3. Water In The Atmosphere Flashcards

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
rain shadow
dry, leeward side of a mountain range
26
convective uplift
rising of an air parcel that is warmer and less dense than the surrounding air
27
orographic uplift
rising of air over mountains
28
frontal uplift
rising of warm air masses where they meet relatively cold air masses
29
convergent uplift
rising of air as a result of converging airflow
30
cloud
aggregation of microscopic water droplets and ice crystals suspended in the air
31
cirrus
high cloud with a feathery appearance that is composed of ice crystals
32
cumulus
dome-shaped, bunched cloud, with a flat base and billowy upper portions
33
stratus
cloud type characterized by low, flat sheets of clouds
34
nimbostratus
rain-producing low-level sheets of clouds
35
cumulonimbus
cloud that extends high into the atmosphere and is capable of strong vertical development and of producing severe weather
36
fog
cloud at or near ground level that reduces visibility to less than 1km
37
radiation fog
fog that results when the ground radiates its heat away at night, cooling the air above it to the dew point
38
advection fog
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
condensation nucleus
small particle in the atmosphere, about 0.2 Mm in diameter, on which water vapour condenses
40
collision and coalescence
process by which cloud droplets merge to form raindrops
41
ice-crystal process
the process by which ice crystals grow within a cloud to form snow
42
hail
hard, rounded pellets of ice that precipitate from cumulonimbus clouds with strong vertical airflow
43
negative feedback
process in which interacting parts in a system stabilize the system
44
positive feedback
process in which interacting parts in a system destabilize the system