Medium for weather activity, regulates temperature
Oxygen for respiration
Carbon dioxide for photosynthesis
Allows sound to be heard
Troposphere
10km high<|>75% of total mass of atmosphere & 99% of atmosphere's water<|>Wind, clouds, and water vapor<|>Weather activity occurs<|>Temperature decreases as altitude increases
Stratosphere
Flow of air is stable<|>Temperature increases with altitude<|>Where ozone layer exists (40-60 km high)
Mesosphere
Temperature decreases with altitude<|>Coldest layer of earth<|>Where meteors disintegrate due to its temperature
Thermosphere
Absorbs large amount of solar radiation. <|>Temperature increases as distance becomes greater<|>Where international space station and space shuttle flies<|>Where aurora display happens
Aurora borealis
Northern lights
Aurora australis
Southern lights
Ionosphere
Iron rich region of thermosphere
Exosphere
Temperature varies from very hot to very cold<|>Has artificial satellites due to no friction
Lithosphere
Soil part of earth<|>100km<|>Made of granite continental crust, basaltic oceanic crust
Soil components
Clay: fine particles
Silt: larger than clay but smaller than sand
Sand: largest particle, holds nutrients
Loam: accumulation of clay, silt, sand, and humus (decayed plant and animal material)
Hydrosphere
Saltwater: 93% of earth's water
Freshwater: 7% of earth's water
Snow/glacier: largest source of water
Ground water: man's primary source of water
Hydrologic cycle
1. Evaporation: heat from sun converts water to water vapor
2. Condensation: water vapor releases heat turning into droplets to form precipitation
Mix of daily atmospheric events that vary across different regions and change rapidly over short periods of time
Atmosphere
Composed mainly of nitrogen with traces of other gases, surrounds the Earth and is held in place by gravity
Temperature
Measure of the kinetic energy within the particles of an object, or how hot or cold an object is
As height above sea level increases
Temperature decreases
Collision of hot and cold air masses
Can affect the weather due to the differences in the density of the air masses
Air pressure
Amount of pressure exerted by the air in a particular air mass
Air pressure
The number of air molecules above a surface determines air pressure. As the number of molecules increases, they exert more pressure on a surface, and the total atmospheric pressure increases
The normal range of the Earth's air pressure is from 970 MB to 1,050 MB
Low pressure system
An area with lower atmospheric pressure compared to its surroundings
Low pressure system
Brings high winds, warm air, and atmospheric lifting
Produces clouds, precipitation, and other turbulent weather, such as tropical storms and cyclones
Brings warmer weather, storms, and rain
High-pressure system
Also called an anticyclone, an area where the atmospheric pressure is greater than that of the surrounding area
Movement of high-pressure systems
1. Clockwise in the Northern Hemisphere
2. Counterclockwise in the Southern Hemisphere
3. Due to the Coriolis Effect
High-pressure systems
Caused by subsidence
Bring cool temperatures and clear skies
Wind
Movement of air, forms because of differences in temperature and atmospheric pressure between nearby regions
Wind is the great equalizer of the atmosphere, transporting heat, moisture, pollutants, and dust great distances around the globe
Front
Boundary between high pressure and low pressure
Relation of front
Causes different types of wind and weather patterns
Humidity
Amount of moisture, or water vapor in the air
Humidity
Affects the weather by leading to the formation of clouds and precipitation
Can make an area feel warmer with high humidity, or cooler with low humidity
Warm and tropical areas are typically very humid
Precipitation
Any liquid or frozen water that forms in the atmosphere and falls back to the earth
Formation of precipitation
Water vapor condenses into bigger and bigger droplets of water in the clouds