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"To the dull mind all nature is leaden. To the illumined mind the whole world burns and sparkles with light." -- Ralph Waldo Emerson

Earth's Atmosphere, Weather, and Climate

 

14.1
Composition

Review Questions

Gases
78%
21 %
Nitrogen
Oxygen

1%

Water Vapor up to 4%
Argon
0.93%
CO2
0.03%

Neon
Helium
Methane
Krypton et.al.

Liquids, Solids Dust, salt, ice, liquid water

 

Structure
Lower Layers


Click on image
to see it larger

Troposphere
Bullet7.gif (140 bytes) Containing 75% of the above listed components from the surface to the stratosphere where the weather is.

Stratosphere
Bullet7.gif (140 bytes) contains the jet stream
Bullet7.gif (140 bytes) contains ozone layer 
     Arrow5.gif (101 bytes) Ozone blocks ultraviolet (UV) radiation from the sun

 

Upper Layers Mesosphere

Bullet7.gif (140 bytes) Thermosphere  contains the Ionosphere which is made of ions, which are electrically charged particles, and free electrons

Bullet7.gif (140 bytes) Exosphere
which is the last layer before space.

 

Atmospheric Pressure Air is made of matter,

Bullet7.gif (140 bytes) matter has mass,

Bullet7.gif (140 bytes) Arrow5.gif (101 bytes)therefore Earth's gravity keeps the atmosphere near the surface,

Bullet7.gif (140 bytes) Arrow5.gif (101 bytes)which in turn exerts pressure on you and everything else on the surface.

Atmospheric pressure decreases as elevation above mean sea level increases.

 

Temperature
Bullet7.gif (140 bytes) Layers are defined by temperature.

Bullet7.gif (140 bytes) Atmosphere absorbs energy directly from sun,
reflected and radiated from earth surface,
reflected and radiated from elsewhere in the atmosphere.

14.3  Energy

Energy Transfer

Bullet7.gif (140 bytes) The sun is the ultimate source of all our energy.

 

Radiation Bullet7.gif (140 bytes) Electromagnetic waves send the sun's energy all the way to earth.

Bullet7.gif (140 bytes) This is what you can feel by facing the sun, and absorbing this energy through you skin.  You interpret this as heat.

 

Conduction Bullet7.gif (140 bytes) Direct contact with an energy source.

Bullet7.gif (140 bytes) This is how you can be burned by a hot stove.

 

Convection Bullet7.gif (140 bytes) The flow of a heated fluid (gas or liquid) carries energy with it.

Bullet7.gif (140 bytes)The primary mechanism is the change in density caused by temperature differences:
       Arrow5.gif (101 bytes)
warm air is less dense and rises
       Arrow5.gif (101 bytes)
cold air is denser and sinks

 

Water Cycle Bullet7.gif (140 bytes) All our water moves from ocean to atmosphere to land and back again.

Diagram....A Simpler Diagram

14.4
Movement
Bullet7.gif (140 bytes) Primary cause of atmospheric movement (winds) is uneven heating of the earth's surface.

Bullet7.gif (140 bytes) 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:

Arrow5.gif (101 bytes)warm air is less dense and rises, and
Arrow5.gif (101 bytes)
cold air is denser and sinks

Bullet7.gif (140 bytes) This causes warm air to rise from the tropics, and move horizontally toward the poles,

Bullet7.gif (140 bytes) and for colder air to be pushed towards the tropics

 

Coriolis Effect Bullet7.gif (140 bytes) The deflection of moving fluids by the rotation of the earth.

Bullet7.gif (140 bytes) Toward the right in the northern hemisphere,
and toward the left in the southern.

 

Jet Stream Bullet7.gif (140 bytes) A high altitude narrow belt of high winds, blowing from west to east.

Bullet7.gif (140 bytes) 2 main ones in each hemisphere.

Bullet7.gif (140 bytes) Main directional force behind our surface weather.

 

Surface Winds Bullet7.gif (140 bytes) Divided into belts of winds that blow primarily from one direction.

[Another Map]

Daily changes Sea/Land Breezes Bullet7.gif (140 bytes) Water absorbs and releases heat slower than land.

Bullet7.gif (140 bytes) During daylight, the sun heats the land up and the cooler air over the ocean moves toward land.

Bullet7.gif (140 bytes) At night, the land cools off quicker than the water, and the cooler air over the land moves toward the water.

 

Seasonal changes Monsoons Bullet7.gif (140 bytes) In the tropics, the seasonal differences of the sun's angle of incidence causes a variation on the sea/land breeze scenario noted above.

Bullet7.gif (140 bytes) This results in wet/dry seasons.

Weather
15.1

Weather

Bullet7.gif (140 bytes)  is a description of the current conditions .

Bullet7.gif (140 bytes) Right now, it is hot, or cold, it is raining, or clear.

 

Factors that determine the weather:

Humidity Bullet7.gif (140 bytes) The amount of water vapor in the air.

Bullet7.gif (140 bytes) Directly related to the temperature:

Bullet7.gif (140 bytes) The higher the temperature, the more water the air can hold.
Relative Humidity Bullet7.gif (140 bytes) is the measure of how much water the air is holding,

Bullet7.gif (140 bytes) vs. how much it can hold, at a specific temperature.

 

Dew Point Bullet7.gif (140 bytes) is the temperature at which the air is saturated and the water in it can condense.

Bullet7.gif (140 bytes) So that's what causes clouds to form!

 

Clouds Cloud Types Bullet7.gif (140 bytes) Cloud types

 

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UPDATED: 08/16/03