EQ1 Flashcards

1
Q

Global water stores + total stored water

A

Hydrosphere (all of the water on the earths surface - rivers, sea) = 96.5%
Atmosphere (water stores in the air) = 0.001%
Cryosphere (frozen water) = 1.7%
Lithosphere (rocky outer layer of earths crust) = 1.7%

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2
Q

Total global water

A

Accessible water to humans only exists on the hydrosphere
96.5% of that is ocean water

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3
Q

Earths freshwater supply

A

Only makes up 2.5% of the earths total water store

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4
Q

Surface water + other freshwater

A

Only 1.2% of earths freshwater supply - v small amount

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5
Q

Accessible freshwater

A

Amount of this that is actually accessible = 1%

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6
Q

Hydrological cycle: inputs, flows, fluxes, outputs

A

Fluxes (type of movement) = hydrological cycle: precipitation, surface run-off, evapotranspiration
Main input = HC = precipitation
Main output = HC = evaporation, transpiration, discharge

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7
Q

Relief rainfall

A

Rainfall that occurs because of landscape shape/topography
Occurs due to the change in temp of the air that rises alongside = hill/mountain
Air cools + condenses as it moves up in the atmosphere + forms clouds + rainfall
Creates drier conditions = rain shadow

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8
Q

Conventional rainfall

A

Usually occurs during = summer = UK when the sun heats the land
Creates rising pockets of warm air = convection currents
Warm air rises rapidly where it starts 2 cool + condense 2 form clouds
Clouds can be large cumulonimbus clouds
Clouds can produce heavy rainfall + thunderstorms

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9
Q

Frontal rainfall

A

Occurs when a warm front meets a cold front. Heavier cold air sinks = ground + warm air rises above it
When warm air rises it cools
Cooler air condenses + forms clouds
Clouds bring heavy rain

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10
Q

Flows seen = HC - 7 main categories

A

INTERCEPTION - through the retention of water by plants + soil
INFILTRATION - water soaking into plants + soil
PERCOLATION - deep transfer of water into bedrock
THROUGHFLOW - lateral transfer of water downslope
GROUNDWATER FLOW - v slow transfer of percolated water
SURFACE RUN-OFF - movement of water over land
RIVER/CHANNEL FLOW - water entering river/stream

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11
Q

Physical factors that affect drainage basin

A

Climate
Soil
Geology
Relief
Vegetation

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12
Q

Climate affecting DB

A

mainly impacts inputs/outputs
Changes the amount + type of precipitation + amount of evaporation

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13
Q

Soil affecting DB

A

Affects the importance of different flows in the system -e.g, surface run-off

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14
Q

Geology affecting DB

A

Affects surface run-off
Impacts percolation + groundwater flow rates
Affects soil formation

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15
Q

Relief affecting DB

A

Affects surface run-off
Impacts the amount of precipitation
Slopes affect run-off

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16
Q

Vegetation

A

Affects surface run-off
Presence of plants has major impact on interception, infiltration, transpiration

17
Q

Human factors affecting DB

A

River management
Deforestation
Changing land use (agriculture)
Changing land use (urbanisation)

18
Q

River management- DB

A

Construction of reservoirs
Use for domestic supply + irrigation of crops
All of this removes water from its natural place - disrupts the general flow of the HC

19
Q

Deforestation - DB

A

Reduced evapotranspiration but Inc infiltration + surface run-off
Less rainfall put into the atmosphere + potentially less rainfall over time
Soil has a surplus of water as there is no vegetation to absorb it

20
Q

Changing land use (agriculture) - DB

A

Arable to pastoral farming: compacts soil + Inc run-off
Pastoral to arable farming: ploughing Inc infiltration rates (loosening the soil allowing it to take more water in from precipitation)

21
Q

Changing land use (urbanisation) - DB

A

Tarmac, tiles, concrete = speed up surface run-off, Inc flooding
Impermeable surfaces means no absorption

22
Q

Example = human factors: Amazonia

A

Amazon basin contains the worlds largest area of tropical rainforest. Deforestation has disrupted the drainage basin cycle. Number of ways;
- lowering of humidity (less evapotranspiration taking place + less water vapour in the atmosphere)
- less precipitation
- more surface runoff + infiltration (compacting soil from removing trees)
- more soil erosion + slit being fed into rivers

23
Q

Water budgets

A

Annual balance b/ precipitation, evapotranspiration, run-off
Annual balance b/ inputs + outputs
Can be calculated globally/locally
Useful for calculating the amount of water available for human use + available soil water
Polar: low budget, low availability etc

24
Q

Water regimes

A

River regimes = annual variation in discharge/flow of a river at a particular point + usually measured in cumecs. Influenced by;
-size of the river + where discharge measurements are taken along it’s course
- amount seasonality + intensity of the precipitation
- temps with possible meltwater + high rates = evaporation in the summer
- geology + soils particularly their permeability + porosity: groundwater notes in permeable rocks is gradually released into the river = base flow
- type of vegetation cover: wetlands can hold water + release slowly into the river
- human activities aimed at regulating a river’s discharge

25
Q

The Amazon - rivers discharge

A

High flow Dec-May
Dry season Jun-Nov
Moderate variability in seasons
Human influence increasing w/ urbanisation + deforestation

26
Q

Alaska - rivers discharge

A

High flow apr-aug due 2 snowmelt
Low flow sep-mar as ice is forming
Large flow variability
Relatively few human influences