Paper 1 : Freshwater Drainage Basin Flashcards

1
Q

Drainage Basin

A

An area where water supplied by precipitation is transferred to the ocean or larger stream.
- Includes all areas drained by a river.
- Divided by watersheds

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2
Q

Confluence

A

Where 2 rivers meet

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3
Q

Tributary

A

Smaller rivers join the larger river

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4
Q

Watershed

A

The area of highland forming the edge of a river basin.

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5
Q

Source

A

Where the river begins

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6
Q

Mouth

A

The the river ends / meets the sea

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7
Q

Channel

A

Where the river flows -> the drainage basin is an open system = has inputs and outputs + storage transfers

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8
Q

Precipitation

A

Any moisture that falls from the sky.

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9
Q

Interception

A

When an object stops precipitation from reaching the ground.

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10
Q

Evapotranspiration

A

Water evaporating from the vegetation

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11
Q

Infiltration

A

When water travels from the surface into the ground.

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12
Q

Overland flow

A

Surface runoff

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13
Q

Evaporation

A

Surface stores + rivers turning into water vapour

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14
Q

Surface storage

A

Any water held on the surface

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15
Q

Throughflow

A

The movement of water through unsaturated ground

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16
Q

Soil moisture

A

Water stored below surface in unsaturated ground

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17
Q

Groundwater storage

A

Water stored in saturated ground

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18
Q

Groundwater flow

A

Movement of water through saturated ground

19
Q

Perlocation

A

Water travels from unsaturated ground into saturated ground

20
Q

River discharge

A

Discharge is the river that flows into the sea

21
Q

Factors that influence local hydrology

A

Amount, intensity, variability, type (snow,rain), geographical distribution

22
Q

Factors that affect evaporation

A

Temp, humidity, wind speed, vegetation, colour of surface

23
Q

Aquifers

A

Rocks that contain high amounts of water + provide a source of water, water moves slowly through permeable rock.

24
Q

Field capacity

A

The amount of water held in the soil after excess drains away

25
Phreatic zone
Permanently saturated zone
26
Cryosphere
66% of freshwater in high latitude+altitude regions, when it melts it becomes part of the hydrological cycle
27
River discharge
Is the volume of water passing a given point over a set time
28
River discharge equation
Cross sectional area x mean velocity
29
River velocity
The speed and direction of a river (m/sec) Measure in the centre of river. Affected by friction = travels fastest at the centre and slower at banks + bed.
30
Factors affecting velocity
Channel shape - measured by hydraulic radius = cross sectional area / wetted perimeter - the higher the ratio, the more efficient the stream Channel roughness - causes friction, slowing the water down, caused by irregularities in river bed, boulders, trees, vegetation + contact between water and the bed. Channel gradient - slope / steepness = the steeper the gradient the faster the velocity
31
River long-profile
Upper = steep sides, shallow river, v-shaped valley, vertical erosion Middle = steep, deep channel, lateral erosion, gently sloping sides Lower = deeper channel, very wide, almost flat valley, gentle, high rates if deposition
32
Erosional processes: Abrasion Attrition Hydraulic action Solution
Abrasion = (corrosion) is the wearing away of the bank + bed by the carried load. Attrition = the wearing away of the load, creating smaller particles. Hydraulic action = the force of air + water on the sides of the river + cracks. Direct force causes pressure to drop + bubbles to form. Solution = the removal of chemical ions (Ca) dissolving certain types of rocks
33
Factors affecting erosion
Heavier load, fast velocity, steeper gradient, softer rock, acidic water, high rates of deforestation = increased erosion
34
Transportation Processes: Traction Saltation Suspension Solution
Traction = movement of large boulders Saltation = movement of smaller rocks + pebbles Suspension = movement of silt Solution = the minerals dissolved
35
Deposition
Sediment dropped, carried by wind + water. - increases at a shallower gradient = lower velocity - increases with a lower volume of water - increases with a increase in friction between water + channel
36
Interlocking spurs (upper)
Projections of high land that alternate from either side of a v-shaped valley
37
Waterfall (upper)
When a river flows overland that has two different heights + rock types. - Softer rock erodes faster = undercutting harder rock - Leaving an overhang = until it collapses - Fallen rocks crash into plunge pool - Repeated upstream leaving behind a gorge
38
Meander (middle)
A bend in a river channel. - Forms when water erodes the banks of the outside + sediment is deposited on the inside
39
Ox-bow lake (middle)
The neck of the meander gets narrower,eventually cutting it off during a flood, sediment seals it off
40
Floodplain (lower)
An area of land alongside a river prone to flooding = very fertile land due to deposition
41
Levee (lower)
A natural / artificial wall that blocks water. - Formed by repeated flooding (sediment) - Used to create available land or divert a body of water
42
Hydrographs
Shows how a river channel responds to key processes of the hydrological cycle, measures the speed at which rain falling on a drainage basin reaches the river channel Discharge or run-off is plotted against time
43
Factors affecting hydrographs
Channel modifications = channelisation, enlargement, straightening = increases movement of water - lowers lag times (increases carrying capacity) Urbanisation = removal of trees = decreased evapotranspiration + interception = increased runoff (impermeable surfaces) Removal of vege - shorter lag times, increased peak flows, flood risk, runoff and lower carrying capacity. Vege type = winter means fewer leaves , lowers interception