Air Parcels
Energy Transfer
Humidity
Temeprature
Changes
100

This is an amount of air that moves as a unit.

Air parcel

100

This is the ultimate source of energy that causes weather to occur on Earth.

The sun

100

The gaseous form of water is known as this.

Water vapor

100

This is the measure of how hot or cold something is.

Temperature

100

This is the process by which a solid becomes a liquid.

Melting

200

An air parcel over the Pacific Ocean would have this characteristic.

High humidity

200

If an air parcel is warmer than the surrounding air, then this will happen.

Energy will transfer from it to the surrounding air

200

Water vapor in the air is specifically known as this.

Humidity

200

After an air parcel is warmed, it will do this in the troposphere.

Rise higher

200

This is the process by which a liquid becomes a solid.

Freezing

300

An air parcel over Antarctica would have these two characteristics.

Low temperature and low humidity

300

Energy transfer always happens in this direction.

From higher to lower energy

300

An air parcel that has higher humidity could result in a storm with greater amounts of this.

Precipitation

300

The temperature of an air parcel will decrease until is is the same as this.

The temperature of the surrounding air

300

This is the process by which a liquid becomes a gas.

Evaporation

400

Air parcels can rise higher and lower in this layer of Earth's atmosphere, where weather occurs.

Troposphere

400

In the thermometers we've used in class to measure air temperature, energy transfers from air molecules to this liquid inside.

Alcohol

400

Clouds form when this happens to the water molecules in the air.

They lose energy (energy transfers out)

400

If you have two air parcels with different starting temperatures, this is the one most likely to result in more rainfall.

The warmer one

400

This is the process by which a gas becomes a liquid.

Condensation

500

Air parcels are full of air molecules. The most abundant being this gas.

Nitrogen

500

The energy that causes the warming of the atmosphere comes directly from this.

Earth's surface

500

Dew point is the temperature at which liquid water droplets begin to do this.

Form

500

Higher temperatures have this effect on humidity.

Higher humidity

500

Phase changes occur because this changes.

The kinetic energy of the molecules (temperature)

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