Mapa mental
Changing Climate
Contenido del mapa
Changing Climate
Past Climate Change
- Know has changed in past by...
- Fossils of animals and plants that no longer exist
- Evidence of Glaciation in now ice free regions
- Evidence of rocks showing climate conditions when the rocks were formed
- Evidence from ice cores in Greenland and Antarctica showing how much CO2 was in the atmosphere
- In the past 400,000 years there has been a Quarternary period.
- Temperatures varied 1.5 degrees either side of the average
- This small change makes a huge difference in what can be grown
- Temperatures varied 1.5 degrees either side of the average
- Know has changed in past by...
Causes of Climate Change
- Volcanic Eruptions
- Large eruptions emit vast quantities of dust
- Emitting gases such as sulphur dioxide into the atmosphere
- This blocks out or absorbs solar radiation, so the Earth cools.
- Emitting gases such as sulphur dioxide into the atmosphere
- Large eruptions emit vast quantities of dust
- Sunspot activity
- Sunspots are darker areas on the sun's surface
- They are a sign if greater solar activity
- They come and go in 11 year cycles
- However, they have been observed in longer periods such as 1645-1715
- A period which coincides with the Little Ice Age
- However, they have been observed in longer periods such as 1645-1715
- They come and go in 11 year cycles
- They are a sign if greater solar activity
- Sunspots are darker areas on the sun's surface
- Changes in Earth's orbit and rotation
- The shape of the earth's orbit changes
- It becomes more or less circular
- This happens over 100,000 year periods, known as Orbital Eccentricity
- The Earth wobbles on its axis over 26,000 years, known as precession.
- The tilt of the axis varies between 21-24 degrees over 40,000 years
- When used together these effects change the amount of solar energy the Earth's surface receives
- The tilt of the axis varies between 21-24 degrees over 40,000 years
- The Earth wobbles on its axis over 26,000 years, known as precession.
- This happens over 100,000 year periods, known as Orbital Eccentricity
- It becomes more or less circular
- The shape of the earth's orbit changes
- Volcanic Eruptions
Little Ice Age
- Approx 1300-1870,
- Approx 1 degree lower average temperature than today.
- Impacts
- The Baltic Sea froze over in winter
- Many other rivers in Europe did the same.
- Sea Ice from the North reached as far south as Iceland
- Winters were much colder and longer
- This reduced the growing season dramatically
- Led to widespread crop failure and famine
- The price of grain increased everywhere
- Leading to social unrest and revolt
- The price of grain increased everywhere
- Remote areas abandoned
- Such as Greenland, as survival became impossible
- Glaciers advanced in the Alps and Northern Europe
- Overran towns and farms
- The Baltic Sea froze over in winter
- Approx 1300-1870,
Megafauna and the Ice Age
- 10,000-15,000 years ago the Ice Age ended
- Temperatures rose as much as 5 degrees
- Many megafauna disappeared completely.
- It was a mass extinction event
- EG: Mammoths, Sabre-tooth tigers and giant beavers became extinct.
- WHY?
- Their preferred food disappeared so they died out.
- Humans hunted them
- We know this from evidence from remains
- WHY?
- EG: Mammoths, Sabre-tooth tigers and giant beavers became extinct.
- It was a mass extinction event
- Many megafauna disappeared completely.
- Temperatures rose as much as 5 degrees
- 10,000-15,000 years ago the Ice Age ended
UK Climate today
- UK has a maritime climate
- Is mild and wet
- Precipitation every month of the year
- Low average temperatures in winter but never below freezing
- Summers are warm but not hot
- WHY?
- Prevailing South-Westerly winds produce precipitation
- Surrounding seas reduce summer temperatures
- Make winters mild
- Gulf Stream current brings warm water across the Atlantic, warming the air
- 5 main air masses
- Polar Maritime is wet and cold, causing cold and showers from the Greenland Arctic sea.
- Arctic Maritime ic wet and cold, causing snow in winter from the Arctic
- Polar Continental is cold in winter, hot in summer, causes snow in winter and dry in summer, from Central Europe.
- Tropical Continental is hot and dry, causing dry summers from North Africa
- Tropical Maritime is warm and moist, causing clouds, rain and mildness, from the Atlantic
- UK has a maritime climate
Greenhouse Effect
- Greenhouse gases retain heat from the sun
- Without them the planet would be too cold to sustain life
- Solar energy passes through the atmosphere without an effect
- 1/2 is absorbed by the Earth. The rest is reflected back by the cloud or upper atmosphere into space
- The other half is absorbed by the ground and radiated into the atmosphere
- Some is trapped by greenhouse gases
- The other half is absorbed by the ground and radiated into the atmosphere
- 1/2 is absorbed by the Earth. The rest is reflected back by the cloud or upper atmosphere into space
- Solar energy passes through the atmosphere without an effect
- Without them the planet would be too cold to sustain life
- Greenhouse gas emission is increasing due to industrial revolutions
- EG: Deforestation produces CO2
- Reducing trees lowers Earth's ability to absorb CO2
- Is predicted to heat the Earth too hot to survive in by 2090
- EG: Deforestation produces CO2
- Greenhouse gases retain heat from the sun
Impacts
- Sea levels rise due to melting ice caps
- Cause floods
- Developed countries
- New species migrate
- Increased storminess increases erosion
- Costs pf protecting low lying areas
- Costs to NHS due to heatwaves
- Domestic tourism increases
- More frequent floods
- Farmers have to alter crops to suit climate
- Developing Countries
- Rising sea levels erode swamps
- Areas more prone to drought
- Flooding more common
- Rising sea levels cause land loss
- Water shortages could lead to famine
- Sea levels rise due to melting ice caps
Información
- Descripción
- GCSE Geography Mapa Mental sobre Changing Climate, creado por Lambylittle el 07/04/2014.
- Creado por
- Lambylittle
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