Hydrosphere Flashcards

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1
Q

Describe the Global Hydrological Cycle (8) [DIAGRAM]

A

DRAW DIAGRAM

  • Water evaporates from the ocean into the atmosphere
  • This water condenses to form clouds
  • Wind carries the clouds inland by advection
  • The cloud droplets become heavy and fall as precipitation
  • The precipitation reaches land and runs off the surface to the ocean if the land is impermeable
  • If the land is permeable, the water droplets infiltrate the soil and move towards the ocean as soil through-flow
  • The water could also percolate into the rock below the soil and move as groundwater flow towards the ocean
  • Some run off os soil through-flow may be absorbed by trees and transpired back into the atmosphere
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2
Q

How have humans had an effect on the Global Hydrological Cycle? (10)

A

Mining has an impact on cycle

  • Mining reduces vegetation cover, resulting in more surface run off
  • Reduced vegetation cover also results in lower evapo-transpiration, altering rainfall patterns

Urbanisation has an impact on cycle

  • More impermeable surfaces increases surface run off, raising river levels
  • Impermeable surfaces also decrease amount of groundwater storage, reducing the water table
  • Urbanisation requires takes water to use in cities, reducing water in rivers due to reservoirs being built

Deforestation has an impact on cycle

  • Cutting down trees increases surface run off
  • It also decreases evapo-transpiration, and alters cloud formations
  • There will be more extreme river flows as water is not intercepted by vegetation

Irrigation has an impact on cycle

  • It can increase evaporation by placing water in surface stores
  • It involves taking water from a river which can reduce the rivers flow
  • The crops that irrigation is used for will absorb water as they grow, which increases evapo-transpiration
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3
Q

Describe the movement of water within a drainage basin, referring to inputs, storages, transfers and outputs (8)

A

Each drainage basin is a system with inputs, storages, transfers and outputs.

• Inputs are where water enters the system

  • Water can enter the system as precipitation

• Storages are places where water is held in the system

  • Water can be held on lakes on the surface or in soil and rocks in the ground

• Tranfers are processes by which water moves through the system

  • The water can move as surface run off, or as through-flow underground

• Outputs are where water leaves the system

  • The water can leave the system by entering the sea through rivers or by being evaporated into the atmosphere
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4
Q

How does erosion change from the upper course to the lower course of a river? (5)

A

The Upper Course

  • Areas with steep gradients will have an increased velocity and so the potential for erosion is higher
  • The river can transport larger pieces of rock in the upper course so can erode the sides of the river by abrasion
  • Hydraulic action occurs so will wear away the river bed by the force of water acting on it

The Middle Course

• The main areas of erosion will occur on the outside bends of the river through hydraulic action and abrasion

The Lower Course

• Erosion at this point is minimal but may be found in meanders

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5
Q

Describe the formation of a meander (8) [DIAGRAM]

A
  • Meanders begin where riffles and pools develop across the bed of a river
  • A riffle is a shallow area of the river where there is less speed, so more deposition
  • A pool is a deep area of the river where there is more speed, so more erosion
  • The flow of the river is deflected away from the slow moving riffle towards the fast moving pool, swinging the current from side to side
  • As the river swings in this motion, lateral erosion occurs, creating a river cliff on alternating banks
  • As these banks increase in size more water is deflected here, so there is less water flowing across the riffles
  • As the energy of the water in the riffles decrease, the river deposits here and creates a point bar
  • This process keeps going, and creates a clearly defined meander in the river
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6
Q

Describe the formation of an ox-bow lake (6) [DIAGRAM]

A
  • At lateral erosion continues to occur, the river’s meander becomes more sinuous
  • lateral erosion at the outer banks narrows the neck of the meander
  • During a time of extra river energy, like a flood, the river cuts through this neck of the meander and forms a new channel
  • After the flood the river may continue to flow through this channel
  • As the river flows along this channel, it deposits at the sides due to slow flow, and eventually these deposits seal off the old meander
  • The old meander now becomes an ox-bow lake
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7
Q

Describe the formation of a waterfall (6) [DIAGRAM]

A
  • The river flows over bands of softer and harder rocks
  • The softer rock is eroded more quickly
  • The river undercuts the harder rock leaving an overhang
  • The river forms a plunge pool below the waterfall
  • As the overhanging rock is unsupported, it falls into the plunge pool
  • The waterfall is moved upstream, and this process continues to cut back a gorge into the hillside
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8
Q

Describe and explain the changing river levels in a typical hydrograph (6)/(6) [DIAGRAM]

A

Rising Limb

- Short Lag time

  • The drainage basin may be small, so water takes less time to reach the river
  • The slopes of the basin may be steep, so water gets to the river more quickly
  • If rock is impermeable in the basin, water flows as run off and not through soil
  • If the stream density is high in the basin then more water can flow into the river through tributaries
  • If there is little vegetation, water is not intercepted

OR

- Long lag time

  • The drainage basin may be large, so water takes more time to reach the river
  • The slopes of the basin may be gentle, so water gets to the river slowly
  • If rock is permeable in the basin, water flows through flow and not as run off
  • If the stream density is low in the basin then there is less water that can flow into the river through tributaries
  • If there is lots of vegetation, water is intercepted

Falling Limb

• Less steep than the rising limb as water is still reaching the river as soil though flow or groundwater flow

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9
Q

What are the 7 characteristics of a river can you comment on?

A
  • Width
  • Straightness
  • Discharge (Tributaries)
  • Stage
  • Tidal
  • Artificial or natural
  • Landforms
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