Clouds
Fog
Humidity
Atmospheric Structure and Composition
Energetics
100

Small particulate needed to promote condensation for cloud formation 

Cloud condensation nuclei (CCN)

100

Fog is really just _______ on the ground

A cloud
100

The name we give air which cannot hold any more moisture content

Saturated

100

These are the 2 gases that primarily compose the atmosphere

Nitrogen and Oxygen

100

The 3 types of heat transfer

Conduction, convection and radiation

200

The prefix given to clouds in the middle layer of the atmosphere

Alto

200

This type of fog occurs when moist air is forced up a mountain slope

Upslope fog

200

The value of relative humidity when air is completely saturated

100%

200

This is the layer of the atmosphere where weather occurs

Troposphere

200

The heat energy required or released during the phase change of a substance

Latent heat

300

The height of clouds that are better at reflecting solar radiation and cooling the earth

Low clouds

300

This type of fog forms on clear, calm nights when moist air near the surface is in contact with the ground.

Radiation fog

300

The rate of evaporation _______ as air gets further from saturation

Increases

300

The 2 layers of the atmosphere where temperature increases with height

Stratosphere and thermosphere

300

The interaction when radiation (light) bounces off a substance and spreads it out in all directions at a lower intensity

Scattering

400

The name given to clouds that extend from low to high altitudes, and are most associated with thunderstorms.

Cumulonimbus

400

This type of fog forms when cold air moves over warm bodies of water

Steam/evaporation fog

400

The temperature to which air must be cooled in order to become saturated

Dew point

400

This is the gas responsible for warmer temperatures in the stratosphere

Ozone

400

Name given to the region of the IR spectrum where there are no significant greenhouse gases to absorb this outgoing radiation

Atmospheric window

500

The height at which a rising air parcel becomes cool enough that water vapor will begin to condense

Lifting Condensation Level

500

This type of fog forms when warm moist air is passed over a cold surface.

Advection fog

500

The term for the amount of water vapor needed to make the air saturated

Saturation vapor pressure

500

The percentage of the atmosphere, by mass, BELOW you when the pressure around you is 800 hPa.

20%
500

This law states warmer objects emit a higher proportion of their energy at shorter wavelengths than colder ones

Wien's Law