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Higher Global Climate Change

by Mr Bell

Pages 2 and 3 of 37

Global Issues 1
GLOBAL CLIMATE CHANGE
Higher Geography
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Global Climate Change
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Physical causes

Human causes

Local and Global effects

Management strategies and their limitations 
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Physical Causes
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1.Variations in Energy Emissions from the Sun

2.Variations in the Orbit & Movement of the Earth

3.Variations in Volcanic Activity

4.Variations in Ice Caps
Variations in Energy Emissions from the Sun
Solar activity: variations in solar energy and sun spot activity can alter global temperatures. Scientists have shown that variations in sun spot activity follow an 11-year pattern. 
Variations in the Orbit & Movement of the Earth
Milankovitch’s theory: changes in the Earth’s orbit and tilt alter the amount of energy reaching the Earth. When there is less energy reaching Earth during the Northern Hemispheres' Summer ice will last longer increasing the Albedo effect. This is because most of the Earth land in is in the Northern Hemisphere.
Milankovitch Cycles
Eccentricity
This is the change in the shape of the earth's orbit around the sun. 
Over time the Earth will be closer to, or further away from the Sun altering the amount of energy we receive.
Occurs over 97,000 years.
Milankovitch Cycles
Axial Precession
This is a change in how close the Earth is to the Sun when Summer occurs. When the Earth is further away from the Sun in our Summer (Northern Hemisphere) we have cooler summers allowing snow to last for longer and possibly develop into glacial ice. This increases the Albedo effect.
Occurs over a 23,000 year cycle.
Milankovitch Cycles
Axial Tilt
The less the tilt the less the variation in Summer and Winter temperatures.
This will make Summers less warm and will encourage snow to last longer forming glacial ice.
Occurs over 41,000 years.
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