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General Atmospheric Circulation and Weather Systems
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General or average atmospheric flow
Polar High Cold polar air Sub-polar Low Sub-tropical High Warm tropical air Equatorial Trough Inter tropical convergence zone (ITCZ) Warm tropical air Sub-tropical High Sub-polar Low Cold polar air Polar High Document Reference: RTC-PRE Date of last revision: 21 August 2017
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High and low pressure cells
Document Reference: RTC-PRE Date of last revision: 21 August 2017
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High and low pressure cells Sub-tropical or mid latitude lows
Surface trough Tropical Cyclone Anticyclone Anticyclone Sub-tropical or mid latitude lows Document Reference: RTC-PRE Date of last revision: 21 August 2017
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Frontal systems - only in mid latitude cyclones
Document Reference: RTC-PRE Date of last revision: 21 August 2017
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Southerly onshore and inland flow
Document Reference: RTC-PRE Date of last revision: 21 August 2017 6
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Ridging high behind cold front
Document Reference: RTC-PRE Date of last revision: 21 August 2017 7
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Coastal Lows 1. Usually occurs in winter.
2. Dry, warm to hot winds from the land ahead of the low. 3. Cool winds from the sea behind the low. 4. Moves from the west coast and propagates along the SA coast to dissipate near Mozambique. 5. Usually indicates an approaching cold front. Document Reference: RTC-PRE Date of last revision: 21 August 2017
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Cut off low (COL) and Upper air trough
Document Reference: RTC-PRE Date of last revision: 21 August 2017
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Pressure systems and resulting winds
Wind is the movement of air caused by differences in surface temperatures and air pressure. The greater the difference, the faster the air moves (strong winds). Always blows from an area of a high pressure to an area of a low pressure. Document Reference: RTC-PRE Date of last revision: 21 August 2017
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Measurement Averaged quantities: for Forecasting: 10 min average
for Climatological statistics: 60 min average Highest gust: – the maximum observed wind speed over a specified time interval Wind has a direction and speed – Direction is from where the wind is coming (either geographic [NW, SSE etc] or degrees) – Speed is how fast/strong the wind is blowing – indicated in either m/s, knots or km/hr 0.5ms-1 = 1 kt = 1.85 km/hr Document Reference: RTC-PRE Date of last revision: 21 August 2017
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Wind direction Compass direction Exact equivalent in degrees Calm - N by E 11.25 NNE 22.5 NE by N 33.75 NE 45 NE by E 56.25 ENE 67.5 E by N 78.75 E 90 E by S 101.25 ESE 112.5 SE by E 123.75 SE 135 SE by S 146.25 SSE 157.5 S by E 168.75 S 180 Compass direction Exact Equivalent in degrees S by W 191.25 SSW 202.5 SW by S 213.75 SW 225 SW by W 236.25 WSW 247.5 W by S 258.75 W 270 W by N 281.25 WNW 292.5 NW by W 303.75 NW 315 NW by N 326.25 NNW 337.5 N by W 348.75 N 360 Variable Document Reference: RTC-PRE Date of last revision: 21 August 2017
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Subsiding air over the plateau
Local winds Berg Wind Formation Subsiding air over the plateau Surface winds flow down towards the sea Air descends and warms at DALR Escarpment Berg wind Subsidence Berg winds Winds blowing from the interior to the coast warm up and reach the coastal regions as hot, dry and windy. This can cause the highest temperature reached during winter along the coastal regions. Temperature increases by 1oC / 100m 18oC 28oC 23oC 1000m 100m 700m 400m 300m 200m 500m 900m 800m 600m 22oC 19oC 21oC 25oC 26oC 27oC 24oC Sea level Document Reference: RTC-PRE Date of last revision: 21 August 2017
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Local winds Anabatic winds Katabatic winds
During the day, these are upslope winds driven by the warmer surface temperatures on a mountain slope than the surrounding air column which causes the air to rise. Katabatic winds During the night, these are downslope winds driven by the colder surface temperatures on a mountain slope than the surrounding air column which causes the air to move down. Document Reference: RTC-PRE Date of last revision: 21 August 2017
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Local winds Sea and Land Breeze
During the day, the warms up faster than the sea. The wind then blows from the sea to the land as a sea breeze. At night, the land cools faster than the sea. The wind then blows from the land to the sea as a land breeze. Document Reference: RTC-PRE Date of last revision: 21 August 2017
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Winds in the vertical Altitude (Height) Wind – length represents speed
Ocean – lowest resistance Rural area – moderate resistance Urban area – highest resistance due to tall buildings Wind – length represents speed Altitude (Height) Document Reference: RTC-PRE Date of last revision: 21 August 2017
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The End
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