The Water Cycle Flashcards
Where is water stored?
The atmosphere
The ocean
Ice caps - cryosphere
Soil
Groundwater
Vegetation
Lakes and rivers
What is the difference between blue and green water?
Blue water: water in the form of oceans/ lakes/ rivers
Green water: water stored in vegetation and organic matter
Define the global hydrological cycle
The continuous cycle of water between the oceans, the land, and the atmosphere on a global scale. This is a closed system.
Why is water a valuable resource?
Most of it is seawater
69% of freshwater is locked up as snow and ice
30% is deep underground
Our water supply is unevenly distributed
Varying residence times
Fossil water- not renewable or reachable for human use
Or very short residence times- we can’t harness the water as it disappears too quickly
This means that only about 1% of freshwater is easily available for humans to use
What is a water budget?
Water budgets show the annual balance between inputs
(precipitation) and outputs (evapotranspiration) and their
impact on soil, water availability and are influenced by climate
type ( tropical temperate or polar examples).
What two processes drive the hydrological cycle?
Gravitational and solar energy
What is fossil water?
Untapped ancient stores of freshwater exist in polar regions and beneath some deserts
What is throughflow?
Also known as inter-flow; water seeping laterally through soil below the surface, but above the water table
What three components are part of any water cycle?
Stores
Fluxes: which measure rate of flow between the stores
Processes: physical mechanisms that drive the movement of water
Label a drainage basin
Drainage basin factors
Snow - capped peaks hold water back until thaw - delayed flow
Large drainage basins affected more by precipitation
Forest and vegetation result in more inception
Impermeable soils and rocks prevent infiltration and cause surface saturation
Impermeable urban surfaces
Reservoirs hold water back and create new surface water stores
Grasslands have higher infiltration, percolation, throughflow and evaporation
Steep slopes promote faster movement
Define the water balance and why it is important to analyse
Is the balance between inputs (precipitation) and outputs (runoff and groundwater storage) into a river. This affects the river regime (pattern of flow) and is essential to predict flooding, ensure there is enough water in the system to meet human needs, and manage amounts of water extraction from the river.
The Water Budget Graph
Soil moisture surplus: after winter in spring there is an abundance of soil moisture that can supply rivers
Soil moisture utilisation: when evapouration exceeds precipitation in the summer and is utlized
Soil moisture deficit: By the second half of the summer there has been so much evapouration that there is a soil defecit
Soil moisture recharge: In winter precipitation is increased and evapouration falls in autumn allowing soil moisture to be recharged
Define river regime
The variability in the discharge of a river during the year in response to precipitation, temperature, evapotranspiration and drainage basin characteristics
Aral Sea Case study
Formerly one of the four largest lakes in the world with an area of 68,000 km2 (26,300 sq mi), the Aral Sea has been steadily shrinking since the 1960s after the rivers that fed it were diverted by Soviet irrigation projects. By 2007 it had shrunk to 10% of its original size splitting into four different lakes.
Water was required to support the cotton industry (globalisation, human factors)
Amazon Case study
The land of the Amazon Rainforest is naturally nutrient-deficient because most of the nutrients are stored within the aboveground biomass of the vegetation. Tree root systems hold the soil together to slow the rate of flooding and reduce erosion. Trees themselves also absorb water during the rainy season. When the trees are removed from the environment, the rainy season can have devastating effects. Rains wash away the vital topsoil and what nutrients are left. Increased deforestation therefore leads to decreased biodiversity and species richness.
Due to slash and burn technique there is no vegetation for inception
Hydrographs: Baseflow
Estimate of the water that flows into a river from groundwater flows
Hydrographs: Attendant discharge
The discharge before a storm event
Draw a hydrograph
Include these labels:
Baseflow
Peak discharge
Peak rainfall
Rising limb
Receding limb
Attendant discharge
Lag time
Agricultural drought
Happens when crops become affected due to a lack of supply of surface or groundwater.
Famine drought
Happens when there is crop failure on such a large spatial scale that a humanitarian crisis ensues for a region.
Meteorological drought
Happens when dry weather patterns dominate an area
Hydrological drought
Occurs when low water supply becomes evident, especially in streams, reservoirs, and groundwater levels, usually after many months of meteorological drought.
Physical factors affecting drought: Sea temperature
If sea surface temperature changes then this can cause a change in the amount of rainfall different regions receive.