ELSS Flashcards

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1
Q

Hydrological cycle and drainage basins

A

A drainage basin is an area of land drained by a river where water is collected and travels down like a stream.

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2
Q

Interception , infiltration , through flow, relocation

A

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.

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3
Q

Outputs

A
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4
Q

Flows

A

Interception,infiltration,through flow , prelocation

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5
Q

Outputs

A

Evaporation transpiration(water lost through plants through pores into atmosphere.)and channel flow (discharge into another larger drainage basin or river.)

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6
Q

Physical factors of a drainage basin

A

Climate
Seasonality - Vancouver is wettest between October and March.
Summer temps increase evaporation .
Geology
Determines underground storage due to permeability

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7
Q

Water budgets

A

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.

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8
Q

River regime

A

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.

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9
Q

Deficits with hydrological cycle

A

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 .

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10
Q

Surpluses with hydrological cycle

A

Flooding
Human activities like decoration and urbanisation can increase flood risk.

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