IEB Grade 12 Geography: Climatology, Fluvial Geomorphology, and Economic Geography

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Comprehensive vocabulary flashcards covering South African climatology, fluvial geomorphology, and agricultural economic geography for Grade 12 IEB students.

Last updated 4:09 PM on 6/8/26
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40 Terms

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Isobars

Lines connecting places of equal atmospheric pressure on a synoptic chart, where the spacing indicates pressure gradient wind strength.

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High Pressure (Anticyclones)

Atmospheric systems where pressure increases toward the center (e.g., 1024 hPa1024\text{\text{ hPa}}), characterized by subsiding, diverging air masses and absolute atmospheric stability.

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Low Pressure (Cyclones)

Atmospheric systems where pressure decreases toward the center (e.g., 1000 hPa1000\text{\text{ hPa}}), characterized by ascending, converging air currents and highly unstable weather fronts.

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Wind Velocity Plotting (Full Feather)

A symbol on a wind vector shaft representing a speed of 10 knots10\text{\text{ knots}}.

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Wind Velocity Plotting (Pennant Triangle)

A symbol on a wind vector shaft designating a speed of 50 knots50\text{\text{ knots}}.

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Mid-Latitude Cyclones (MLCs)

Massive low-pressure wave systems (10003000 km1000\text{--}3000\text{\text{ km}} in scale) moving West to East, driven by prevailing Westerlies, typically delivering winter rainfall to the Western Cape.

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Tropical Cyclones (TCs)

Intense cyclonic systems (100500 km100\text{--}500\text{\text{ km}} scale) manifesting over warm tropical ocean corridors (>26.5oC> 26.5^\text{o}C) during late summer to autumn.

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The Eye

The absolute calm, cloudless core of a Tropical Cyclone consisting of subsiding air.

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Eye Wall

The symmetrical area surrounding the Eye of a Tropical Cyclone featuring massive convective cumulonimbus towers.

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Coastal Lows

Localized, shallow low-pressure cells that migrate along the coastline ahead of cold fronts, driving rapid wind shifts and marine fog.

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Moisture Front / Trough

A summer phenomenon where warm humid air from the South Indian High collides with cool dense air from the South Atlantic High over the interior plateau.

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Line Thunderstorms

Volatile, linear convective structures created along the Moisture Front zone.

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Intertropical Convergence Zone (ITCZ)

The planetary convergence belt where the North-East and South-East Trade Winds meet, shifting dynamically with the Earth's thermal equator.

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Berg Winds

Dominant winter winds created when the Kalahari High forces dry plateau air down the Great Escarpment, heating adiabatically at approximately 1oC1^\text{o}C per 100 meters100\text{\text{ meters}}.

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Anabatic Winds

Daytime local winds where solar radiation heats upper valley slopes, causing air to expand, become less dense, and flow up the slopes.

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Katabatic Winds

Nighttime local winds where terrestrial longwave radiation cools upper slopes, causing dense air to flow down into the valley floor under gravity.

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Thermal Belt

A stable temperature inversion midway up valley sides produced when cold katabatic currents displace warmer air upward.

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Frost Pockets

Cold pools of air on the valley floor that can drop below 0oC0^\text{o}C, affecting crop placement.

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Topographic Aspect

The orientation of a slope; in the Southern Hemisphere, north-facing slopes receive direct insolation and are warmer and drier than south-facing slopes.

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Catchment Area

The geographic basin bounded by a perimeter highland ridge (watershed) that sheds precipitation into a single master drainage system.

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Watershed (Interfluve)

A perimeter highland ridge that bounds a catchment area.

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Water Table

The baseline level below which a waterbody is saturated.

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Dendritic Drainage Pattern

A tree-like, branching configuration developing on horizontally uniform, homogeneous sedimentary or igneous rock structures.

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Trellis Drainage Pattern

A pattern where main channels run parallel and secondary tributaries strike at precise 90o90^\text{o} angles, dictated by alternating hard and soft rock layers.

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Rectangular Drainage Pattern

A pattern with sharp right-angle bends controlled by jointing frameworks or fault lines in highly fractured basement rock.

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Radial Drainage Pattern

A pattern where channels radiate outward and downward from a single elevated dome or volcanic peak.

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Strahler's Stream Ordering Method

A numerical classification where two channels of order nn merge to form a channel of order n+1n+1, while intersections with lower-order streams do not increment the value.

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Laminar Flow

A mechanical regime where water layers slide smoothly in parallel sheets, requiring perfectly smooth, straight artificial channels.

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Turbulent Flow

A chaotic mechanical regime producing swirling eddies and vertical vectors, dominant in natural streams with rough, boulder-strewn beds.

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Longitudinal Profile

The side-view cross-section of a river channel traced from its source to its marine base level.

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Outer Bank (Undercut Slope)

The part of a meander where centrifugal force drives maximum velocity and erosion, creating a steep river cliff.

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Inner Bank (Slip-off Slope)

The part of a meander where water velocity drops, triggering deposition of bedload to form a gentle point bar.

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Oxbow Lake

An isolated loop abandoned by a river when it cuts directly through a meander neck during high-discharge flood stages.

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Stream Capture (River Piracy)

When an energetic stream breaches its watershed boundary via headward erosion and intercepts the flow of an adjacent, less energetic stream.

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Misfit Stream

The lower remaining remnant of a captured stream that is severely under-fit for its large, pre-existing valley floor.

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Elbow of Capture

The sharp, high-angle physical bend marking the exact site of structural diversion during stream capture.

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Wind Gap

The newly exposed, abandoned gravel-filled dry valley segment downstream of the elbow of capture.

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River Rejuvenation

An increase in a graded river's vertical kinetic energy caused by a drop in regional base level or tectonic uplift, leading to downward cutting.

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Knickpoint

A waterfall marking the intersection of old and new graded curves within a rejuvenated river system.

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Food Security

When all individuals, at all times, have physical, social, and economic access to sufficient, safe, and nutritionally optimal food sources.