3. Water In The Atmosphere Flashcards

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1
Q

evaporation

A

change in the state of water from liquid to gas

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2
Q

condensation

A

change in the state of water from gas to liquid

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3
Q

hydrologic cycle

A

movement of water within the atmosphere, biosphere, lithosphere, and hydrosphere

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4
Q

transpiration

A

loss of water to the atmosphere by plants

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5
Q

hydrogen bond

A

bond between water molecules that results from the attraction between one water molecule’s positive end and another’s negative end

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6
Q

latent heat

A

energy that is absorbed or released during a change in the state of a substance, such as during evaporation or condensation of water

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7
Q

saturation

A

point at which an air parcel’s water vapor content is equal to its water vapor capacity

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8
Q

humidity

A

the amount of water vapor in the atmosphere

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9
Q

evapotranspiration

A

combined processes of evaporation and transpiration

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10
Q

hygrometer

A

instrument used to measure humidity

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11
Q

vapor pressure

A

portion of air pressure exerted exclusively by molecules of water vapour

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12
Q

millibar (mb)

A

measure of atmospheric pressure; average sea level pressure is 1013.25 mb

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13
Q

saturation vapor pressure

A

vapor pressure at which saturation occurs

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14
Q

specific humidity

A

water vapor content of the atmosphere, expressed in grams of water per kilogram of air (g/kg)

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15
Q

relative humidity (RH)

A

ratio of water vapour content to water vapour capacity, expressed as a percentage

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16
Q

air parcel

A

body of air of uniform humidity and temperature

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17
Q

dew point

A

temperature at which air becomes saturated

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18
Q

adiabatic cooling

A

cooling of an air parcel through expansion

19
Q

adiabatic warming

A

warming of an air parcel through compression

20
Q

dry adiabatic rate

A

rate of temperature change in an unsaturated parcel of air; 10°C/1, 000 m

21
Q

lifting condensation level (LCL)

A

altitude at which an air parcel becomes saturated

22
Q

moist adiabatic rate

A

rate of cooling in a saturated air parcel; usually about 6°C/ 1, 000m

23
Q

stable atmosphere

A

condition in which air parcels are cooler and denser than the surrounding air and will not rise unless forced to do so

24
Q

unstable atmosphere

A

condition in which air parcels rise on their own because they are warmer and less dense than the surrounding air

25
Q

rain shadow

A

dry, leeward side of a mountain range

26
Q

convective uplift

A

rising of an air parcel that is warmer and less dense than the surrounding air

27
Q

orographic uplift

A

rising of air over mountains

28
Q

frontal uplift

A

rising of warm air masses where they meet relatively cold air masses

29
Q

convergent uplift

A

rising of air as a result of converging airflow

30
Q

cloud

A

aggregation of microscopic water droplets and ice crystals suspended in the air

31
Q

cirrus

A

high cloud with a feathery appearance that is composed of ice crystals

32
Q

cumulus

A

dome-shaped, bunched cloud, with a flat base and billowy upper portions

33
Q

stratus

A

cloud type characterized by low, flat sheets of clouds

34
Q

nimbostratus

A

rain-producing low-level sheets of clouds

35
Q

cumulonimbus

A

cloud that extends high into the atmosphere and is capable of strong vertical development and of producing severe weather

36
Q

fog

A

cloud at or near ground level that reduces visibility to less than 1km

37
Q

radiation fog

A

fog that results when the ground radiates its heat away at night, cooling the air above it to the dew point

38
Q

advection fog

A

fog that results from moist air moving over a cold surface, such as a lake or a cold ocean current, that lowers its temperature to the dew point

39
Q

condensation nucleus

A

small particle in the atmosphere, about 0.2 Mm in diameter, on which water vapour condenses

40
Q

collision and coalescence

A

process by which cloud droplets merge to form raindrops

41
Q

ice-crystal process

A

the process by which ice crystals grow within a cloud to form snow

42
Q

hail

A

hard, rounded pellets of ice that precipitate from cumulonimbus clouds with strong vertical airflow

43
Q

negative feedback

A

process in which interacting parts in a system stabilize the system

44
Q

positive feedback

A

process in which interacting parts in a system destabilize the system