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Earth’s Changing Atmosphere
Main Topics• Definition and Characteristics of the Atmosphere• Changes to the Atmosphere composition• Layers of the Atmosphere Characteristics• How the Earth gets its energy / heat• 3 Types of Heat Transfer
– Radiation, Conduction, Convection
• Forms of Radiation• Ozone Layer• Greenhouse Effect
The Atmosphere makes life on Earth possible
• Atmosphere –The whole layer of air that surrounds
Earth–A mixture of gasses–Keeps Earth warm–Protects life
The atmosphere protects life by:• Absorbing harmful radiation• Maintaining Earth’s temperature• Providing elements essential for life
Characteristics of the Atmosphere
• Altitude - the distance above sea level
• Density - the amount of mass in a given volume
– The density of the atmosphere decreases with altitude
– Most of the mass of the atmosphere is close to Earth’s surface
Materials in the Atmosphere
GasGas PercentPercent
Nitrogen (NNitrogen (N22)) 78.0878.08
Oxygen (OOxygen (O22)) 20.9420.94
Argon (Ar)Argon (Ar) 0.980.98
Carbon Dioxide (COCarbon Dioxide (CO22)) 0.040.04
Other ElementsOther Elements 0.010.01
Water Vapor (HWater Vapor (H22O)O) 0-10-1
Gases of Earth's Atmosphere
Natural Processes modify the atmosphere
• The exact amounts of some gases in the air (atmosphere) change depending on: –Location–Time of day –Season–Other factors
Sudden Changes
• Dramatic events may cause a change in the atmosphere
• It may take a long time for the atmosphere to restore balance
• Examples– Volcanic Eruptions – Forest Fires– Dust Storms
The atmosphere has temperature layers
• Density changes with altitude• Temperature changes with altitude• Pattern of temperature changes defines
different layers
Layers of the atmosphere
• Troposphere • Stratosphere• Mesosphere• Thermosphere• Exosphere
The Layers
Troposphere• Lowest layer• Decreases in Temperature• Includes weather, birds, clouds
Stratosphere• 2nd Layer• The lower end of it is extremely cold
– Temperature increases
• Ozone, weather balloon, and planes are found here
Mesosphere
• 3rd layer• Temperature decreases• Very strong winds• Very little information
about layer• Contains meteors
Notice the temperatures
Thermosphere• 4th Layer• Temperature increases• Very thin• Contains the Aurora Borealis, space
crafts
Exosphere
• Last Layer–Not always considered a layer…still
debated
• Gradually fades into the vacuum that is space………
• Contains satellites
How does the Earth get heated?
• Energy transfer from the sun
Energy
• The ability to do work or cause change• Temperature
– The average amount of energy of motion of each molecule (the measure of how hot or cold something is)
• Gas– Moving particles, the hotter they get the
faster they move
The atmosphere moves energy
• Energy moves by heat transfer• There are 3 types of heat transfer
– Radiation– Conduction– Convection
Radiation• The transfer of the Sun’s energy to the Earth’s
surface• Solar radiation heats both the surface and the air
– Includes visible light• Earth’s surface gives off a type of invisible radiation
called Infrared radiation
Earth’s absorption of Radiation• 30% of incoming solar energy is reflected by clouds• 70% is absorbed and becomes different forms of
energy– Absorbed by oceans, landforms, and living things
(photosynthesis and respiration)
• This absorbed energy heats the Earth’s surface
Conduction
• The transfer of heat energy from one substance to another through DIRECT contact
• The Earth’s surface heats the air (gas) molecules directing above it
• Molecules of air gain energy when they collide with the molecules in grains of hot sand.
Convection
• Transfer of energy from place to place by the motion of gas or liquid (fluids)
• Up and down movement of molecules not the side to side movement
Density and Convection
• The atmosphere gets less dense at higher altitudes
• Warm air is less dense than cold air– Warm air has more energy, so
molecules move faster than cold ones– This makes them collide more, then
they spread out– More space between molecules = less
dense
Transfer of Energy
Gases Absorb and Give Off Radiation
The Atmosphere affects light in 4 ways.1. Absorbs Light2. Reflects Light3. Lets Light Pass Through4. Emits (Gives Off) Light
On sunny days more visible light gets to the earths surface.
On cloudy days clouds reflect and absorb most of the sunlight
Forms of Radiation We Cant See
• Ultraviolet Radiation– More energy than the light
you can see– Can cause sunburns and
other damage
• Infrared Radiation– Less energy than the light
you can see– Warms the materials that
absorb it
Ozone Layer Protects Life• Ozone - O3
– Ozone in stratosphere is called the ozone layer
– Protects life on Earth– Absorbs harmful ultraviolet
radiation from sun• Too much can cause
sunburn, skin cancer, and can harm crops, plastic or paint
– Lets other types of radiation like visible light through
Greenhouse Effect• Keeps Earth Warm• Slow the movement of energy away from the Earth’s
surface• Greenhouse gases
– Includes carbon dioxide, methane, water vapor, and nitrous oxide
– Gases mix with gases in the air like nitrogen and oxygen. Not its own layer
– Found in the troposphere– Absorbs and emits infrared radiation
Animation