14.1
Composition |
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Review Questions
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Gases |
78%
21 % |
Nitrogen
Oxygen |
1% |
Water Vapor up to 4%
Argon 0.93%
CO2 0.03%Neon
Helium
Methane
Krypton et.al. |
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Liquids, Solids |
Dust, salt, ice, liquid water |
| Structure |
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Lower Layers

Click on image
to see it larger |
Troposphere
Containing 75%
of the above listed components from the surface to the stratosphere where the weather is.Stratosphere
contains
the jet stream
contains ozone
layer
Ozone blocks ultraviolet (UV) radiation from
the sun
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Upper Layers |
Mesosphere
Thermosphere contains the Ionosphere
which is made of ions, which are electrically charged particles, and free
electrons
Exosphere which
is the last layer before space.
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| Atmospheric Pressure |
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Air is made of matter,
matter has mass,
therefore Earth's gravity keeps the atmosphere near the
surface,
which in turn exerts pressure on you and everything else on
the surface.
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Atmospheric pressure decreases as elevation
above mean sea level increases. |
| Temperature |
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Layers are defined by temperature.
Atmosphere absorbs energy directly from sun,
reflected and radiated from earth surface,
reflected and radiated from elsewhere in the atmosphere. |
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14.3 Energy
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Energy
Transfer |
The sun is the ultimate source of all our energy. |
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Radiation |
Electromagnetic waves send the sun's energy all the way to
earth.
This is what you can
feel by facing the sun, and absorbing this energy through you skin. You interpret
this as heat.
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Conduction |
Direct contact with an energy source.
This is how you can be burned by a hot stove.
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Convection |
The flow of a heated fluid (gas or liquid) carries energy
with it.
The primary mechanism
is the change in density caused by temperature differences:
warm air is less dense and rises
cold air is denser and sinks
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Water Cycle |
All our water moves from ocean to atmosphere to land and
back again.Diagram....A Simpler Diagram |
14.4
Movement |
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Primary cause of atmospheric movement (winds) is uneven
heating of the earth's surface.
The angle of
incidence, that is, the angle at which the sun's rays strike the earth's surface, is
greatest in the tropics (within 23 ½º of the equator) and least near the
poles.
Remember:
warm air is less dense and
rises, and
cold air is denser and sinks
This causes warm air to rise from the tropics, and move
horizontally toward the poles,
and for colder air to be pushed towards the tropics
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Coriolis Effect |
The deflection of moving fluids by the rotation of the
earth.
Toward the right in
the northern hemisphere,
and toward the left in the southern.
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Jet Stream |
A high altitude narrow belt of high winds, blowing from
west to east.
2 main ones in each
hemisphere.
Main directional force behind our surface weather.
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Surface Winds |
Divided into belts of winds that blow primarily
from one direction.[Another Map] |
| Daily changes |
Sea/Land Breezes |
Water absorbs and releases heat slower than land.
During daylight, the sun heats the land up and the cooler
air over the ocean moves toward land.
At night, the land cools off quicker than the water, and
the cooler air over the land moves toward the water.
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| Seasonal changes |
Monsoons |
In the tropics, the seasonal differences of the sun's angle
of incidence causes a variation on the sea/land breeze scenario noted above.
This results in wet/dry seasons. |
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| Weather |
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| 15.1 |
Weather |
is a description of the current conditions .
Right now, it is hot, or cold, it is raining, or clear.
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Factors
that determine the weather: |
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Humidity |
The amount of water vapor in the air.
Directly related to the temperature:
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The higher the temperature, the more water the air can
hold.
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Relative Humidity |
is the measure of how much water the air is holding,
vs. how much it can hold, at a specific temperature.
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Dew Point |
is the temperature at which the air is saturated and the
water in it can condense.
So that's
what causes clouds to form!
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| Clouds |
Cloud Types |
Cloud types |
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