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Atmosphere
Forms the boundary between Earth and space. It is the outer limit of the biosphere and its composition and processes support life on Earth.
Composition of the Atmosphere
78% nitrogen (N2), 21% oxygen (O2), 0.9% trace gases like argon and carbon dioxide (CO2).
Layers of the Atmosphere
Troposphere (where most weather occurs)
Stratosphere (ozone layer)
Mesosphere
Thermosphere
Exosphere
Insolation
Refers to incoming solar radiation.
Heat Islands
Geothermal Heat
Thermal energy in the Earth’s crust.
Tectonic Regions
Areas of the Earth that are close to tectonic plate boundaries or where the plate is thin enough to allow geothermal heat to rise to the surface.
Tectonic Plate
Latitude
The position of a place on Earth relative to the equator.
Tropopause
The atmospheric boundary layer that separates the troposphere (below) from the stratosphere (above).
Tricellular Atmospheric Circulation
There are three circulation cells: Hadley, Ferrel, and Polar cells. These cells redistribute heat and influence weather patterns.
Tricellular Model
Explains how heat is distributed from the equator to the poles.
Coriolis Effect
Causes the atmosphere to move faster at the equator than at the poles.
Prevailing Winds
Surface winds that blow (go) predominantly from a single, most frequent direction over a specific region of the Earth.
Jet Streams
Fast-flowing, narrow bands of wind high up in the atmosphere.
Atmosphere System Inputs and Outputs
