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Free Online Flashcard Deck

2 Atmospheric Moisture and Cloud Formation Free Online FlashCards

Study 2 Atmospheric Moisture and Cloud Formation with 12 free online flashcards. Review key terms, definitions, and concepts with this interactive flashcard deck.

12 cards
01
Front

What does humidity describe?

Back

Humidity describes the amount of water vapor in the air.

02
Front

What does relative humidity compare?

Back

Relative humidity compares the water vapor present with the amount needed to saturate the air at its current temperature. Air at 100% relative humidity is saturated.

03
Front

How can temperature change relative humidity without changing water vapor?

Back

Warming raises the amount of water vapor needed for saturation, so relative humidity can fall. Cooling can raise relative humidity even when the water-vapor content stays the same.

04
Front

What is the dew point?

Back

The dew point is the temperature air must reach by cooling, at constant pressure and with no change in water-vapor content, to become saturated.

05
Front

What happens during evaporation, and what does it require?

Back

Evaporation changes liquid water into water vapor. It requires energy, commonly supplied by sunlight and the surrounding air.

06
Front

How do plants add water vapor to the atmosphere?

Back

Transpiration is the release of water vapor from plants; it adds moisture to the atmosphere.

07
Front

What role do condensation nuclei play in cloud formation?

Back

When air becomes saturated, water vapor can condense onto tiny particles called condensation nuclei, such as dust, sea salt, or smoke. The resulting droplets or ice crystals can form clouds.

08
Front

What happens to energy when water vapor condenses?

Back

Condensation changes water vapor into liquid water and releases energy to the surrounding air.

09
Front

What may clouds contain below freezing?

Back

At temperatures below freezing, clouds may contain ice crystals as well as, or instead of, liquid droplets.

10
Front

How do maritime tropical and continental polar air masses differ?

Back

An air mass takes on characteristics of the region where it forms. Maritime tropical air is generally warm and humid, while continental polar air is generally cold and dry.

11
Front

How can a front contribute to cloud formation?

Back

Where air masses meet, fronts can force air upward and contribute to cloud formation.

12
Front

Why does rising air cool higher in the atmosphere?

Back

Higher in the atmosphere, pressure is lower. Rising air expands in this lower pressure and cools.