The water cycle or Hydrologic cycle is the recycling process of water between oceans, atmosphere and - PowerPoint PPT Presentation

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The water cycle or Hydrologic cycle is the recycling process of water between oceans, atmosphere and

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Evaporation- liquid to gas & Transpiration- water vapor released by plants. Distribution of water on ... Infiltrate- When water seeps or sinks into the ground. ... – PowerPoint PPT presentation

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Title: The water cycle or Hydrologic cycle is the recycling process of water between oceans, atmosphere and


1
The water cycle or Hydrologic cycle? is the
recycling process of water between oceans,
atmosphere and land.
2
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3
Quick review
How does water vapor enter the atmosphere? By
what two processes?
Evaporation- liquid to gas Transpiration- water
vapor released by plants
4
Distribution of water on Earth
5
Important terms
  • Infiltrate- When water seeps or sinks into the
    ground.
  • Run Off- precipitation can flow over Earths
    surface and return to rivers, lakes and oceans
    and re-enter the water cycle.
  • Water retention- precipitation is stored or
    retained on land surface as ice or snow

6
Runoff
7
Factor affecting infiltration
  • Degree of saturation- the more saturated the
    loose material and ground is the less
    infiltration that will occur.
  • Vegetation reduces infiltration

8
  • 3. Slope of the land

The steeper the slope of the land the less water
that can seep into the ground. Steep slope less
infiltration.
Example On the side of a mountain less water
will seep in than in the bottom of a valley that
is flat.
9
4. Porosity
  • Porosity- The percentage of open space in a
    material compared to the total volume.
    Determines the amount of water or air a material
    can hold.
  • Shape, packing and sorting effect porosity

10
Factor affecting porosity
  • 1. Shape well-rounded particles have greater
    porosity than angular or plate-shaped particles.
    Well rounded particles do not fit together as
    tightly.
  • 2. Packing The more closely packed particles
    are the lower the porosity.
  • 3. Sorting When all particles are about the
    same size they are sorted
  • When particles are mixed in all different sizes
    they are unsorted.
  • Unsorted particles have less porosity. Small
    particles can fit between larger particles
    filling in the space and lowering porosity

11
Sorting and Porosity
12
5. Permeability
  • Permeability- the ability of a material to allow
    fluids such as water to pass through.
  • Material can be porous and impermeable
  • How well connected the pores or openings in
    the rock are determines the permeability.

13
6. Capillarity- water is stopped for moving
downward by attractive forces between water
molecules.Capillary Action- Movement of water
upward from the water table to the surface
against gravity.When size of particles
increases, porosity increases this reduces
capillarity.
14
7. Land Use
  • How people use the land affects how much water
    seeps into the ground. Roads parking lots, and
    building covers create a surface the is
    impermeable to liquids.

15
  • Why does runoff occur?
  • Precipitation rate is greater than infiltration
    rate
  • Pore spaces are saturated with water
  • Slope of surface is too great
  • Water on surface is not evaporating of
    sublimating into a gas.
  • Runoff increases stream discharge

16
Factor affecting Climate
Climate Controls These factors affect how a
climate will be. Latitude Planetary wind
pressure belts Ocean and other large bodies of
water Mountains Elevation Ocean
Currents Vegetation
17
  • Stream discharge- The volume of water flowing
    past a certain spot in a stream over a certain
    period of time.
  • Climate- The overall view of a regions weather
    conditions over a long period of time. (10s of
    thousands of years)
  • The average temp and amount of moisture play
    key roles in the determination of a climate.

18
  • Latitude Temp
  • Lower latitude warmer temps all year
  • Ex Equator
  • High Latitude Cold temps all year.
  • Ex North Pole

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  • Large bodies of water
  • moderate temp. Land near water will cool and
    heat slower. Water has a high specific heat.
  • Surface Ocean Currents
  • Warm currents bring warmer temps and cold
    currents bring cooler temps.
  • Ex the gulf stream brings England and Ireland
    warmer temps
  • Elevation
  • the higher the elevation the cooler the
    weather.
  • Ex Now capped Mtns.

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  • Mountains
  • mountain can block winds causing a moist area
    on one side of the mountain (windward) and a dry
    areas on the other (leeward).

Clouds Precipitation
Air sinks, compresses and warms. DRY AIR
leeward
windward
Air rises, COOLS and condenses
wind
23
  • Vegetation
  • The more vegetation/plants the more humid the
    climate.
  • Ex Rain Forest very moist
  • Desert has few plant and is very dry

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