1.0 Introduction to river environments Flashcards

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1
Q

Fluvial

A

A term applied to the action of rivers and streams

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2
Q

Fluvial Geomorphology

A

The study of processes and landforms resulting from river erosion, transport and deposition

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3
Q

What is the Global Hydrological Cycle?

A

The continual circulation of water between the Earth’s surface and the atmosphere.

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4
Q

What kind of system is the GHC and why?

A

Closed system- It doesn’t have any external inputs or outputs; water circulates through a number of stores

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5
Q

How does water move between stores in the GHC?

A

Movement between stores comes through inputs and outputs in a series of flows/ transfers and fluxes/ processes

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6
Q

How does water move through the cycle (in what form?)

A

Water moves through the cycle in all 3 forms

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7
Q

Explain why the GHC is a closed system (short answer)

A

Water on the Earth’s surface or in its atmosphere isn’t lost into space neither is it added to from outside of the atmosphere.

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8
Q

How much water is within the system?

A

A finite amount

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9
Q

Since there is a continuous cycle of water, what are the major stores it flows between?

A

Oceans, atmosphere, biosphere, land surface & groundwater store

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10
Q

What is the circulation in the GHC driven by?

A

-Solar energy (evapotranspiration)
-Gravitational potential energy
-Infiltration, percolation, throughflow, groundwater flow

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11
Q

Residence time within key stores

A

Vastly different

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12
Q

What is the significance of variations in solar energy input (polar vs rainforest) and geomorphology or landscapes?

A

Local/ regional variation in operation of system between different climatic zones and drainage basins

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13
Q

What is fossil / paleo water?

A

Untapped ancient stores or freshwater exist in the polar regions and below many deserts.

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14
Q

How much freshwater does Kenya’s Lotikipi Aquifer contain?

A

Estimated 200 billion cubic metres of freshwater

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15
Q

Define ‘residence time’

A

Storage times of the world’s main water stores/ resources

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16
Q

Residence time of oceans

A

4000 years

17
Q

Describe the hydrology of The Cryosphere (Polar Regions)

A

Seasonal thaws bring increased surface saturation and thinning permafrost. If this thaw becomes continuous, water flows away and is lost which is known as Cryosphere loss

18
Q

Describe the hydrology of The Cryosphere (Polar Regions)

A

Seasonal thaws bring increased surface saturation and thinning permafrost. If this thaw becomes continuous, water flows away and is lost which is known as Cryosphere loss

19
Q

Describe the hydrology of Tropical Rainforests

A

Permanently dense forest produces high rates of evapotranspiration, with water returning to the surface as precipitation that feeds large rivers such as the Amazon

20
Q

Identify the key factors to t influence the operation of the Hydrological Cycle in Polar Regions

A

Low temperatures - high % of water held in ice
Low evapotranspiration
Low annual precipitation
Seasonal change- freeze/thaw
Limited vegetation
Permafrost - impermeable

21
Q

Identify the key factors to t influence the operation of the Hydrological Cycle in Tropical Rainforests

A

High temps - high evapotranspiration
High annual precipitation
Limited seasonal change (year round heat/rain)
Vast vegetation coverage- interception and storage- little water reaches ground or infiltrates

22
Q

What is a drainage system an example of?

A

An open system which is a subsystem within the closed system if the GHC

23
Q

Drainage Basin

A

Has stores , flows and processes (like closed system) but inputs/ outputs are added from outside the system and transfer to other drainage basins

24
Q

Where do inputs come from within an open system?

A

Precipitation

25
Q

Where do outputs include in an open system?

A

Evapotranspiration or river discharge into other drainage basins, lakes or coastal environment -> the ocean store

26
Q

Within the GHC and drainage basin subsystems, what can the interaction between human and physical environments result in conditions lead to?

A

Water surplus (river flooding)
Water deficit (drought)