ATPL Fronts And Depressions Flashcards

1
Q

Explain what is meant by air-mass modifications

A

Continental = land air mass
Maritime = ocean air mass
Cold air moving to warm area = cold advection (unstable)
Warm air moving to cold area = warm advection (stable)

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2
Q

Explain what’s meant by air-mass modification by regions

A

Continental arctic - land air mass from arctic
Maritime polar - ocean air mass from arctic
Maritime tropical - ocean air mass from tropics
Maritime equatorial - ocean air mass from equator
Continental Antarctic - land air mass from Antarctic

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3
Q

Describe following factors associated with either ‘cold air advection’ or ‘warm air advection’ (stability)

A

K = Cold e.g PmK = Polar maritime cold
•W = Warm e.g TmW = Tropical maritime warm

•Cold air advection = cold air moving into warmer areas
•Warm air advection = warm air moving into cold areas

  • Cold air warms up as it moves to warmer areas increasing instability
  • warm air colds down as it moves to colder areas, increasing stability
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4
Q

Describe the following factors associated with either ‘cold air advection’ or ‘warm air
advection’ cloud types

A
  • Cold advection = Cumuliform cloud
  • Warm advection = Low level Stratiform cloud or fog
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5
Q

Describe the following factors associated with either ‘cold air advection’ or ‘warm air
advection’ likely precipitation

A

Cold advection = showers

Warm advection = drizzle

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6
Q

Describe the following factors associated with either ‘cold air advection’ or ‘warm air
advection’ - visibility reductions

A

Cold advection = visibility good except in showers

Warm advection = reduced visibility due to drizzle and fog

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7
Q

Describe the following factors associated with either ‘cold air advection’ or ‘warm air
advection’ - turbulence

A

Cold advection = moderate to severe turbulence

Warm advection = nil or light turbulence

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8
Q

Describe concepts of convergence and divergence

A

•(Low) Convergence = air flowing in and ascending at the surface

•(High) Divergence = air descending at the surface and diverging

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9
Q

Explain the vertical motions generated by convergence and divergence near the earth’s
surface and immediately beneath the tropopause

A

(Lows) Lower level convergence = upper level divergence

(Highs) Lower level divergence = upper level convergence

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10
Q

Explain the concept of vorticity and the different types

A

Means rotation/spin of airmass like a river with rotating eddies.

Relative vorticity = wind velocity pattern aloft. Caused by shear (horizontal difference in speeds) or curvature (forced changed in direction which imparts a spin). Can be anti/cyclonic

Earths velocity = generated by earths spin which is always cyclonic. Stronger than relative velocity.’

Absolute velocity = earths vorticity + relative, absolute is always cyclonic

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11
Q

Explain the two components of relative velocity

A

Curvature velocity - when a fluid(the air) is forced to change direction, a spin is imparted onto that fluid.

Shear velocity - vorticity generated in a straight-line flow if theres a wind speed differential in the horizontal plane. Generated most readily when a jet stream exists within the linear section of the flow between ridges and troughs.

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12
Q

Describe the effect of the following on the intensity of fronts, and on the extent of cloud and precipitation: amount of moisture in the warm rising air

A

Greater the amount of moisture the greater the development of cloud/precipitation

Larger amounts of latent heat released increasing instability

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13
Q

Describe the effect of the following on the intensity of fronts, and on the extent of cloud and precipitation:

Stability or instability of rising air

A

Unstable = cumulus

Stable = layer type - stratiform

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14
Q

Describe the effect of the following on the intensity of fronts, and on the extent of cloud and precipitation:

Slope of frontal surface

A

Steep sloping = cumulus

Shallow sloping = stratiform

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15
Q

Describe the effect of the following on the intensity of fronts, and on the extent of cloud and precipitation

Speed of front

A

Faster the front the narrower it’ll be but greater its intensity and activity

Cold fronts tract at 0.8x speed of wind 0.6 for warm

Slow front = stable stratiform
Fast = unstable cumulus

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16
Q

Describe the effect of the following on the intensity of fronts, and on the extent of cloud and precipitation

Temperature contrast across the front

A

Greater the contrast, the greater the intensity as more air will be able to rise on warm side.

17
Q

escribe the sequence of events during the passage of an idealised cold front and
warm front (or warm sector) in both hemispheres, in terms of pressure changes

A

Cold front Pressure:
Before - decrease
At - arrest or fall
After - increase

Warm front pressure
Before - decrease
At - arrest or fall
After - increase

18
Q

escribe the sequence of events during the passage of an idealised cold front and
warm front (or warm sector) in both hemispheres, in terms of

Temperature changes

A

Cold front -
Before - steady warm
At - abrupt decrease
After - steady cold

Warm front -
Before - steady/slight decrease
At - increase
After - little change

19
Q

escribe the sequence of events during the passage of an idealised cold front and
warm front (or warm sector) in both hemispheres, in terms of

Cloud

A

Cold front:
Before - Cs or As
At - Cu,Cb, No
After - clear, isolated Cu, Cb

Warm front:
Before - Ci, Cs, As, St, Ns, Sc, Cu, Cb
At - St, Ns, Cu,Cb
After - low-level cloud may persist

20
Q

escribe the sequence of events during the passage of an idealised cold front and
warm front (or warm sector) in both hemispheres, in terms of

Precipitation

A

Cold front:
Before - none
At - heavy showers/hail
After - isolated showers

Warm front:
Before - Light to persistently heavy
At - drizzle
After - occasional rain/drizzle

21
Q

escribe the sequence of events during the passage of an idealised cold front and
warm front (or warm sector) in both hemispheres, in terms of

Visibility

A

Cold front:
Before - fair
At - very poor
After - very good, reduced in showers

Warm front:
Before - good but becoming poor in rain
At - very poor
After - fair but poor in drizzle/rain

22
Q

escribe the sequence of events during the passage of an idealised cold front and
warm front (or warm sector) in both hemispheres, in terms of

Dew point changes

A

Cold front:
Before - no change
At - increase
After - lower then in advance of front

Warm front:
Before - slight increase
At - steady
After - higher than in advance of front

23
Q

Explain concept of occluded front

A

Cold front overtaking warm front
Depends on how cold air is Infront of warm front
Coldest air will be undercut everything else

24
Q

Explain how convergence drives an increase in vorticity through conservation of angular momentum

A

Angular momentum = airmass x RPM x Radius^2

where k is constant and air mass can’t change its size so RPM and radius can change due to absolute velocity.

RPM increase = radius reduce (convergence)
RPM decrease = radius increase (divergence)

25
Q

Outline the effect of vorticity advection on the development of mid-latitude
pressure systems

A

Vorticity advection = horizontal movement of spinning air aloft

•If spinning air aloft links up with spinning air at surface it will create either a high or a low depending on if its convergence or divergence

•Most highs and lows in mid latitudes created this way

26
Q

With respect to depressions of the Southern Hemisphere outside the tropics, describe the development and associated cloud

of the high mid - high latitude depression, where upper level divergence dominates the formation process

A

If upper-level divergence dominates the lows will have very strong upward vertical motion
•Extensive cloud band will form creating cold fronts and warm fronts with mostly unstable clouds

27
Q

With respect to depressions of the Southern Hemisphere outside the tropics, describe the development and associated cloud of the

sub-tropical depression, where advection of warm moist air and latent heat release dominate the formation process

A

Warm moist air moving towards the poles from tropics/subtropics
•Radius on which it rotates reduces towards the poles
•Creates low level convergence
•Will be enhanced further by release of latent heat
•Unstable cloud