the water cycle and water insecurity Flashcards
what are the inputs in drainage basin system
- precipitation
- water diversion into area
- groundwater flow into area
- surface water flow into area
- surface runoff into area
what are the outputs in a drainage basin
- evapotranspiration
- wateer diversion out of area
- groundwater flow out of area
- surface water out of area
- surface run off out of area
- industrial/residential uses of an area
describe drainage basin system
inputs>drainage basin store> outputs
what is drainage basin store controlled by
- geology
- relief
- water quantity
- available energy
- land use
- drainage density
- vegetation
closed system
where there are no inputs or outputs of matter from an external source- when inputs and outputs are balanced example global hydrological cycle
open system
a system with inputs and outputs from another place
-can end up loosing mkre water then inputs due to evapotranspiration
what are the two processes that drive the hydrological cylce
- solar power
- gravitational potential energy
solar power
- energy from sun heat water
- evaporation increases as global climate warms
- moisture levels in atmosphere increase
- condensation and precipitation increase as earth cools
gravitational potential energy
- water moves by gravity
- wunoff and groundwater gets transported to sea
what is the cryosphere
ice- glaciers and ice sheets
fluxes
global transfer of water
annual flux
variations due to seasons and temperature
global water budget
difference between inputs and outputs
thermohaline circulation
1) polar ocean colder +denser than trpical water so it sinks
2) sinking cold water replced by tropical water on surface
3) water movement from tropics warms up cold water from ocean depths
tropics
where the suns energy is the most concentrated=highest levels of evaporation especially in the inter-tropical convergence zone (ITCZ)
evapotranspiration
sum of water evaporation and transpiration from a surface area to the atmosphere.
the 3 pathways that precipitation follow
- infiltration
- overland flow(surface run off)
- evaporation
what are the 2 ways that precipitation pathways can be delayed
- interception= by plants and buildings before evaporation of infiltration of surface
- precolation= through rocks into groundwater and subsequent aquifers
orographic rainfaill -relief
- warm air FORCED to rises over high ground
- air cools as it rises forming clouds
- air warms back as it descends
convectional rainfall -sea/land
- sun heats land and sea, causing the evaporation in water in sea
- warm air rises- form clouds-rains
frontal rainfall- land
warm air rises over cold air in an angle
- air cools-forms clouds
- heavy rain falls along the frount
human impacts on drainage basin
- over-abstraction
- deforestation
- change in land use/urbanisation
- reservoirs