Operation of the Drainage Basin as an Open System Flashcards

(41 cards)

1
Q

Catchment

A

The area of land drained by a river and it’s tributaries

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2
Q

Watershed

A

The highland which divides and separates waters to flowing rivers

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3
Q

Condensation

A

The change from a gas to a liquid, such as when water vapour changes into water droplets

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4
Q

Dew point

A

The temperature at which dew forms; it is a measure of atmospheric moisture

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5
Q

Convectional Rainfall

A

Often associated with intense thunderstorms, which occur widely in areas with ground heating such as the Tropics and continental interiors

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6
Q

Cyclonic Rainfall

A

A period of sustained, moderately intensive rain; it is associated with the passage of depressions

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7
Q

Orographic Rainfall

A

Concentrated on the windward slopes and summits of mountains

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8
Q

Interception loss

A

This is water retained by plant surfaces and later evaporated or absorbed by the vegetation and transpired

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9
Q

Throughfall

A

This is when the rainfall persists or is relatively intense, and the water drops from the leaves, twigs, needles etc

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10
Q

Stem Flow

A

This is when the water trickles along twigs and branches and then down the trunk

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11
Q

Infiltration

A

The movement of water from the ground surface into soil

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12
Q

Infiltration Capacity

A

The maximum rate at which rain can be absorbed by soil

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13
Q

Surface run-off

A

The movement of water that is unconfined by a channel across the surface of the ground. Also known as overland flow

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14
Q

Percolation

A

The transfer of water from the surface or from the soil into the bedrock beneath

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15
Q

Saturated Overland Flow

A

The upward movement of the water table into the evaporation zone

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16
Q

Evapotranspiration

A

The combined effects of evaporation and transpiration

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17
Q

Channel flow

A

The flow of water in streams or rivers

18
Q

Channel Storage

A

The storage of water in streams or rivers

19
Q

Potential Evapotranspiration

A

The water loss that would occur if there was an unlimited supply of water in the soil for use by vegetation

20
Q

Deforestation

A

The cutting down and removal of all or most of the trees in a forested area

21
Q

Afforestation

A

The planting of trees in an area that has not been forested in recent times

22
Q

Drainage basin

A

The area of land drained by a river and its tributaries

23
Q

Drainage Basin

A

The area of land drained by a river and it’s tributaries

24
Q

Inputs of drainage basin

A

Precipitation

25
Impacts of inputs on drainage basin depend on:
``` The amount of precipitation The type of precipitation Seasonality Intensity of precipitation Variability ```
26
Secular variability
Long term variability, result of climate change trends
27
Periodic variability
Happens in annual, seasonal, monthly, diurnal context
28
Stochastic Variability
Results from random factors, such as the localisation of a thunderstorm within a basin
29
Interception
Process by which water is stored in the vegetation, 3 main components - interception loss, through fall and stem flow.
30
Factors affecting interception loss
- point of storm, more interception loss at start and following dry period - type of tree: coniferous tree greater, as dense needles. - seasonality in deciduous forests: summer/winter - wind speeds: decrease, intercepted water dislodged, and increases evaporation - intensity & duration of rainfall - amount of rainfall increases, less water intercepted as tree canopies become saturated - agricultural crops- more interception with more dense crop
31
Factors affecting infiltration
- decreases with time during a period of rainfall as a constant low level is reached - Antecedent soil moisture, wet soils, less infiltration as already saturated - Soil texture, level of porosity - Type, amount and seasonal changes in vegetation. More vegetation = more infiltration - Nature of soil surface, compact promotes overland flow - Slope angle, steep = more runoff, flat = infiltration
32
Throughflow
The lateral transfer of water down slope through soil via natural pipes and percolines.
33
Percolines
Lines of concentrated water flow between soil horizons to the river channel
34
Fluxes in drainage basin
Interception, Infiltration
35
Flows and transfers in drainage basin
- Overland flow/surface runoff - Throughflow - Percolation - Saturated overland flow - Channel flow
36
Outputs of drainage basin
Evaporation, transpiration
37
Factors affecting Evaporation rate
- Climatic factors; temperature, hours of sunshine, humidity and windspeed. Temperature most important. - size of water body - depth of water - water quality - type of vegetation cover - colour of water surface
38
Factors affecting transpiration rate
- Time of year - type and amount of vegetation cover - degree and availability of moisture in the atmosphere - length of growing season
39
Physical factors affecting the drainage basin system
- Climate - Soils - Geology - Relief - Vegetation
40
Human factors affecting the drainage basin
- River management: Building dams/reservoirs, reduces flows. Abstracting water for domestic and industrial use, reduces flow. Abstracting groundwater for irrigation, reduces the water table. - Deforestation: reduces evapotranspiration, increases infiltration and surface runoff - Changing land use - AGRICULTURE: soils compacted by livestock, increased surface runoff. soils aerated by ploughing, increased infiltration as soils loosened - Changing land use - URBANISATION: changing to urban land surfaces, increased surface runoff and less infiltration and percolation. Drains move rainfall to rivers and streams faster, increased chance of flooding.
41
Components of drainage basin mostly affected by humans
- evaporation & evapotranspiration - interception - infiltration - groundwater - surface runoff