Alternative sources of energy represent sustainable, low carbon alternatives.
Carbon capture
- not yet economically viable
- It uses technology to capture CO2 that is produced by burning fossil fuels in electricity generation and industrial process. Once captured, the CO2 is compressed, piped and injected underground for long-term storage in suitable geological reservoirs, such as depleted oil and gas wells.