Hydrological Characteristics (Cambridge (CIE) O Level Geography)
Revision Note
Written by: Bridgette Barrett
Reviewed by: Jenna Quinn
The Characteristics & Processes of Rivers
Water on Earth
Only 2.5% of the water on Earth is freshwater
68.7% of freshwater is stored in glaciers and ice sheets and 30% is groundwater
The remaining 1.3% of freshwater is in rivers, soil moisture, lakes and the atmosphere
All water is part of the hydrological cycle
Sources of Water
Hydrological cycle
The hydrological cycle is a closed system
Water is constantly recycled through the system
Within the hydrological cycle, there are stores and transfers (flows)
The Hydrological Cycle
Stores are those places where water is held for a period of time. These include:
Water in the atmosphere in the form of water vapour or water droplets in clouds
Surface stores such as puddles, lakes, rivers and reservoirs
Interception is how precipitation is prevented from reaching the ground, usually by being caught on leaves or branches
Aquifers are permeable rocks such as limestone and sandstone which can hold water
Ice and snow
Seas and oceans
Flows are the ways in which water is moved around the hydrological cycle. They include:
Evaporation
Condensation
Transpiration
Evapotranspiration
Precipitation
Overland flow
Infiltration
Percolation
Through flow
Groundwater flow
Examiner Tips and Tricks
Remember that percolation and infiltration are not the same. Percolation happens after the water has infiltrated the soil.
Worked Example
Which of the following statements are correct?
Tick two statements in the table below:
[2 marks]
| Tick |
Overland flow occurs under the surface of the land |
|
Water percolates from the surface into the soil |
|
Groundwater flow moves water through the rocks |
|
Water flows to the river on the surface by through flow |
|
Interception occurs when water vapour is evaporated |
|
Infiltration occurs when water soaks into the soil |
|
Answer:
Ground water flow moves water through the rocks [1]
Infiltration occurs when soil soaks into the soil [1]
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