Airmasses and fronts Flashcards

1
Q

what happens to an airmass when it goes pass a warm, moist ocean

A
  • warm: heating the airmass, cause the lower layer to be unstable
  • moist: increase moisture in the airmass, esp. in the lower layer due to evaporation of the ocean surface
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2
Q

what happens to an airmass when it goes over an cold continent.

A
  • cold: no mixing of airmass, remains stable

- continent: airmass is dry. longer continental track: even drier

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3
Q

describe the tropical continental airmass(Tc) in summer, with respect to its temp., humidity, stability, weather and visibility

A

temp- very warm (from Sahara)
humidity- dry (continental track)
stability- generally unstable (warming of air)
weather- clear, thundery shower (warmth, sunshine)
visibility- moderate/poor (pollutant from continent)

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4
Q

describe the tropical continental airmass(Tc) in winter, with respect to its temp., humidity, stability, weather and visibility

A

temp- average (cooling of airmass)
humidity- rather moist (pick up some from the ocean)
stability- relatively stable (cooling)
weather- cloudy
visibility- moderate/poor (pollutant fr. cont.)

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5
Q

describe the tropical maritime airmass(Tm) in exposed area, with respect to its temp., humidity, stability, weather and visibility

A
temp- similar to sea temp.
humidity- very moist 
stability- rather stable (its journey is over cool water)
weather- low cloud, drizzly fog (coast)
visibility- poor (due to fog)
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6
Q

describe the tropical maritime airmass(Tm) in sheltered area (lee side of mountains), with respect to its temp., humidity, stability, weather and visibility

A

temp. - warm (clouds break releases latent heat)
humidity- moist
stability- stable aloft (latent heat warms the bottom)
weather- clear, clouds break; dry
visibility- moderate (dissipation of fog)

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7
Q

describe the Polar continental airmass(Pc) with long sea track, with respect to its temp., humidity, stability, weather and visibility

A

longer sea track - pick up properties from ocean
temp- cold (ocean warms up a bit)
humidity- moist in the low layer (due to ocean)
stability- unstable at the low layer
weather- rain, shower (moist)
visibility- good (ocean wash away pollutant)

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8
Q

describe the Polar continental airmass(Pc) with short sea track, with respect to its temp., humidity, stability, weather and visibility

A
temp- very cold
humidity- very dry
stability- stable 
weather- clear (cold air- no clouds)
visibility- moderate
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9
Q

describe the polar maritime airmass(Pm) in summer, with respect to its temp., humidity, stability, weather and visibility

A
temp- similar to the ocean temp, cool
humidity- very moist
stability- unstable (since its moist)
weather- showers
visibility- good
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10
Q

describe the polar maritime airmass(Pm) in winter, with respect to its temp., humidity, stability, weather and visibility

A
temp- even cooler
humidity- very moist
stability- unstable 
weather- showers, hail or thunders in hilly areas
visibility- good
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11
Q

describe the returning polar maritime airmass(rPm) all year long, with respect to its temp., humidity, stability, weather and visibility

A
temp- warm (warmer than Pm)
humidity- very moist
stability- unstable 
weather- with clouds, possible showers
visibility- good
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12
Q

describe the arctic maritime airmass(Am) in summer, with respect to its temp., humidity, stability, weather and visibility

A
temp- cold
humidity- rather moist
stability- unstable
weather- heavy showers/thunderstorm
visibility- good
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13
Q

describe the arctic maritime airmass(Am) in winter, with respect to its temp., humidity, stability, weather and visibility

A
temp- very cold
humidity- moist (less moisture than summer as cold air holds less water)
stability- unstable 
weather- heavy shower, hails, thunder
visibility- very good
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14
Q

general rules for different airmass

A

continental- weather is usually clear
maritime- weather is usually showery
if airmass contains some warmth- weather is cloudy
warmth hitting coast- weather is foggy

humidity: in winter, colder air, hold less water–> less moist than it is in summer

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15
Q

define front

A

the transition between 2 different airmasses

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16
Q

what types of clouds are associated with warm front?

A

thick stratus clouds mainly.

stratus, nimbostratus, altostratus, cirrostratus, cirrus

17
Q

a temperature inversion will be experienced during the passage of a warm front, what does this mean

A

temperature usually decreases with height, however with warm front, since air is warm, temperature increases with height, causing inversion

18
Q

what is the wind direction with the passage of warm front

A

veering. clockwise direction

19
Q

true or false:

the frontal surface of warm front is steeper than cold front

A

false

20
Q

true or false:

front moves slower than wind therefore u can feel rain before the passage of front

A

true. therefore you first feel the rain then the sudden change in temp

21
Q

if you see a halo, what does it indicate

A

warm front is approaching, bringing rain

22
Q

in a cold front, why does the underlying cold air curves at the ground.

A

due to friction. so the slope might be vertical near ground, or even slope the other way

23
Q

cold front travels _______ than warm front

A

faster

24
Q

why does the dew point decreases in the passage of a cold front

A

less water content can be held in cold air, hence dew point decreases (less water needed to reach saturation)

25
Q

what does pressure increase with the passage of cold front

A

cold air is denser, hence has a higher pressure.

26
Q

what types of clouds are associated with cold front

A

medium to high clouds

altocumulus, cumulonimbus, cirrostratus,cirrus

27
Q

what are ana fronts and kata fronts

A

ana- classical textbook fronts (less common in uk)

kata- weaker fronts (more common in uk) more low clouds associated

28
Q

what are the characteristics of clouds in warm and cold front

A

warm- thick clouds, formed behind the front

cold- thin elongated clouds, formed in advanced of front, mainly high clouds and medium clouds

29
Q

life cycle of a midlatitude cyclone

A
  1. disturbance in the stationary polar front in the mid latitude
  2. cold air from the pole pushes the cold front to the south and the tropical air pushes the warm from to the north, creating a low pressure in the middle
  3. cold air has a higher pressure while warm air has a lower pressure, this creates a pgf and this powers the development of the cyclone
  4. low-pressure is deepened, warm sector formed.
  5. occlusion is formed when cold air catches up with the warm front
  6. once occluded front is formed, power decays as there is no pgf.
  7. warm air has completely risen and cooled. temperature difference is quelled out occluded front then disappeared, leaving a low pressure system.
30
Q

cold occlusion

A
  • very cold air behind the cold front
  • common in summer as it is warmer inland
  • clouds and precipitation are behind the occlusion
31
Q

warm occlusion

A
  • cooler (warm) behind the cold front
  • common in winter as it is colder inland
  • clouds ad precipitation in advance of the passage of occlusion
32
Q

how is the weather after occlusion?

A
  • rainy, breezy with belt of clouds

- wind veers

33
Q

fronts are first clearly described by the ___________ in the early 1920s

A

Bergen School