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Unit 6: Atmospheric Science

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What is the name of the radiation that we receive from the sun? How about the Earth? ... A sling-psychrometer is the tool used for figuring this ... – PowerPoint PPT presentation

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Title: Unit 6: Atmospheric Science


1
Unit 6 Atmospheric Science
  • Topics
  • 1. Review Energy Transfer
  • 2. Dew Point Humidity
  • 3. Energy at the Earths surface

2
Review
  • What is the name of the radiation that we receive
    from the sun? How about the Earth?
  • What are the 3 forms of energy transfer?
  • What is the wavelength of UV rays?
  • What waves do waves do we get from the sun? How
    about the Earth?

3
Dew Point and Humidity
  • The dew point is the air temperature at which
    condensation occurs
  • Condensation is the process of water vapor
    turning into liquid water.
  • The humidity is the percentage of water vapor in
    a parcel of air
  • A parcel is just a portion/section of the air

4
How does dew form?
  • It is a relationship between the amount of
    humidity and the temperature

5
Time- 2 Pm Temp- 80
Time- 7AM Temp.- 55
Time- 6 PM Temp- 68
Time- 8 PM Temp- 55
Dew droplets
D.P.- 55 Humidity- 45
D.P.- 55 Humidity- 70
Dew Point- 55 Humidity- 100
D.P.- 55 Humidity-100
6
Dew Point versus Humidity
  • The dew point is not only on the ground it is
    also up in the sky
  • As you go higher in the sky the temperature cools
    to the dew point and condensation occursCLOUDS

7
Cloud Formation
Expands as condenses due to thinner air
Dew Point breached
Rising air cools to the dew point
8
Humidity
  • The Relative Humidity is the percentage of water
    vapor in a parcel of air.
  • According to the previous diagrams, what time of
    day is the relative humidity the highest?
  • Early morning and late evening
  • Is there any difference between 80 humidity in
    the summer and winter?

9
Mr. Bacciles Demonstration
  • When the air is heated it expands. Therefore,
    there is more room to fit water vapor. So 80
    humidity in the summer is actually much more
    water vapor in the air.

summer
winter
10
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11
Figuring Dew Point and Humidity
  • A sling-psychrometer is the tool used for
    figuring this
  • There is a wet-bulb and a dry-bulb on the tool
  • The wet-bulb measures the amount of moisture in
    the air.
  • How does this work?

12
The Wet-bulb
  • The same reason why you feel cool after swimming
    in the summer
  • If the air is dry, then there is a lot of room
    for water vapor in the air.
  • Therefore, the water on your skin will evaporate
    quickly into the air
  • Evaporation is cools its surroundings, therefore
    your skin feels colder

13
  • Clear Skies very little moisture in the air
    more room in the air for evaporation cooler
    skin (wet-bulb)
  • This will cause a big difference between the
    wet-bulb and dry-bulb
  • Cloudy Skies lots of moisture in the air less
    room in the air for evaporation less change in
    temp. (wet-bulb)
  • This will cause a Small difference between the
    wet-bulb and dry-bulb

14
The Wet-Bulb cont.
  • The wet-bulb works the same way. When you spin
    it, the dry bulb reads the air temperature and
    the wet-bulb reads the moisture
  • If the air is dry, there will be a big difference
    between the two temperatures
  • If the air is very moist, then both will be
    similar

15
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16
Using the E.S.R.T.
  • If the dry-bulb temperature is 20 degrees and the
    wet-bulb is 15 degrees, what is the dew point and
    humidity.
  • First take difference between the wet-bulb and
    dry bulb 5 degrees
  • Now, use the difference number 5 and the dry bulb
    temperature 20

17
Energy at the Earths surface
  • Energy interacts at the Earths surface in many
    ways
  • It reflects (bounces off), refracts (bends),
    scatters (like reflection but in all directions),
    absorbs (soaks in) and radiates (gives off)
  • It is important to remember if an object is a
    good radiator then it is also a good absorber

18
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19
REFLECTION
  • Electromagnetic energy bounces off a medium
  • The surface needs to be light in color and
    flat!!!
  • The angle of incidents needs to match the angle
    of reflectionlet me show you

20
ANGLE OF INCIDENTS
ANGLE OF REFLECTION
21
ABSORPTION
  • When the radiation is soaked into the ground like
    a sponge it is absorbed
  • The best surface for this is dark colors and
    rough surfaces!!!!
  • It is very important to remember if a surface
    absorbs energy fast, it will also radiate it fast
    (if something warms fast then it cools fast)
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