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
Troposphere
Stratosphere
Mesosphere
Thermosphere
Exosphere
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
Temperature decreases with altitude
Stratosphere
Air flow is more stable than troposphere
Contains ozone layer which protects from harmful UV rays
Temperature increases with altitude
Mesosphere
Temperature decreases with altitude
Coldest layer of atmosphere
Burns up most meteors and asteroids before reaching Earth's surface
Thermosphere
Closer to the sun, absorbs a large amount of solar radiation
Temperature increases tremendously with distance from Earth
International Space Station and space shuttles orbit in 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
The basis for scientists dividing the atmosphere into different layers is the change of temperature with height
Auroras are bands of light with different colors, called aurora borealis in the north and aurora australis in the south
Auroras can be seen in the ionosphere, which is an ion-rich region found within the thermosphere
Latitude
Measures the distance north or south of the equator
Latitude lines
Start at the equator (0 degrees latitude) and run east and west, parallel to the equator
Equator
A circle of latitude that divides a spheroid, such as Earth, into the Northern and Southern hemispheres
On Earth, the Equator is an imaginary line located at 0 degrees latitude, about 40,075 km in circumference, halfway between the North and South poles
Longitude
Measures distance east or west of the prime meridian
Lines of longitude
Also called meridians, are imaginary lines that divide the Earth and run north to south from pole to pole
Prime meridian
The line of 0° longitude, the starting point for measuring distance both east and west around Earth
The prime meridian is arbitrary, meaning it could be chosen to be anywhere
The imaginary lines of latitude and longitude intersect each other, forming a grid that covers Earth
Coordinates
The points of latitude and longitude that can be used together to locate any point on Earth
Latitude and longitude
Broken into degrees, minutes, seconds and directions, starting with latitude
An area with coordinates marked 41° 56' 54.3732" N, 87° 39' 19.2024" W would be read as 41 degrees, 56 minutes, 54.3732 seconds north; 87 degrees, 39 minutes, 19.2024 seconds west
Tropical Zone
The Tropic of Cancer and the Tropic of Capricorn, where countries experience a tropical climate with an annual average temperature above 18°C
Temperate Zone
Between the Tropic of Cancer and the Arctic Circle in the north, and between the Tropic of Capricorn and the Antarctic Circle in the south, where countries go through four seasons
Polar Region or Frigid Zone
Areas within the Arctic Circle and Antarctic Circle, where temperatures never go above 10°C even in summer
Using latitude and longitude is not the only way to describe the location of a certain area, another way is by identifying the landmasses and bodies of water that are found in that area
Natural resources
Materials that can be used to support life and provide energy, supplied by the sun or Earth's natural processes
Renewable resources
Natural resources that can be replenished or regenerated naturally over time, either through natural processes or human intervention
Non-renewable resources
Natural resources that exist in finite quantities and cannot be replenished or regenerated within a human lifespan or over geological timescales
Atmosphere
A layer of gases surrounding a planet or other celestial body held in place by gravity
Troposphere
The layer closest to the Earth's surface, where weather occurs and contains the majority of the atmosphere's mass
Stratosphere
Above the troposphere, where the temperature generally increases with altitude due to the ozone layer
Mesosphere
Above the stratosphere, where temperatures decrease with altitude again
Thermosphere
Beyond the mesosphere, where temperatures increase significantly with altitude due to the absorption of solar radiation
Exosphere
The outermost layer of the Earth's atmosphere, where atmospheric particles escape into space