Weather 1
Weather 2
Weather 3
Weather 4
Weather 5
100

When liquid water becomes warmer it can __________.

Evaporate

100

The _________ is warmest at the surface and coldest at its highest point.

Troposphere

100

What happens when water vapor cools? Choose all that apply

A. It becomes liquid water

B. It stays the same

C. Energy transfers

D. Clouds form

A. It becomes liquid water

B. It stays the same

D. Energy transfers

100

The energy that transfers out of an air parcel to form clouds originally comes from ___________.

The sun

100

Why do warm temperatures lead to more rainfall?

Warm temperatures lead to more rainfall because the higher it rose, the more energy the parcels lost and the more the water vapor condensed.

200

When does the air parcel stop losing energy? 

Air parcel stops losing energy when it reaches thermal equilibrium with its surrounding environment.

200

What causes an air parcel to stop rising?

Something that causes the parcel to stop rising is when its tempature cools to match or become lower than the surrounding atmosphere.

200

Does higher energy cause more rainfall?

Yes

200

Condensation releases latent heat, slowing the cooling of moist air

Latent heat release


200

Air parcels carry heat energy upward in the atmosphere, contributing to convection

Convection

300

What is wind? 

Wind is air that travels around the world.

300

Rising air cools because the pressure around it decreases with height

Decreasing air pressure

300

An air parcel rises, expands, and cools without exchanging heat with its surroundings

Adiabatic cooling

300

The vertical distance an air parcel moves where its temperature changes due to pressure differences

Altitude or height

300

The process of water turning from a gas into liquid in the atmosphere

Condensation

400

How can wind be related to severe rainstorms?

Wind could push air parcels higher in the troposphere causing severe rainstorms

400

The spreading out of rising air due to lower pressure causes a drop in temperature

Expansion cooling

400

Dry air cools faster than moist air when it rises through the atmosphere

Dry adiabatic rate

400

The type of weather often formed when large air parcels rise over mountains


Orographic precipitation 

400

The invisible gas in the air that condenses to form clouds when an air parcel cools

Water Vapor

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