Local Climate: Aspect, Inversions and Valley Winds
Understand why opposite slopes heat differently, how cold air collects on a valley floor, and how anabatic and katabatic winds develop.
Learn how Highs and Lows differ in pressure, vertical air movement and surface circulation, and why each brings the weather it does.
By the end, you can
distinguish a High from a Low and describe their air movement in the Southern Hemisphere.
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High and Low Pressure Cells
Two engines, opposite directions
Almost every weather question in Grade 12 comes back to one thing: is the air going down or up?
That single fact decides the cloud, the rain, the wind and the temperature. Get the vertical movement right and the rest follows without memorising anything. 🌤️
South Africa sits under the influence of three semi-permanent Highs — the South Atlantic, the South Indian and the Kalahari High — which is why so much of the country is dry for so much of the year.
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High and Low Pressure Cells
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Next on the Geography path · step 6 of 11
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Understand why opposite slopes heat differently, how cold air collects on a valley floor, and how anabatic and katabatic winds develop.
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The whole Geography path → All High School MicroQuests → Browse all 134 →
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High and Low Pressure Cells
R19 · 12 min · certificate