Synoptic Classifications Flashcards
1
Q
Tropical disturbances in the easterlies
A
Easterly waves
Easterly lows
2
Q
Easterly waves
A
- warm humid air
- associated with ICTS
- disturbances in tropical easterly flow
- barotropic
- no slanting with height
- open waves and cold core closes lows
- warm cored high pressure / ridge in upper air
- lower level convergence
- upper leve divergence
- strong uplift
- wide spread rain to east of trough
- winds northerly component
- rain for few days
3
Q
Easterly lows
A
- surface convergence to east of low
- divergence higher than easterly wave
- very strong uplift
- heavy rains
- wind Northward component
- years with this type of system difference between dry/wet years
4
Q
Temperate disturbances in the westerlies
A
- westerly waves
- cut-off lows
- southerly meridional flow
- ridging anti cyclones
- west coast troughs
- cold fronts
- tropical cyclones
5
Q
Westerly waves
A
- baroclinic
- tilted westward with height
- closed circulation at surface may be present
- surface convergence to the rear of the trough
- conservation of absolute vorticity and effects
- upper air divergence occurs to the east and ahead of trough line
- ideal conditions for sustained gentle uplift
- cloud and precipitation occur in unstable air to the rear and surface trough
- produce heavy rains between October and April
6
Q
Cut-off lows
A
- more intense form of westerly wave
- cold-cored depression
- starts as trough and deepens into closed circulation
- unstable, baroclinic systems
- slope west with weight
- strong convergence and vertical motion
- comma clouds
- associated with floods
- peaks in march - may and September and November
7
Q
Southerly meridional flow
A
- strong zonal pressure gradient
- forms between high west and low east
- upper level westerly wave: divergence and vertical motion
- coastal rainfall
- sharp drop in temps
8
Q
Ridging anticyclones
A
- upper level westerly wave: widespread general rainfall over eastern SA
- strong pressure gradient: causes advection of moisture and allows for a lot of unstable air
- weakening inland pressure gradients, changing curvature, orographic forcing and upper level divergence combine
- general rains or thunderstorms
- ridging high produce extensive clouds over coastal areas (similar to westerly waves but a lot more extensive)
- sometimes high not deep enough to cross Drakensburg mountains (then you won’t have any upper level forcing and divergence)
- brings rainfall from October to may
9
Q
West coast troughs
A
- surface trough over the west coast combines with approaching westerly wave: widespread rainfall over western parts
- surface convergence combines with upper level divergence
10
Q
Cold fronts
A
- occurs together with westerly waves and cutoff lows
- should not be considered in isolation
- associated with cold invasion from the south
- distinct cloud bands
- distinct wind shift
- most frequent in winter with the northern movement of westerlies: because ICTZ moving northward due to summer being in the northern hem, we have a more frequent occurrence of the cold front system.
- ahead= divergence and subsidence
- convection to rear with max surface convergence
11
Q
Conditions required for the formation of tropical cyclones
A
- Water temps of at least 26.5C down to depth of at least 50m
- Rapid cooling with height
- High humidity especially in the lower to mid troposphere
- Low wind shear
- Distance from the equator
- A pre existing system of disturbed weather
12
Q
Composite of synoptic types
A
- interplay of different synoptic features that play together with one another and may cause a composite of synoptic features and inference.
13
Q
Fine weather and mildly disturbed conditions
A
- subtropical cyclones
- coastal lows
- berg winds
14
Q
Subtropical cyclones
A
- associated with anticyclone vorticity
- deep systems tilted towards northwest with height.
- divergence near the surface
- strong subsidence ( marked conditions in subtropical regions)
- max = June/July
- min = dec/Jan
- when prevailing = produce severe heat waves
15
Q
Coastal low
A
- cyclonic vorticity with eastward movement of plateau
- initiate on west coast and travel along the coast
- warm offshore air flow ahead
- cold onshore air flow behind
- shallow (850hPa / 1500 m)
- resemble cold fronts
- not a majority rain producing system, and can couple with wave in upper air to form depression and rainfall