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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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