5 - deficit within the water cycle ✅ Flashcards
what is a deficit in the water cycle
when there are greater outputs than inputs to the cycle resulting in a depletion of the stores
what can cause deficits in the water cycle (3)
- seasonal variation eg dry seasons
- longer term climate change
- human depletion of stores for use
what does more precipitation create
high precipitation = increased surface runoff and channel flow
so drier seasons = reduced river discharge and runoff
what is a water balance graph
shows the balance between inputs and outputs
how are wet seasons characterised (4)
- precipitation exceeds evapotranspiration = water surplus
- ground stores fill with water
- more surface runoff
- higher discharge = river levels rise
how are dry seasons characterised (2)
- evapotranspiration exceeds precipitation = ground store depletion
- some flows into the river channel, isn’t replaced by precipitation
what is the water balance co-efficient
difference between annual precipitation and potential evapotranspiration
what is water stress
areas where total withdrawals from the area exceed the renewable inputs to the system so the stores begin to be depleted
where is freshwater extracted from
- surface water stores eg lakes
- aquifers
why do humans extract water
- household activities eg washing
- drinking water for exponentially growing population
what is being done to save the Aral Sea
- more efficient irrigation system funded by UN and world bank
- dam that funnels water to Aral
- reducing salinity
what are aquifers
AQUIFERS = permeable porous water bearing rocks such as chalk
what are artesian aquifers
develop where sedimentary rocks have formed a syncline or basin like structure
the aquifer is confined between impermeable rock layers
how did the Ogallala Aquifer form
- formed more than 2 million years ago from melting glaciers
- extensive groundwater resources were virtually unknown until the early 1900s and were not tapped for irrigation water until around 1950
what are the key features of the Ogallala Aquifer (2)
- has extremely low natural recharge rate because its in an area with low precipitation
- water withdrawn from it is so big the aquifer is being depleted eight times faster than its natural recharge rate