Transcript Atmosphere
Atmosphere
Composition of the Earth’s
Atmosphere
The
atmosphere is a mixture of gases
with some suspended solids and
liquids.
Nitrogen is the most common gas at
78% of the atmosphere.
Oxygen is the next most common gas
at 21%
Composition of the Atmosphere
Earth’s Atmosphere
Trace
amounts of other gases are
found that total only 1 %: water vapor,
Carbon Dioxide, Neon,
Methane,Ozone, Hydrogen, Helium
Other Planets’ Atmospheres
Earth’s Atmosphere
Brown
Smog is made from nitrogen
oxides and hydrocarbons. (L.A. type)
Gray Smog is from burning coal or oil
and contains sulfur oxides.
Ozone is a pollutant when it is near the
ground. It is in most smogs.
Structure of the Atmosphere
There
are five main layers in the
atmosphere.
The lowest layer is the Troposphere.
The Stratosphere and Mesosphere are the
next highest layers.
The Thermosphere and then the
Exosphere are the highest layers.
Layers of the Atmosphere
Layers of the Atmosphere
A. The Troposphere:
1.Close to the ground
2. Contains 75% of the Earth’s gases.
3. Weather, clouds and smog occur at this
level.
It ends at 10 Km above sea level.
Layers of the Atmosphere
Layers Of the Atmosphere
B. The Stratosphere
The ozone layer is within the stratosphere. It is a
thin layer of O3 which absorbs UV radiation.
C. The Mesosphere is the middle layer.
D. The Thermosphere contains the ionosphere.
The ionosphere is a layer of electrically charged
particles. Radio waves bounce off of it.
E. The Exosphere is the highest level before
space.
Atmospheric Pressure
Gases
in the atmosphere have mass and
weight. Gravity pulls on the
molecules and causes pressure.
Pressure is force exerted on an area.
P= F/A
At sea level there are more molecules of air
above an area, so there is more pressure.
Units for Pressure
The S.I. Unit for pressure is Atmospheres
(Atm)
The old unit used on T.V. is inches Hg
( Which is mercury)
A metric unit is mm Hg ( millimeters)
Another unit used is millibars (mb)
Temperature in the Atmosphere
NAME
Exosphere
Height
(Km)
500 Km
Temperature
(Celcius)
600-1000
Thermosphere
200 - 500
0-600
Mesosphere
50 -150
-5 to 0
Stratosphere
10 - 50
-60 to -5
Troposphere
0 – 10
-60 to 50
The Ozone Layer
20 Km above sea level
Ozone is 3 atoms of oxygen.
Located in the Stratosphere.
Ozone absorbs UV radiation from the sun.
ODP’s = Ozone Depleting Gases
CFC’s are ODP’s… Chlorofluorocarbons
CFC’s break the ozone down to oxygen molecules
Energy from the Sun
Radiation is the transfer of energy by
electromagnetic waves. EM waves
30% of the radiation from the sun is
reflected off of the Earth.
50% of the radiation is absorbed by Earth’s
surface.
Clouds and the atmosphere absorb 20 % .
Energy Transfer in the
Atmosphere
Conduction – the transfer of energy when
molecules bump into one another.
Air near the heated surface of the Earth is
heated by conduction.
Energy Transfer…
Convection - the transfer of heat by the
flow of materials.
Heated air is less dense and rises, cold air
sinks. This flow of air is called a
convection current.
The Water Cycle
The Hydrosphere = All of the water on the
Earth’s surface.
97% of water is salt water, only 3% is fresh.
67% of the fresh water is frozen at the polar
ice-caps , which are 2 miles thick in some
places.
The Water Cycle
The Water Cycle
Water evaporates and becomes a gas.
The evaporated water rises in the
atmosphere.
As the water rises, it cools.
As the gaseous water cool, it condenses to
form a liquid…clouds.
Precipitation is next; the water falls as rain,
snow, sleet, or hail.
Water Cycle
Water
is recycled constantly.
Water is purified through the water
cycle.
Movement of Air
Wind is caused by the uneven heating of the
Earth’s surface and atmosphere.
Areas of temperature difference create areas
of pressure difference.
Wind is the movement of air from areas of
high pressure to areas of low pressure.
Movement of Air
The
Coriolis Effect = the rotation of the
Earth shifts the wind to the right and north.
The Jet streams = high altitude, strong
winds. The flow west to east in the U.S.
The Jet stream has a major effect on
weather.
Movement of Air
Movement of Air
Sea Breezes – created during the day
because solar radiation warms the land
more than the water. It comes in from the
sea.
Movement of Air
Land Breezes – created at night, cold air
over the land forces up the warmer air over
the sea. The wind goes out to sea.
Monsoon winds are seasonal winds that
occur in tropical areas. ( This creates a wet,
very rainy season.)
Tools of Meteorology
Anemometer
Barometer
Psychrometer
Rain Gauge
UV Meter
Weather Satellite
Weather Balloon