Earth is the only planet that is known to sustain life in our solar system
One of the factors that make our planet habitable is its atmosphere
Atmosphere
The blanket or envelope of gases surrounding the earth
The atmosphere keeps us warm, gives us oxygen to breathe, and is where weather happens
The atmosphere keeps the overall temperature of the earth fairly steady, especially between night and day
Gases in the earth's atmosphere
78% nitrogen
21% oxygen
1% other trace gases including carbon dioxide, inert gases, hydrogen, methane, ozone
Layers of the atmosphere from ground level upward
Troposphere
Stratosphere
Mesosphere
Thermosphere
Exosphere
Basis for dividing the atmosphere into layers
Change of temperature with height
Troposphere
Lowest layer
Makes up 75% of total mass of atmosphere
Contains 99% of atmosphere's water
Where wind, clouds, and weather phenomena take place
Air is constantly moving
Stratosphere
Air flow is more stable than troposphere
Ozone layer is found here
Protects from harmful UV radiation
Mesosphere
Temperature decreases with height
Coldest layer
Burns up most meteors and asteroidsbefore reaching Earth's surface
Thermosphere
Closer to the sun
Absorbs a large amount of solar radiation
Temperature increases tremendously
International Space Station and space shuttles orbit in this layer
Ionosphere is found within this layer
Exosphere
Merges into outer space
Temperature varies from very hot to very cold
Ideal for placing artificial satellites as there is little friction
Auroras are bands of light with different colors, called aurora borealis in the north and aurora australis in the south
The earth's atmosphere is divided into different layers and is made of different types of gases
More than three quarters of earth's atmosphere is made up of nitrogen while one film is oxygen
The remaining one percent is a mixture of carbon dioxide water vapor ozone and other trace gases
These gases not only produce important weather features such as cloud and rain but also have considerable influence on the overall climate of the earth through the greenhouse effect and global warming
Greenhouse
A structure with walls and roofs made chiefly of a transparent material such as plastic or glass, useful in growing seedlings when this winter or spring before planting them in the open field
Uses of greenhouses
Growing seedlings
Protecting flowering and ornamental plants from harsh weather conditions and insect attacks in tropical countries
How greenhouses work
Transparent covering allows visible light to enter without obstruction
Warms the inside of the greenhouse as energy is absorbed by the plants soil and other things in the building
Air warmed by the heat inside is retained in the building by the roof and wall
Transparent covering prevents the heat from leaving by reflecting the energy back into the walls and preventing outside winds from carrying it away
Greenhouse effect
The process where greenhouse gases trap the heat in the atmosphere
The greenhouse effect is a natural process that warms the earth's surface and makes the earth much warmer than it would be without an atmosphere
The greenhouse effect plays an important role in our survival
Due to different human activities, more greenhouse gases are emitted into the earth's atmosphere which results in an enhanced greenhouse effect
Enhanced greenhouse effect
More heat is trapped and reflected back to the earth's surface due to the higher presence of greenhouse gases
Global warming
The current rise in the average temperature of earth's air and oceans
Sources of greenhouse gas emissions
Burning fossil fuels for electricity, heat and transportation
Deforestation and land clearing for agriculture
Degradation of soils
Agricultural activities
Waste management
Energy use
Biomass burning
Use of fertilizers
Industrial processes
Refrigeration
Use of consumer products
Many of these greenhouse gases can cause earth's atmosphere to trap more and more heat, increase air temperature and cause global warming
Global warming is feared to melt polar ice caps and cause flooding to low-lying areas, resulting in a reduction in biodiversity and changing climates around the globe, causing stronger typhoons and creating many health related problems
There are a number of unique combinations of atmospheric phenomena experienced by people in all parts of the world
Common atmospheric phenomena
Breezes
Monsoons
Intertropical Convergence Zone
How air behaves when heated
1. Air molecules move faster and spread out
2. Makes the air less dense or light
3. Warm air rises
Warm air rises
Surrounding air moves toward it to replace the rising warm air
Wind
Air that is moving horizontally
Land surface heats up faster than bodies of water during the day, but land loses heat faster than bodies of water at night
Breezes
Localized winds experienced by those living in coastal areas
Types of breezes
Sea breeze
Land breeze
Sea breeze formation
1. Land warms up faster than bodies of water during the day
2. Warm air above land rises
3. Cooler air above the sea moves toward the land and replaces the warm air