4.1.1 Movements of water in the hydrosphere are driven by solar radiation and gravity.
4.1.2 The global hydrological cycle operates as a system with stores and flows.
4.1.3 The main stores in the hydrological cycle are the oceans (96.5%), glaciers and ice caps (1.7%), groundwater (1.7%), surface freshwater (0.02%), atmosphere (0.001%), organisms (0.0001%).
4.1.4 Flows in the hydrological cycle include transpiration, sublimation, evaporation, condensation, advection, precipitation, melting, freezing, surface run-off, infiltration, percolation, streamflow and groundwater flow.
4.1.5 Human activities, such as agriculture, deforestation and urbanization, can alter these flows and stores.
4.1.6 The steady state of any water body can be demonstrated through flow diagrams of inputs and outputs.
4.1.7 Water has unique physical and chemical properties that support and sustain life.
4.1.8 The oceans act as a carbon sink by absorbing carbon dioxide from the atmosphere and sequestering it.
4.1.9 Carbon sequestered in oceans over the short term as dissolved carbon dioxide causes ocean acidification; over the longer term, carbon is taken up into living organisms as biomass that accumulates on the seabed.
4.1.10 The temperature of water varies with depth, with cold water below and warmer water above.
4.1.11 Stratification occurs in deeper lakes, coastal areas, enclosed seas and open ocean, with a thermocline forming a transition layer between the warmer mixed layer at the surface and the cooler water below.
4.1.12 Global warming and salinity changes have increased the intensity of ocean stratification.
4.1.13 Upwellings in oceans and freshwater bodies can bring cold, nutrient-rich waters to the surface.
4.1.14 Thermohaline circulation systems are driven by differences in temperature and salinity.
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