Physical Geography & Supply
Physical geography and supply
The following physical factors affect the production of energy in different parts of the world in a variety of ways:
- Climate
- Geology
- Drainage
Table of Physical Factors Affecting Supply of Energy
Factor |
Explanation: how this influences energy supply |
Examples |
|
Climate |
Sunshine hours and intensity |
Where solar insolation is high - high angle of sun and longer hours of daylight - solar energy is an effective renewable energy option |
Solar power is highly productive in California, southern Spain, north Africa and the Middle East |
Wind strength |
Strong prevailing winds blowing in upland or open spaces allows for effective use of wind turbines Global wind energy has grown rapidly in the last twenty years uplands facing prevailing winds and a large, shallow continental shelf for offshore wind turbines where the wind is more consistent. |
The UK can exploit wind energy It has consistent prevailing winds blowing onto the west of the island And a shallow continental shelf allowing offshore wind farms |
|
Precipitation |
HEP schemes tend to be built in areas with high amounts of rain or snow Exotic rivers have sources in upland areas of high precipitation but then later flow through arid regions. These can produce sufficient flows downstream to allow for HEP despite surrounding precipitation levels being low. |
The Dinorwig HEP scheme, in North Wales, is the largest scheme of its kind in Europe and built in an area that receives more than 1500mm of average rainfall per year The Aswan High Dam HEP scheme was built in an arid area of Egypt with an average precipitation of 10mm per year, but is fed by the exotic river Nile |
|
Biomass growth |
Tropical climates encourage fast plant growth and suitable growing conditions for sugarcane, used in bio-ethanol production |
Around 70% of Brazil’s renewable energy supply and 25% of its transport fuel is from biomass - one of the highest ratios in the world |
|
Geology |
Fossil fuel rock structure |
Fossil fuels rely on certain geological conditions to form. Coal seams form from fossilised and buried ancient swamp forests Oil and natural gas form when decomposed marine organisms are trapped between layers of impervious rocks within anticlines |
Much of Britain contains coal seams and natural gas and oil fields remain in exploitable conditions in the North Sea |
Geothermal crustal structure |
There is potential for geothermal energy where the earth’s crust is thin so that magma is nearer the surface |
New Zealand, Iceland and Japan all have relatively thin crusts. 90% of all homes in Iceland are heated by geothermal energy |
|
Tectonic plate structure |
The stability and safety of energy schemes built on active tectonic plate margins can make them risky, particularly with HEP and nuclear power |
Until 2011, Japan was generating 30% of electricity from nuclear reactors but following the 2011 earthquake and tsunami that resulted in radioactive leaks from the Fukushima plant, the country’s nuclear energy plan has been reassessed |
|
Drainage |
Freshwater abstraction |
Water from river networks support a range of energy schemes. For example thermal power stations use large amounts of water to produce the steam that turns the turbines. Nuclear reactors require cooling from a water supply. Most fossil-fuel and nuclear power stations are situated on major rivers for a constant supply. |
Drax power station, in North Yorkshire, UK was once Western Europe’s largest coal-fired power station and used water from the River Ouse. In 2012 it was converted into the UK’s largest generator of renewable biomass electricity |
Dam construction |
Drainage basins containing deep and steep-sided valleys, with a reliable supply of river flow, provide good conditions for dams and HEP |
The Aswan High Dam was chosen as a location due to the steep-sided valley and huge river discharge of the river Nile at that point |