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Water Cycle 1
System components
• Stores are natural reservoirs of water, such as the
ocean, lakes or ice caps
• A water flow entering a store is called an input: for
example a river entering the ocean
• Flows leaving stores are called outputs: for example,
evaporation of ocean water
• Flows are movements (or transfers or fluxes)
between stores in a system
Class activity
What is the difference between an open system and a closed
system? What examples are there of each?
Water Cycle 1
The global water cycle
• The global water
cycle is shown as a
‘black box’ model
• What are the
strengths and
weaknesses of
viewing water
stores and flows in
this way?
Class activity
What systems have you studied in other Geography topics? What
are their similarities and differences?
(c) Hodder Education [OCR A-level Geography (Raw)]
Water Cycle 1
Another view of the water cycle
Class activity
Which illustration of the water
(c) Hodder Education cycle do you prefer, and why?
[Edexcel A-level Geography Book 2 (Dunn)]
Water Cycle 1
The concept of mass balance
• At a global scale, mass balance means that the total
amount of water is always conserved
• At the global scale, there is a fixed amount of water in the
Earth-atmosphere system (about 1385 million cubic
kilometres of water)
• Transfers can occur; changes occur in where water is stored
without affecting the mass balance. For instance, water
vapour in the atmosphere is precipitated on to the land as
rain or snow after condensation occurs: although it has
changed state, all water still remains in the system
Class activity
What other water transfer processes are there?
Why don’t they affect the system’s mass balance?
Water Cycle 1
Global water stores
Store Volume Per cent of Distribution and characteristics
(cubic km) total water
Oceans 1,335,000 97 Oceans cover two-thirds of the Earth
Cryosphere 26,000 2 Ice and snow stores found at high
latitudes (poles) and high altitudes
Groundwater 15,000 1 Can remain stored for 10,000 years
River and lakes 178 0.01 Uneven distribution due to climate
Soil moisture 122 0.01 Permafrost in Russia and North America
Atmosphere 13 <0.01 There is sufficient moisture for ten days
of rain in the atmosphere
Biosphere 0.6 <0.01 Distributed unevenly because of climate
Class activity
(1) Compare the size of the different stores (2) What local factors
affect water storage in different places?
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