ATPL Fronts And Depressions Flashcards
Explain what is meant by air-mass modifications
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)
Explain what’s meant by air-mass modification by regions
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
Describe following factors associated with either ‘cold air advection’ or ‘warm air advection’ (stability)
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
Describe the following factors associated with either ‘cold air advection’ or ‘warm air
advection’ cloud types
- Cold advection = Cumuliform cloud
- Warm advection = Low level Stratiform cloud or fog
Describe the following factors associated with either ‘cold air advection’ or ‘warm air
advection’ likely precipitation
Cold advection = showers
Warm advection = drizzle
Describe the following factors associated with either ‘cold air advection’ or ‘warm air
advection’ - visibility reductions
Cold advection = visibility good except in showers
Warm advection = reduced visibility due to drizzle and fog
Describe the following factors associated with either ‘cold air advection’ or ‘warm air
advection’ - turbulence
Cold advection = moderate to severe turbulence
Warm advection = nil or light turbulence
Describe concepts of convergence and divergence
•(Low) Convergence = air flowing in and ascending at the surface
•(High) Divergence = air descending at the surface and diverging
Explain the vertical motions generated by convergence and divergence near the earth’s
surface and immediately beneath the tropopause
(Lows) Lower level convergence = upper level divergence
(Highs) Lower level divergence = upper level convergence
Explain the concept of vorticity and the different types
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
Explain the two components of relative velocity
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.
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
Greater the amount of moisture the greater the development of cloud/precipitation
Larger amounts of latent heat released increasing instability
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
Unstable = cumulus
Stable = layer type - stratiform
Describe the effect of the following on the intensity of fronts, and on the extent of cloud and precipitation:
Slope of frontal surface
Steep sloping = cumulus
Shallow sloping = stratiform
Describe the effect of the following on the intensity of fronts, and on the extent of cloud and precipitation
Speed of front
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