Amounts of Co2 released into the atmosphere as a result of activities by a person, organisation or country
Climate Change
The increasing changes global climate over a period of time
Corrie
A hollow where a glacier started, Corries are also called cirques and cums (hoom)
Drumlin
A long smooth hill shaped like the back of a spoon, created by a glacier
Erratic
A large rock that's different from those around it; it was carried there by a glacier
Emissions
The production of air pollution
Food Miles
A measure of the distance food products are transported from the producer to the consumer
Fossil Fuels
Natural fuels such as coal, oil or gas, formed millions of years by the remains of living organisms
Glacier
A river of ice
Global Warming
The increase in global temperatures due to the increasing amounts of greenhouse
Greenhouse Effect
The warming of the Earth's surface and lower atmosphere due to the presence of greenhouse gases in the atmosphere
Moraine
Material deposited by a glacier
The 3 ways that scientists can measure how the Earth's climate has changed in the past
1. Ocean floor sediment
2. Ice Sheets
3. Tree rings
3 ways that the Earth's climate can change naturally
Changes in the Earth's orbit and axis
Sun Spots
Volcanic eruptions
The ice began a long time ago, during the ice age when there were lowtemperatures and vastsheets of ice covering the planet
The planet began to warm up and the ice ended, but the temperature didn'trisesteadily
About 12,000 years ago
The Vikings were able to explore Greenland and grapes were able to be grown in Britain
Sediment builds upon the ocean floor layer by layer over millions of years
Ocean floor sediment
1. Sediment is drilled and studied using radiometricdating
2. Radiometric dating tells the age of the layer and what the climate was
Ice sheets
Built up in layers from snow
Analysis of the cores shows scientists how much snow fell and the temperature and amount of gases in the air
Tree rings
Tell us the age of trees
If the climate is warm and humid the rings will be bigger
We know about the climate history of the planet through studying oceanfloorsediment, ice sheets, and tree rings
Earth's orbit and axis
Sometimes the orbit is more oval shaped leading to coolertemperatures in the northern hemisphere
During a cycle of average 40,000 years the axis varies from 22.1 to 24.5degrees, the smaller the angle the less icemelts in the northern hemisphere
Sun spots
May cause the sun to give off different amounts of energy
Sun spots
More heat and light
Volcanic eruptions
Huge eruptions blast millions of tonnes of ash into the atmosphere
The ash spreads out blocking the sun for a short amount of time
Gases like Sulphurdioxide which forms a sulphuric acid mist high in the atmosphere absorb sunlight keeping it from reaching the earth
Greenhouse effect
Greenhouse gases form a layer of gases around our planet that stops heat from escaping into space
Greenhouse effect
1. Travels towards the earth
2. About half is absorbed by the earth's atmosphere
3. The rest is absorbed by land and oceans
4. The earth releases some heat towards space
5. Some heat passes through the atmosphere but most is captured by the greenhousegases
Global warming
The process of our planet heating up
Global warming
Increased greenhousegases in the atmosphere
The earth has warmed up by 1degree
Knock-on effect on climates and lots of creatures could find they can't adapt
Carbon dioxide
We breathe it out, but deforestation means plants can't absorb as much, also released by flights, increased car use and coalpowerstations
Methane
Released by animals that chew the cud, swamps, paddy fields, landfillsites and oil and gas
Nitrous oxide
Released by some fertilizers, powerplants, also destroys the ozonelayer
Fossil fuels
When burnt, release carbondioxide and nitrous oxide, also dangerous to transport due to risk of explosions and oilspills, expensive to import, take up a lot of land
Coal
90%carbon, releases the most carbon dioxide, also releases sulphurdioxide
Food miles
The distance travelled by foodproducts between production and consumption
Carbon footprint
The amount of Carbon that you let into the atmosphere each year