Water Flashcards
store
reservoirs where water is held
(oceans , lakes )
fluxes
way water moves between stores
flows
movement of water
hydrological cycle
a closed system driven by solar and gravitational potential energy
why the hydrological cycle is a closed system
no external outputs or inputs , the total volume of water is infinite and constant but can exist in different states
hydrosphere
water on surface
96.5% of total water
lithosphere
water in earths crust
1.7% of global water
atmosphere
water as vapour in earth above us
0.001% of total water
4 main stores of water
cryosphere
atmosphere
lithosphere
hydrosphere
cryosphere
areas of earth where water is frozen into snow or ice
1.7% of global water
how water is stored on land
rivers, streams , lakes and groundwater (blue water as visible)
or in plants in soil or vegetation itself
(green water as invisible)
how is water stored in the atmosphere
mainly as vapour ,
what is the carrying capacity in the atmosphere linked to
the temperature
ocean as a store
stores over 1 million
home to 96% of earths water
residence times
average time a water molecule will spend in that reservoir or store
what does residence time effect
-it impacts on turnover within the water system ,
-accesible stores ( rivers and lakes) are easily turned over due to evaporation or transpiration
- inaccessible stores ( deep ground water) can be stored for 10,000 years and become fossil water as it’s non renewable
fluxes - infiltration
water soaked into the ground
fluxes - precipitation
the movement of water from the atmosphere to the ground as droplets fall from clouds
fluxes - interception and transpiration
plants take water from the ground and return to atmosphere by transpiration
fluxes - accumulation
snow and ice melt back into liquid
fluxes - condensation
water vapour rises into the clouds after being evaporated
fluxes -evaporation
change in state of water from a liquid to a gas as water is heated by the sun
fossil water
deep ancient water from former wetter periods
main input and output of hydrological cycle
input - precipitation
output- evaporation , transpiration , discharge
flows - through flow
lateral movement of water down a slope
flows - groundwater flow
long process of percolated water into rivers
flows - infiltration
water soaking into plants and soil
flows - surface run off
movement of water overland
flows - percolation
- deep transfer of water into bedrock
flows - interception
retention of water by plants and soil
frontal rainfall
due to a weather front
warm air has to rise over weather front and cools as it rises causing heavy rain
convectional rainfall
occurs on warm days when warm air rises and cools and condenses as it does
relief rainfall
due to topography
air rises over a mountain and cools as it rises causing rain
availability of freshwater
only hydrosphere is accessible
only 2.5% of this is freshwater
only 1.2% of this is on surface
only 1% is accessible
drainage basin
an open system that is the area of land drained by a river and it’s tributaries
why the drainage basin is an open system
as it has external inputs and outputs that cause the amount of water in the drainage basin to vary
drainaige basin - watershed
the highland which divides and separates waters flowing to different rivers
outputs of drainage basin
transpiration from vegetation
evaporation
input of drainage basin
precipitation
source
top of river / origin
confluence
junction where two different rivers meet
tributary
small channel that flows into the main channel
distributary
small channel that flows out of main channel
mouth
end of river where the river flows out to the body of water
conditions needed for precipitation to fall
air cooled to a saturation point
temp below dew point
condensation to facilitate growth of water droplets in clouds
5 physical factors influencing drainage basin
- climate
- relief
- geology
-vegetation
-soil type
rain shadow
a dry area on the side of the mountain as mountain shelters it
interception loss
water retained by plant surfaces then lost due to evaporation or absorbed by plant and transpired
infiltration capacity
max rate which rain can be absorbed by soil in a given condition
5 factors effecting rate of infiltration
- decreases with persistent rainfall
- volume of water already in soil
- type of vegetation cover ( forest is best)
- nature of soil surface
- topography ( steep slopes encourage run off)
outputs of drainage basin - evapotranspiration
combined effect of evaporation and transpiration- accounts for nearly 100% of removal of precipitation in arid areas
physical factors affecting the drainage basin - climate
climate infleunces
- inputs and outputs
- evaporation and precipitation amount
physical factors affecting the drainage basin - soils
soils determine
- amount of infiltration
- sand soils infiltrate
- clay soils don’t
physical factors affecting the drainage basin - geology
impacts
- percolation
- soil formation
physical factors affecting the drainage basin - relief
impacts
- surface run off
- type of precipitation ( relief rainfall)
physical factors affecting the drainage basin - vegetation
imapacts
- interception
- infiltration
- transpiration
human impacts of drainage basin - river management
construction of reservoirs disrupts the flow
human impact on drainage basin- deforestation
increases EVT
increases infiltration
increases surface run off
human impact on drainage basin - urbanisation
impermeable surfaces cause
decreases infiltration
increases SR
human impact on drainage basin - changing land use
arable to pastrol farming = increase soil compaction which increases SR
pastoral - arable farming = increase infiltration due to ploughing
6 main components affected by humans
- evaporation
- EVT
- SR
- infiltration
- interception
- groundwater
water budgets
the annual balance between precipitation , EVT and run off
balance between inputs and outputs
polar regions have low water budget
river regimes
the annual variation in discharge of a river at a particular point measured in cumecs
what is most of the river flow from
supplied from groundwater between periods of rain which feed steadily into the river system from base water flow
eg of river regime - Alaska
Apr- Aug= high flow due to snow melt
Sep - Mar = low flow as ice forms
large flow variability
few human influences
eg of river regime - Amazon
Dec - may = high flow
Jun - nov = low flow
moderate variability but human activity is increasing this
characteristics of river regime are influenced by 7 factors:
size of the river
where measurement is taken
amount and intenisty of precipiation
temps
geology
type of vegetation
human activity
case study - how human factors have affected amazon basin 7 ways
deforestation has disrupted basin by :
- lowering humidity
- increase SR
- increase infiltartion
- increase evaporation
-decreasing transpiration
- increasing soil erosion
- increasing silt in rivers
storm hydrographs
show variation of discharge within a short period of time ( storm, group of storms) not normally longer than a few days
storm hydrographs - lag time
time interval between peak rainfall and peak discharge
flashy storm hydrographs
- steep rising and falling limb
- short lag time
- high peak discharge
delayed hydrographs
- gentle rising limb
- lower peak discharge
- slightly steeper falling limb
- more manageable
Factors affecting shape of hydrograph - climate
flashy hydrographs are due to intense storms or low evaporation
delayed hydrographs are due to steady precipitation and high evaporation
Factors affecting shape of hydrograph - geology
flashy hydrographs will have impermeable rocks such as clay
delayed hydrographs will have permeable rocks that allow percolation
Factors affecting shape of hydrograph - relief
flashy hydrographs will have steep relief of land
delayed hydrographs will have gentle relief