ELSS Flashcards
Hydrological cycle and drainage basins
A drainage basin is an area of land drained by a river where water is collected and travels down like a stream.
Interception , infiltration , through flow, relocation
I- precipitation being intercepted by vegetation therefore not reading the soil.
I- water on the ground so along into soils and porous rock.
TF- flow of water in soil towards the river.
P- water through soil or porous rock being stored as groundwater.
Outputs
Flows
Interception,infiltration,through flow , prelocation
Outputs
Evaporation transpiration(water lost through plants through pores into atmosphere.)and channel flow (discharge into another larger drainage basin or river.)
Physical factors of a drainage basin
Climate
Seasonality - Vancouver is wettest between October and March.
Summer temps increase evaporation .
Geology
Determines underground storage due to permeability
Water budgets
Show annual balance between inputs )precipitation )and outputs (ebapotranspiragkon) and the impact on soil water availability.
They can be influenced by climate types:
Tropical - tropical wet or dry seasons.
Polar - tundra and ice caps.
River regime
Indicates annual variation of discharge from a river showing climate, geology and soils .
As global temps rise river discharge is likely to increase as glacial meltwater increases river output.
Deficits with hydrological cycle
Droughts - long period of time below average percipitation.2006 south Australia river Murray dried up, 6mil sheep died.
Deforestation reduces soils ability to sore water .
Surpluses with hydrological cycle
Flooding
Human activities like decoration and urbanisation can increase flood risk.