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Grade 12 Valley and Local Climates Summary - Geography

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This document is a complete set of Grade 12 Geography notes on Valley and Local Climates. It includes all key concepts, diagrams, explanations of temperature inversions, katabatic and anabatic winds, frost pockets, pollution traps, aspect influence, and real-world examples. Designed for quick understanding and strong exam performance.

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Valley climates

Micro climate - climate of a small area

Temperature difference in valleys

Slope aspect - angle at which the sun's rays strike a slope

Sun always vertically overhead earth between the tropics (23 ½ °N and 23 ½ °S)

Between 23 ½ °N and the North Pole + 23 ½ °S and the South Pole → sun's rays strike
earth's surface at angle less than 90°

In summer → angle is greater than it is in winter




The area of earth that a band of the sun's rays has to heat in summer (a) is smaller
than the area of earth that a band of the sun's rays has to heat in winter (b) ∴
earth's surface → hotter in summer

, ➔ Sun's rays strike land at a low angle to the horizontal
➔ Sun's rays coming from north side (direction of equator)
➔ North-facing slope receives most heat from sun
➔ South facing slope doesn’t receive sun → shadow zone

Shadow zone - an area, such as a slope, that doesn’t receive sunlight




Valley winds

Wind blows from high to low pressure

➢ Warm air = low pressure
➢ Cold air = high pressure

4 winds that blow in valleys:

➔ Upslope wind - local wind that blows up sides of valley during day

➔ Valley wind or anabatic wind - a local wind that blows up the length of the
valley during the day, from the bottom to top of mountain

➔ Downslope wind - local wind that blows down sides of valley during night

➔ Mountain wind or katabatic wind - local wind that blows down the sides of a
valley during the night, from top to bottom of mountain

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