Ch.4 : humidity,Condensation, Clouds Flashcards

0
Q

Condensation

A

water vapor changes back to liquid

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1
Q

evaporation

A

sun’s energy transforms enormous quantities of liqiud into water vapor

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2
Q

saturation

A

condensation & evaporation are equal humidity is now 100% = same # of water leavin the liquid as going back in
for every molecule that evaporates , one musy condense

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3
Q

subsaturation

A

if more evaporation is occurring than condensation, then net evaporation is occurring

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4
Q

supersaturation

A

if more condensation than evaporation is occurring

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5
Q

cloud condensation nuclei

A

air molecules are microscopic bits of dust, smoke and salt, many of these surfaces on which water spray condense

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6
Q

humidity

A

refers to any one of a number of specifying the amount of water vapor in air

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7
Q

relative humidity

A

•ratio of the amount of water vapor actually in the air to maximum amount of water vapor required for saturation at a particular temp & pressure
• its ratio of airs water vapor content to its capacity
R.H = water vapor content/ water vapor capacy

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8
Q

vapor pressure

A

the partial pressure of water vapor

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9
Q

saturation vapor pressure

A

how much water vapor is necessary to make the air saturated at any given temperature

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10
Q

dew point

A

•represents the temp to which air would have to be cooled (with no chamge in air pressure or moisture content) for saturation to occur
•good indicator of the air’s actual water vapor content
•high dew points indicate high water vapor content
low dew point = low water vapor content

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11
Q

dew

A

as surface cools below this temp , water vapor begins to condense upon them , forming tiny visible soecks of water

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12
Q

frost

A

delicate white crystals of ice that form in this manner

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13
Q

fog

A

when visibility lowers to less than 1 km & air is west with millions of tiny droplets, the haze becomes a cloud resting near the ground

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14
Q

cloud

A

visible aggregate of tiny water droplets or ice crystals suspended in the air

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