EARTH'S ATMOSPHERE
LAYERS OF THE ATMOSPHERE
TEMPERATURE
ENERGY TRANSFER
Misc
100

the most abundant gas in the atmosphere

nitrogen

100

the layer where weather is found

troposphere

100

the primary motion responsible for day and night

rotation

100

when you touch a hot spoon, heat is transferred by

conduction

100

produces a larger number of weaker rays that travel in different directions

scattering

200

the gas that makes up about 21% of the atmosphere

oxygen

200

where the ozone layer is found

stratosphere

200

the primary motion responsible for seasons

revolution

200

the type of energy transfer that happens in a pot of hot water

conduction

200
this is the distance above sea level
altitude
300

excess of this gas contributes to global warming

carbon dioxide

300

the "hot layer" of the atmosphere

thermosphere

300

two causes for temperature variation not related to water

latitude, cloud cover, altitude

300

the type of heat transfer that can happen in a vacuum 

radiation

300

the energy transferred from one object to another because of a difference in the objects’ temperature.

heat

400

condition of the earths atmosphere at a given point in time

weather

400

this happens to temperature as altitude increases in the troposphere

decreases

400

lines that connect areas of the same temperature

isotherms

400

Many clouds reflect a lot of sunlight because they have a high

albedo

400

first day of winter and summer

solstice

500

condition of the earth's atmosphere on average over a period of time

climate

500

layer that protects earth from meteors

mesophere

500

This heats and cools more rapidly and leads to a greater variation in temperature

land

500

occurs when light bounces off an object- it keeps the same intensity

reflection

500

the first day of spring and autumn

equinox

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