1/37
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced | Call with Kai | Chat |
|---|
No analytics yet
Send a link to your students to track their progress
Plants
Determine the type of biome in an area.
Weather
Current and short-term atmospheric conditions. Ex: it is raining today.
Climate
Long-term atmospheric conditions over a long period of time in a certain area. Ex: The average temperature in Townsville on October 13th is 78 degrees.
Nitrogen
The 1st most prevalent gas in the dry sea level troposphere. 78%.
Oxygen
The 2nd most prevalent gas in the dry sea level troposphere. 21%.
Argon
The 3rd most prevalent gas in the dry sea level troposphere. 1% (0.934%).
Carbon dioxide
The 4th most prevalent gas in the dry sea level troposphere. 0.04%.
Troposphere
The layer of the atmosphere that life takes place in. Weather and the greenhouse effect (CO2, H2O, N2O, CH4, CFCs) take place here. Temperature decreases with higher altitude. The tropopause is its boundary.
Stratosphere
The 2nd layer of the atmosphere (going up). The ozone layer (earth’s sunscreen) is found here. Temperature increases with higher altitude. The stratopause is its boundary.
Mesosphere
The 3rd layer of the atmosphere (going up). Temperature decreases with higher altitude. The mesopause is its boundary.
Thermosphere
The 4th layer of the atmosphere (going up). Temperature increases with higher altitude.
Exosphere
The 5th layer of the atmosphere (going up). Temperature decreases with higher altitude.
How cold fronts cause rain
Cold air is dense, so as it advances, it pushes air ahead of it upward. This rising air expands and cools, causing water to condense, leading to rain.
Low pressure
Vertical air movement: Rising
Horizontal air movement: Counterclockwise
General weather: Clouds, rain, storms, hurricanes
High pressure
Vertical air movement: Sinking (descending)
Horizontal air movement: Clockwise
General weather: Sunny to fair (few clouds)
Affects evaporation of sweat
How humidity affects human comfort.
How curvature of the earth leads to uneven heat distribution
The sun shines directly on the equator, but its energy is dispersed as you move poleward.
The hemisphere that is tilted toward the sun is experiencing the most heat.
How the tilt of the earth on its axis causes the seasons.
Circulation cells
Develop due to Earth’s rotation and uneven solar heating across Earth’s surface. They transport excess heat away from the tropics and give the heat to the poles. They create tropical rainforests with rising air, create deserts with sinking air.
The sun is on varying cycles of intensity
How the sun influences global climate.
Ocean currents
Winds off South America blow offshore (westward), pushing surface water westward and bringing up cold, nutrient rich water.
Upwelling
The process where cold, nutrient-rich water is brought to the surface.
El Nino
Every 2-7 years, this occurs. Interactions between the oceans and the atmosphere cause the normal winds to slacken or reverse.
It causes pooling of warm water to the South American coast, suppression of upwelling, and reduced fishing success.
La Nina
An enhanced version of the normal ocean currents (Winds off South America blow westward and cause warmer waters on the Pacific coast of Asia)
Rainshadow effect
Urban heat island
Mountain climate
How bodies of water can have an influence on weather and climate.
Biomes
Latitude variations
Altitude variations
Tropics
Temperate zone
Polar
Polar easterlies
Located higher than 60° N and lower than 60° S.
60°N: Wind direction is northeast.
60°S: Wind direction is southeast.
Westerlies
Located between 30°N and 60°N, as well as between 30°S and 60°S
30°N-60°N: Wind direction is southwest.
30°S-60°S: Wind direction is northwest.
Northeast tradewinds
Located between the equator and 30°N. Wind direction is northeast.
Southeast tradewinds
Located between the equator and 30°S. Wind direction is southeast.