Moisture Flashcards

(46 cards)

1
Q

Air Mass

A
  • pool of air, same humidity and temperature

- 1000 km^2

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2
Q

How are air masses classified?

A

by temperature and humidity at source region

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3
Q

Atmospheric River

A
  • 400-600 km wide, 1000 km long
  • band of wind transporting moisture
  • 30-50% of annual precipitation
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4
Q

Sea Breeze

A
  • day
  • cool ocean breeze, high pressure
  • flows onto warm land (low pressure)
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5
Q

Land Breeze

A
  • night
  • cool land breeze in high pressure area
  • flows over to warm, low pressure ocean
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6
Q

Air humidity

A
  • amount of water vapour in the air
  • determines rate of condensation, cloud formation, and precipitation
  • depends on temperature
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7
Q

Vapour Pressure

A

-share of air pressure made up by water vapour molecules at given T

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8
Q

Saturation

A
  • evaporation rate = condensation rate

- air is in equilibrium with liquid

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9
Q

Saturated Vapour Pressure

A
  • saturated air’s state
  • depends directly on T
  • 10 degree increase doubles SVP
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10
Q

Warm Tropical air SVP

A
  • lots of water vapour, releases latent heat

- powers the tropical storms

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11
Q

Cold Polar SVP

A
  • transfers less moisture

- polar deserts created

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12
Q

Mixing Ratio

A

mass of water vapour per unit mass of dry air

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13
Q

specific humidity

A

mass of water vapour per unit mass of moist air

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14
Q

Max specific humidity means..

A

max water vapour per unit air mass

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15
Q

Relative humidity =

A

amount water vapour in air/max possible at given T *100

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16
Q

Dew Point

A

-temperature for air mass to become saturated

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17
Q

Condenstation Causes

A
  • addition of water vapour in the air

- cooling of air

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18
Q

Diabatic

A

physical exchange of heat

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19
Q

Adiabatic

A

no physical exchange of heat

20
Q

air stability

A

-temperature difference between inside air parcel and air surrounding parcel

21
Q

Atmospheric Stability

A

-tendency of an air parcel to remain in place / change positions

22
Q

Stable Atmosphere

A

-air resists upward displacement

23
Q

Unstable Atmosphere

A

-air continues to rise until it reaches it’s own temperature and humidity conditions

24
Q

Rising air causes

A

clouds and precipitation

25
Warm air, Cool Air stability
warm air is unstable | cool air is stable
26
Dry Adiabatic Lapse Rate, Wet Rate, and Environmental Rate
10 degree/km 6 degree/km 12 degree/km
27
Cloud Formation (simple steps)
- cooling -> air rises - cools to dew point - saturates - condensation occurs
28
Cloud (buildup)
buildup of moisture droplets and ice crystals
29
Cloud Condensation Nuclei
- 10^-4 mm | - comes from volcanoes, ocean, forest fires, dust, clay and silt, combustion products
30
Cloud drop size vs. Rain drop size
- cloud drop 0.001 mm - 0.2 mm | - rain drop 0.4 mm to 4 mm
31
Drop Growth : Collision
- droplet T> 0 degrees C | - fall, collide, and coalesce
32
Drop Growth: Ice Crystal Growth
- T <0 degrees C for ice and drops - water around drops, vapour pressure gradient towards ice - net flow, accretion
33
Clouds: Low
- stratus, cumulus - cool atmosphere allows low formation - condensation and precipitation
34
Cloud: Vertical
- cumulus and cumulonimbus - high moisture content - possible precipitation
35
Stratocumulus Cloud
- warm atmosphere limits condensation | - clear weather
36
Cloud: Upper
- cirrus - scarcity of moisture - limits condensation
37
Fog (General)
Cloud layer on the ground, when Tdew = Tair
38
Fog: Radiation
- radiational cooling | - calm clear nights
39
Fog: Advection
-warm air passes over cool surfaces
40
Fog:Steam
cool air passes over warm water
41
Fog: Orographic
air is forced over physical barrier
42
Fog: Frontal
lifting associated with fronts
43
Inversion (general)
-warm air over cold surface
44
Inversion: Radiation
-occurs when evening air is still and no clouds are available to trap heat
45
Inversion: Sea Breeze
-windward coasts by cold ocean currents
46
Inversion: Subsidence
Subsiding air undergoes adiabatic heating aloft, air in contact with surface stays cooler