4.1 Introduction to water systems Flashcards

1
Q

what kind of radiation drives the hydrological cycle

A

solar radiation

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2
Q

what fraction of the Earths water storage does fresh water make up

A

a small fraction (approximately 2.6% by volume)

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3
Q

storages of the hydrological cycle

A
  • atmosphere
  • organisms
  • soil
  • oceans
  • groundwater
  • lakes
  • rivers
  • glaciers
  • ice caps
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4
Q

transformation flows within the hydrological cycle

A

( a change in the state of water during the movement process)
- Evaporation: Water changing from liquid to gas.
- Transpiration: Water vapor released from plants.
- EVT (evotranspiration) = most important aspect of water loss as its about 100% of annual percipitation in arid areas, and 75% in humid areas
- Condensation: Water vapor turning into liquid droplets.
- Sublimation: Ice changing directly to water vapor.

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5
Q

transfer flows within the hydrological cycle

A

( the movement of water from one storage to another without changing its state)

  • Surface runoff: Water flowing over land surfaces into streams and rivers.
  • Infiltration: Water seeping into the ground.
  • Stream flow/currents: Movement of water in rivers and oceans.
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6
Q

human impacts on the hydrological cycle A

A

Agriculture
- Irrigation diverts water from natural water bodies, altering local water balances.
- Overuse of groundwater for irrigation can lead to aquifer depletion.
- Agricultural practices can increase surface runoff and soil erosion.

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7
Q

human impacts on the hydrological cycle D

A

Deforestation
- Reduces transpiration and increases surface runoff.
- Can lead to increased flooding and decreased water quality.

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8
Q

human impacts on the hydrological cycle U

A

Urbanisation
- Increases surfaces that dont let water through, reducing infiltration and increasing surface runoff.
- Can lead to urban flooding and decreased groundwater recharge.

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9
Q

Ocean circulation systems

A

driven by differences in temperature and salinity that affect water density. the resulting difference in water density creates a global “conveyor belt” of ocean currents that distributes heat around the world, so affecting the climate.

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10
Q

The Ocean Conveyor Belt

A
  • Surface currents carry warm water from the equator towards the poles.
  • As water cools near the poles, it becomes denser and sinks.
  • Deep ocean currents carry cold water back towards the equator.
  • This cycle helps distribute heat globally, influencing climate patterns.
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11
Q

inputs and outputs of the hydrological cycle

A
  • Primary input: Solar radiation driving evaporation.
  • Outputs: Water leaving the system (e.g., deep groundwater storage).
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12
Q

link between the hydrological cycle and climate

A
  • Water vapor is a greenhouse gas, meaning it traps heat in the Earth’s atmosphere. As temperatures rise due to other greenhouse gases (like CO₂), more water evaporates, increasing the amount of water vapor in the atmosphere.
    This amplifies the greenhouse effect, causing further warming. This is a positive feedback loop.
  • Cloud formation increases global albedo and therefore lowers temperature. BUT cirrus clouds (low, thin) trap heat (infrared radiation) and lead to higher temps, contributing to gh effect.
  • Ocean currents distribute heat, shaping regional climates.
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