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Hydrology
      and
     Fluvial
  Geomorphology

HYDROLOGICAL CYCLE
Condensation
What is hydrological cycle?
• The movement of moisture and energy BETWEEN
  air, land and sea.

• Oceans, rivers, clouds and rain – all contain water
  in a frequent state of change.

• The circulation and conservation of water from
  the land to the sky and back again

• An example of a system which a set of
  components is linked
How does the hydrological cycle work?
• The components of the cycle are:
  – Evaporation
  – Transpiration
  – Evapotranspiration
  – Potential EVT
  – Actual EVT
  – Condensation
  – Precipitation
  – Percolation
  – Groundwater
  – Run-off
Evaporation
• A process by which water
   is converted from its liquid
  form to gaseous form

• transferred from land and water masses to the
  atmosphere.

• Evaporation from the oceans accounts for 80%

• 20% coming from inland water and plant surfaces.
Evaporation
• Wind speed: the higher
  the wind speed, the
  more evaporation
• Temperature: the higher
  the temperature, the
  more evaporation
• Humidity: the lower the
  humidity, the more
  evaporation
Transpiration
A process by
which plants
lose water
vapour into the
air through
their leaves or
stems
Evapotranspiration

  The total loss
   of moisture
  from an area
    by direct
   evaporation
       and
  transpiration
Evapotranspiration (EVT)

  Potential EVT                   Actual EVT
• The amount of water             • Is what
  that could be lost by             actually
  evapotranspiration.               occurs.


• For example, it is              • In the UK
                                    there is more
  potentially high EVT              water
  in deserts, but the               available for
  amount that can take              evapo-
  place is limited due              transpiration
  to the minimal                    than takes
  moisture available.               place
CONDENSATION
A process of the change of
water vapour into water

–Transported water vapour
 and forms tiny droplets in
 clouds
Precipitation
• The deposition of moisture
  from the atmosphere on the
  earth’s surface

• The most important input into
  the system forms includes
  snow, hail, rain, and fog.
Percolation
• The process by which the
  rain water soaks through
  the soil into the rocks

• Water moves downward

• Infiltrates through soil
  until reaches water table

• Water in the soil does not remain there but moves down slowly
  into the lower layers of soil and rock.

• It creates groundwater storage found in rocks and this may
  later be moved sideways through the rock via groundwater
  flow.
Groundwater
• The place where water is stored
  underground in the rock

• Some of the groundwater is
  trapped between rock or clay
  layers

• Water that infiltrates the soil
  flow downward until it
  encounters impermeable rock
  then travels laterally

• The location where water
  moves laterally is known as
  ‘aquifers’
Run-off
•the water that returns
    to the land which
  flows downhill or on
   the surface of earth
At a global scale, the hydrological cycle is a closed system




• Water is circulated continuously fuelled by energy
  from the sun
• No effective gains or loses
• Fixed amount of water
Exercise
1. Define hydrological cycle.                        (2)

2. Draw a well-labelled with brief explanation of the
   following on the diagram:
  a.   Evaporation
  b.   Transpiration
  c.   Condensation
  d.   Precipitation
  e.   Percolation
  f.   Groundwater
  g.   Run-off                                       (18)

3. Explain why hydrological cycle is a closed system. (5)

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Hydrologyical cycle lesson 1

  • 1. Hydrology and Fluvial Geomorphology HYDROLOGICAL CYCLE
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  • 5. What is hydrological cycle? • The movement of moisture and energy BETWEEN air, land and sea. • Oceans, rivers, clouds and rain – all contain water in a frequent state of change. • The circulation and conservation of water from the land to the sky and back again • An example of a system which a set of components is linked
  • 6. How does the hydrological cycle work? • The components of the cycle are: – Evaporation – Transpiration – Evapotranspiration – Potential EVT – Actual EVT – Condensation – Precipitation – Percolation – Groundwater – Run-off
  • 7.
  • 8. Evaporation • A process by which water is converted from its liquid form to gaseous form • transferred from land and water masses to the atmosphere. • Evaporation from the oceans accounts for 80% • 20% coming from inland water and plant surfaces.
  • 9. Evaporation • Wind speed: the higher the wind speed, the more evaporation • Temperature: the higher the temperature, the more evaporation • Humidity: the lower the humidity, the more evaporation
  • 10. Transpiration A process by which plants lose water vapour into the air through their leaves or stems
  • 11. Evapotranspiration The total loss of moisture from an area by direct evaporation and transpiration
  • 12. Evapotranspiration (EVT) Potential EVT Actual EVT • The amount of water • Is what that could be lost by actually evapotranspiration. occurs. • For example, it is • In the UK there is more potentially high EVT water in deserts, but the available for amount that can take evapo- place is limited due transpiration to the minimal than takes moisture available. place
  • 13. CONDENSATION A process of the change of water vapour into water –Transported water vapour and forms tiny droplets in clouds
  • 14. Precipitation • The deposition of moisture from the atmosphere on the earth’s surface • The most important input into the system forms includes snow, hail, rain, and fog.
  • 15. Percolation • The process by which the rain water soaks through the soil into the rocks • Water moves downward • Infiltrates through soil until reaches water table • Water in the soil does not remain there but moves down slowly into the lower layers of soil and rock. • It creates groundwater storage found in rocks and this may later be moved sideways through the rock via groundwater flow.
  • 16. Groundwater • The place where water is stored underground in the rock • Some of the groundwater is trapped between rock or clay layers • Water that infiltrates the soil flow downward until it encounters impermeable rock then travels laterally • The location where water moves laterally is known as ‘aquifers’
  • 17.
  • 18.
  • 19. Run-off •the water that returns to the land which flows downhill or on the surface of earth
  • 20.
  • 21. At a global scale, the hydrological cycle is a closed system • Water is circulated continuously fuelled by energy from the sun • No effective gains or loses • Fixed amount of water
  • 22. Exercise 1. Define hydrological cycle. (2) 2. Draw a well-labelled with brief explanation of the following on the diagram: a. Evaporation b. Transpiration c. Condensation d. Precipitation e. Percolation f. Groundwater g. Run-off (18) 3. Explain why hydrological cycle is a closed system. (5)