chapter 4 water in the atmosphere Flashcards

(54 cards)

1
Q

radiation fog

A

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

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2
Q

advection fog

A

results from moist air moving over cold surface that lowers its temperature to the dew point.
what is seen in winnipeg

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3
Q

condensation nuclei

A

small particles, .2 micrometers in diameter that provide a surface on which water vapor can condense

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4
Q

collision and coalescence

A

the process by which cloud droplets merge to make rain drops

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5
Q

collision and coalescence occurs ar

A

-15 degrees C and warmer in clouds

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6
Q

ice crystal process

A

forms snow in clouds in which the temperature is 0 or below

snow can form through deposition or contact freezing

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7
Q

which process occurs in warm clouds and what is the temperature

A

collision and coalescence process

above 0 degrees C

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8
Q

which process occurs in cold clouds and what is the temperature

A

ice crystal process

below 0 degrees C

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9
Q

with the exception of ___ all types of precipitation are produced through the collision and coalescence process or the ice crystal process

A

hail

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10
Q

______ _____ of the atmosphere determines which form or precipitation occurs

A

temperature profile

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11
Q

hail

A

hard round pellets of ice 5 mm or more in diameter

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12
Q

hail forms in _____ clouds

A

cumulonimbus

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13
Q

graupel

A

small pieces of ice before turning into hailstones

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14
Q

evaporation

A

change in the state of water from a liquid to a gas

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15
Q

transpiration

A

plants change liquid water into water vapour by breathing it out the pores on their leaves during photosynthesis

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16
Q

condensation

A

change in the state of water from a gas to a liquid

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17
Q

sublimation

A

ice shifts directly to water vapour

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18
Q

deposition

A

water vapour forms directly into ice

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19
Q

precipitation

A

solid or liquid water that falls from clouds to the ground

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20
Q

clouds

A

suspended microscopic water droplets and ice crystals that are visible only when they are grouped together in very large numbers

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21
Q

hydrologic cycle

A

the circulation of water within the atmosphere, biosphere, lithosphere, and hydorsphere

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22
Q

evapotranspiration

A

the source of all water vapour in the atmosphere

23
Q

latent heat

A

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

24
Q

evaporation ____ the environment and condensation ____ the environment.

25
humidity
the water vapour content of the air
26
net condensation
occurs when condensation exceeds evaporation, resulting in saturation of the air
27
saturation
the point at which water vapour content is equal to water vapour capacity
28
net evaporation
occurs when evaporation exceeds condensation
29
vapour pressure
the portion of air pressure exerted exclusively by molecules of water vapour
30
specific humidity
water vapour content of the atmosphere, expressed in grams of water per kg of air
31
relative humidity
ratio of water vapour content to water vapour capacity, expressed as a percent
32
temperature and RH are ___ related.
inversely
33
dew point
temperature at which air becomes saturated
34
frost point
when the dew point is at or below freezing, deposition forms crystals of ice called frost
35
dew point depression
the difference between the air temperature and the dew point temperature
36
air parcel
a body of air with uniform humidity and temperature
37
adiabatic cooling vs adiabatic warming
cooling- cooling of an air parcel through expansion | warming- warming of an air parcel through compression
38
dry adiabatic rate
rateof temperature change in an unsaturated parcel of air, water vapour in it but you cannot feel it
39
environmental lapse rate
decrease in air temperature outside the air parcel as altitude increases
40
moist adiabatic rate
rate of cooling in a saturated air parcel
41
unstable vs stable atmosphere
unstable- air parcels that are warmer and less dense that the surrounding air and rise on their own stable- the interior of air parcels is cooler and denser than the surrounding air
42
rain shadow
the dry environment on the leeward side of a mountain range, caused by adiabatic warming
43
convective uplift
rising of an air parcel that is warmer and less dense than the surrounding air
44
orographic uplift
rising of air over mountains
45
frontal uplift
rising of warm air masses where they meet relatively cold air masses
46
convergent uplift
rising of air as a result of converging airflow
47
intertropical convergence zone
converging and rising air strengthens convective uplift and thunderstorms, convective and convergent uplift blend together into a single process
48
nimbostratus
rain producing low level sheets of clouds
49
cumulonimbus
cloud that extends high into the atmosphere and is capable of strong vertical development and severe weather
50
cirrus
high clouds with a feathery appearance that are composed of ice crystals
51
stratus
clouds that are low flat sheets
52
nimbostratus
rain producing sheets of clouds
53
cumulus
bunched clouds with a flat base and billowy upper portions that often rise high into the troposphere
54
cumulonimbus
heaped up rain and hail clouds capabe of strong vertical development that may produce severe weather