Deals with the interests of those who own raw materials, those who work and those with wealth
Socio-cultural dimension
Looks at how different groups of people in society interact, how they treat each other and how they care for each other
Political dimension
Deals with the division of power. What is the role of government, big companies and interest groups when decisions are made?
Physical dimension
Looks at a subject from the interests of nature. The effects on nature often have an impact on human lives
Physical dimension
Scarcity of raw materials
Climate change
Tropics (or tropical zone)
The zone at the equator where it is warm all year round
As you go towards the poles
It gradually gets colder
Tropic of Cancer
The circle of latitude at 23 1/2°N where the tropical zone ends and the temperate zone begins
Tropic of Capricorn
The circle of latitude at 23 1/2°S where the tropical zone ends and the temperate zone begins
Temperate zone
The zone between the circles of latitude at 23 1/2° and 66 1/2°, where it is not too hot and not too cold
Subtropics
The part of the temperate zone that is nearest to the tropics, where the average temperatures are less hot than the tropics but still hotter than the rest of the temperate zone
Polar regions (or polar zone)
The regions that begin at the circles of latitude at 66 1/2°N and 66 1/2°S, where the days are long in summer and short in winter
Polar circles
The circles of latitude at 66 1/2°N and 66 1/2°S
The Earth's surface is 29% land and 71% water
The Sun's rays fall either on land or on water
Temperature difference
If the Sun's rays are absorbed by land or by water
Land
Warms up and cools down in a different way to water
Beach on a summer's day
Sand can be so hot that it hurts your feet
Seawater is much cooler
Evening on the beach
Sand has cooled down quite a lot
Temperature of the sea has not changed
Land surface warms up faster than the sea or ocean, but also cools off faster
Difference in warming up and cooling down
Influences the temperature of the air above land and sea
Air temperature above the sea
Never be very high or very low
The sea has a moderating effect on the temperature
Air temperature above land
Can get very warm and also very cold
The temperature can also change very quickly
Onshore and offshore winds
When wind hits a mountain range
It can only go in one direction: up
Relief rainfall
Precipitation caused when rising air is pushed against a mountain
Windward side
The side of a mountain that faces the wind
Moist air is pushed upwards, cools down and brings rain
Leeward side
The other side of the mountain that's out of the wind
The air on that side goes down and gets warmer
Little or no precipitation
Rain shadow
The area behind the mountain range
We call the rain that falls at the equator convectional rainfall
thelithosphere: the hard and solid land mass called the Earth’s crust and underneath
the hydrosphere: the Earth’s waters
the biosphere: life on Earth
The subtropical zone (or subtropics) is a transitional area between the temperate and tropical zone.
The boreal zone is a transitional area between the temperate and the polar zone.
aridzone (arid means dry), the boundaries are marked by the scarceamount of precipitation and not by temperature.
The eluviation zone is the layer of soil left behind when substances are transported away by water.
The illuviation zone is the layer below where the substances are deposited.
The parent material is located at the very bottom, where there has not yet been any influence of soil formation.