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Climate Regions: Geography Factors and World Systems

Explore global climate regions, South Africa's climate factors, and weather elements like latitude, altitude, and ocean currents in this Grade 8 guide.

#geography#climate-regions#south-africa-climate#weather-elements#latitude#altitude#ocean-currents#education
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CLIMATE REGIONS

Grade 8 Geography • Term 2

Understanding our world's amazing climate systems 🌍

Social Sciences Learner's Book
Made byBobr AI

WHAT YOU WILL LEARN

This term we explore Climate Regions — broken into 3 units:

💡 Don't worry — we will explain everything step by step!

1
Unit 1: Factors That Influence Temperature & Rainfall
2
Unit 2: South Africa's Climate Regions
3
Unit 3: Climate Around the World
Latitude
Distance from Sea
Altitude
Ocean Currents
Mountains
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KEY VOCABULARY — WORD BANK

THERMOMETER

A tool used to measure temperature (how hot or cold the air is)

TEMPERATURE

How hot or cold a place is, measured in degrees Celsius (°C)

ANEMOMETER

An instrument that measures wind speed

HUMIDITY

The amount of water vapour (moisture) in the air

WIND

Air that is moving over the Earth's surface

PRECIPITATION

Any water that falls from the sky: rain, hail, snow, frost

WEATHER

The daily condition of the atmosphere (changes every day, observed over hours)

CLIMATE

The average weather of a place over many years (months or years)

CONDUCTION

How heat flows through a substance like air or water

ALTITUDE

The height of a place above sea level

WINDWARD

The side of a mountain where the wind blows FROM

TEMPERATURE RANGE

Difference between warmest and coldest monthly average temperatures

📚 Learn these words — they appear in every activity and test!

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🌦️ WEATHER

The day-to-day condition of the atmosphere at a specific place and time.

Changes every day
Observed over a small area
Short time period (hours or 24 hours)
📍
Example "Today in Johannesburg it is hot and sunny."

🌍 CLIMATE

The average weather conditions of a place over a long period of time (months or years).

Stays generally the same over years
Observed over a large area
Long time period (30+ years of data)
📍
Example "Johannesburg has hot wet summers and dry cold winters."
VS

🧠 EASY TRICK: Weather = What's happening TODAY. Climate = What USUALLY happens.

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UNIT 1

FACTORS THAT INFLUENCE TEMPERATURE & RAINFALL

There are 5 key factors that control how hot, cold, wet or dry a place is.

1. Latitude (Distance from the Equator)
2. Distance from the Sea
3. Altitude (Height Above Sea Level)
4. Ocean Currents
5. Mountains (Relief)
We will explore each factor one by one — with diagrams and examples!
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FACTOR 1

LATITUDE

Distance from the Equator

🌡️
Places NEAR the equator = HOT temperatures
❄️
Places FAR from the equator = COLD temperatures
☀️
At the equator, sun rays hit DIRECTLY → small area → INTENSE heat
🌐
At the poles, sun rays hit at an ANGLE → large area → less intense heat
📏
The further from equator → the cooler the temperature
🌍
🌍 Real World Example
Bangui (near equator) 26°C
East London (far from equator) 14°C
NORTH POLE
SOUTH POLE
EQUATOR
Tropic of Cancer
Tropic of Capricorn
HIGH TEMPERATURE
Direct rays, small area = Intense Heat
LOW TEMPERATURE
Angled rays, large area = Less Intense Heat
LOW TEMPERATURE
Angled rays, large area = Less Intense Heat
-17°C
27°C
-49°C
🧠 CLOSER to equator = HOTTER. Further away = COLDER.
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LATITUDE & RAINFALL — What happens to rain near the equator?

🌧️
Near the Equator (warm) → Rain falls as LIQUID RAIN
❄️
Near the Poles (cold) → Precipitation falls as SNOW
🌦️
Middle latitudes → Rain in summer, snow in winter
💧
The wettest places on Earth are within 25° of the equator

Average Annual Rainfall by Latitude

Bangui (4°N)
1,500mm
Luanda (9°S)
900mm
Khartoum (16°N)
160mm
Harare (18°S)
830mm
Rabat (34°N)
400mm
East London (32°S)
650mm
City Name
Latitude
Avg Temperature
Distance from Equator
Bangui
4° N
26.0°C (Hot)
(Closest)
Luanda
9° S
25.5°C (Warm)
Khartoum
16° N
29.9°C (Very Hot)
16°
Harare
18° S
18.5°C (High Altitude)
18°
East London
32° S
18.0°C (Mild)
32°
Rabat
34° N
17.5°C (Mild)
34° (Furthest)
🧠 Wetter = closer to equator. Drier = closer to poles.
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FACTOR 2:
DISTANCE FROM THE SEA

1
Land needs LESS heat to warm up than water (heats up twice as fast!)
2
Sun's rays penetrate DEEP into water but only heat the TOP of the land
3
Waves & currents keep mixing ocean water, keeping it COOLER
4
Some sun heat is used to EVAPORATE ocean water instead of heating it
📍 COASTAL PLACES
Cooler summers
+ Warmer winters
= MODERATE (small range)
🏜️ INLAND PLACES
Hotter summers
+ Colder winters
= EXTREME (big range)
ATLANTIC
OCEAN
INDIAN
OCEAN
P
PORT NOLLOTH
Jan (Summer): 16.0°
Jul (Winter): 12.7°
MODERATE (COAST)
D
DOUGLAS
Jan (Summer): 26.3°
Jul (Winter): 10.8°
EXTREME (INLAND)
K
KWADUKUZA
Jan (Summer): 23.7°
Jul (Winter): 17.8°
MODERATE (COAST)
SEA INFLUENCE REACHES COAST →
← SEA INFLUENCE REACHES COAST
🧠 COASTAL = mild temperatures.
INLAND = extreme temperatures (very hot summers, very cold winters)
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FACTOR 3: ALTITUDE

Height Above Sea Level

The HIGHER up you go, the COLDER it gets!

🌡️ Temperature drops 6.5°C for every 1,000 metres you go UP

Why does this happen?

  • The sun heats the Earth's SURFACE first
  • The warm ground then heats the air ABOVE it
  • Higher up = less air molecules = air stays COLD
City Altitude Mean Annual Temp
Durban 4m 20.4°C
Pietermaritzburg 658m 19.2°C
Bloemfontein 1,400m 16.1°C
Maseru 1,528m 15.1°C
Mokhotlong 2,178m 13.1°C
5,000m -2.5°C
4,000m 4.0°C
3,000m 10.5°C
2,000m 17.0°C
1,000m 23.5°C
Sea Level (0m) 30.0°C
Temperature Decreases
Altitude Increases

🧠Think of climbing a mountain — the higher you go, the colder it gets! Snow is only at the top.

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FACTOR 4: OCEAN CURRENTS

How moving ocean water affects our climate

WARM
Ocean Currents

  • Come from warm tropical regions near equator
  • Warm the air above them
  • Warm air holds MORE moisture → brings RAIN
  • Raises temperatures of nearby coastal areas

🌟 Example:
Agulhas Current → warms Durban's coast (20.4°C annual average)

City Profile Port Nolloth Durban
Ocean Current Cold Benguela Warm Agulhas
Average Temp 14.4°C 20.4°C
Annual Rain 60mm 1,009mm

→ DIFFERENCE = 6°C and 949mm of rain!

"Same latitude — TOTALLY different climates because of ocean currents!"

COLD
Ocean Currents

  • Come from cold polar regions
  • Cool the air above them → cool, dry air
  • Less moisture → LESS RAIN
  • Lowers temperatures of nearby coast
  • Can cause FOG along coast
  • Often cause DESERTS on west coasts

🌟 Example:
Benguela Current → makes Port Nolloth cold & dry (60mm rain/year)

🧠 WARM current = warm & rainy coast       |       COLD current = cold & dry coast.

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WORLD OCEAN CURRENTS — Warm & Cold

🔴 Warm Currents

Gulf Stream N. Atlantic
Agulhas Current S. Indian
Mozambique Current
Brazil Current
Kuroshio Pacific
Norwegian Current
Alaska Current
🔴 Warm current → warms coast, brings rain
🔵 Cold current → cools coast, brings dry conditions

🔵 Cold Currents

Benguela Current W. Africa
Peru Current W. S. America
Labrador Current
California Current
Oyashio Pacific
Canary Current
🌡️
Agulhas → Durban 20.4°C
❄️
Benguela → Port Nolloth 14.4°C
🌧️
Warm currents create more rainfall
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FACTOR 5: MOUNTAINS (RELIEF)

How mountains affect temperature

Mountains affect HOW MUCH sunlight different areas receive.
🏔️ North-facing slopes (Southern Hemisphere) → face the sun → WARMER
🌑 South-facing slopes → face away from sun → COOLER
☀️ Areas in direct sunlight for longer = higher temperatures
🌫️ Areas in shadow = much cooler temperatures
In South Africa, people prefer to build houses on NORTH-FACING slopes — they get more sun and are warmer!
Same mountain — different temperatures!
• South-facing slope: 13°C average
• North-facing slope: 23°C average
DIFFERENCE = 10°C!
A
WARM — 23°C
Direct rays
B
COOL — 13°C
Angled rays
C
COLD
Always in shadow
◀ NORTH
SOUTH ▶
🧠 In South Africa: NORTH-facing slope = WARMER (faces the sun). SOUTH-facing slope = COOLER (faces away from sun).
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HOW MOUNTAINS CREATE RELIEF RAIN & RAIN SHADOW AREAS

WINDWARD
SIDE

  • Where wind comes FROM
  • Moist air rises and cools
  • Heavy rainfall
  • Lush green vegetation
  • Example:
    George 770mm
Moist air blows
in from the sea
↗ FORCED TO RISE
↗ Air COOLS as it goes higher
LEVEL OF CONDENSATION
Water CONDENSES →
CLOUDS FORM → RAIN FALLS
↘ Air WARMS and DRIES out
WINDWARD SIDE
Gets LOTS of rain
770mm (e.g. George)
LEEWARD SIDE / RAIN SHADOW
Gets LITTLE rain
244mm (e.g. Oudtshoorn)
Cape Fold Mountains

RAIN SHADOW
(LEEWARD) SIDE

  • Sheltered from wind
  • Dry, warm air descends
  • Very little rainfall
  • Semi-arid/desert conditions
  • Example:
    Oudtshoorn 244mm

🧠 Windward side = WET (wind brings moisture up). Leeward/Rain shadow = DRY (wind has lost moisture going over mountain).

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HOW MOUNTAINS AFFECT WINDS — 3 Key Effects

1️⃣ FORCED ASCENT (Rising Wind)

When moist ocean wind hits a mountain, it is FORCED TO RISE. As it rises it COOLS and forms CLOUDS. RAIN falls on the WINDWARD side. Dry air descends on the LEEWARD side (rain shadow).

🌍 South African example:
Cape Mountains → George (wet) vs Oudtshoorn (dry)

2️⃣ FUNNELING (Channeling Wind)

❄️ Cold Polar Air from Arctic → funnelled south through centre of USA

Mountains on BOTH SIDES of a country can FUNNEL (channel) cold air into the middle. In the USA, the Rockies and Appalachians funnel icy Arctic air into central America, causing VERY COLD winters. New Orleans record low: -14°C!

3️⃣ BLOCKING (Shielding)

The HIMALAYAN mountains BLOCK icy Siberian winds from reaching India. This makes India MUCH WARMER in winter than other places at the same latitude!

City (Same Latitude) Jan Temp
Delhi (India — protected) 14°C
Shiraz (Iran) 6°C
Wuhan (China) 4°C

🧠 Mountains can: FORCE rain (ascent), CHANNEL cold winds (funneling), or BLOCK cold winds (blocking).

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5 FACTORS
That Influence
TEMPERATURE
& RAINFALL
1.LATITUDE
Near equator = HOT & WET
Near poles = COLD & DRY
(Sun's rays most direct at equator)
2.DISTANCE FROM SEA
Coastal = moderate temps
(mild summers & winters)
Inland = extreme temps
(very hot summers, very cold winters)
3.ALTITUDE
Higher up = COLDER
Drops by 6.5°C per 1,000m gained
(Air heats from the ground up)
4.OCEAN CURRENTS
Warm current = warmer coast + more rain
(e.g. Agulhas → Durban)
Cold current = cooler coast + less rain
(e.g. Benguela → Port Nolloth)
5.MOUNTAINS
Windward side = WET (relief rain)
Leeward side = DRY (rain shadow)
North-facing slopes = warmer
South-facing slopes = cooler
Exam Tip: Know all 5 factors, how they affect temperature AND rainfall, and a real South African example for each!
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UNIT 2

SOUTH AFRICA'S CLIMATE

South Africa has many different climate regions because of its unique geography.

Ranges in altitude from low coastal plains to high mountains and a plateau
Stretches over 12° of latitude (north to south)
Its centre is far from the ocean
Influenced by different wind systems
East coast = warm Agulhas current | West coast = cold Benguela current
over 1,000m
Coastal Plain
Port Nolloth
Cape Town
Johannesburg
Durban
We will look at how each of the 5 factors affects South Africa specifically!
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LATITUDE IN SOUTH AFRICA

South Africa covers about 10 degrees of latitude (from 22°S to 35°S). Places further south are generally cooler.

City Latitude Avg Summer Temp Avg Winter Temp
Polokwane 23°53'S 23°C 12°C
Bloemfontein 29°06'S 22°C 7°C
Port Elizabeth 33°59'S 20°C 14°C
Note: Polokwane is closest to equator → hottest summers. Port Elizabeth is furthest south → coolest summers.
BUT: Port Elizabeth has WARMER winters than Bloemfontein — why? → Distance from sea!

Avg Temperatures (°C)

Polokwane
Summer
23°C
Winter
12°C
Bloemfontein
Summer
22°C
Winter
7°C
Port Elizabeth
Summer
20°C
Winter
14°C

DISTANCE FROM THE SEA IN SOUTH AFRICA

📍

Upington

400km from Atlantic Ocean
Summer
28°C
Winter
12°C
Range
16°C
Rainfall
200mm/year

FAR from sea → EXTREME temperature range. HOT summers, COLD winters. Very DRY.

📍

Durban

Right on Indian Ocean coast
Summer
24°C
Winter
16°C
Range
8°C
Rainfall
1,008mm/year

NEAR the sea → MODERATE temperatures. Warm winters. Much WETTER.

🧠 Same country — VERY different climates! Location is everything.
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Altitude's Effect in South Africa

Johannesburg, Mbombela, and Maputo are at SIMILAR latitudes. BUT their altitudes are very different — causing very different temperatures!

City Johannesburg Mbombela Maputo
Altitude 1,740m 671m Sea level
Summer Temp 20°C 26°C 26°C
Winter Temp 10°C 16°C 20°C
Annual Rain 713mm 667mm 800mm
Frosts? 4 months/year Very rare Never

Johannesburg is 1,740m above sea level — that's why it's MUCH COLDER than coastal cities at the same latitude!

⚠️ Johannesburg gets FROSTS (ground freezes) in winter — altitude makes it colder!

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THE DRAKENSBERG MOUNTAIN EFFECT

Warm, moist air
from Indian Ocean
Forced to Rise
Ixopo 1,000mm rain
High areas 2,000m+
Dry Descending Air (West)
• Mthatha: 600mm
• Oudtshoorn: 150mm
The Drakensberg acts like a wall — trapping moist Indian Ocean air on the east, making the west much drier.
🧠

High altitude = colder + frost-risk. Mountains block rain = dry leeward side.

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THE 4 ELEMENTS OF WEATHER

Weather is made up of these 4 main elements

🌡️ TEMPERATURE

How HOT or COLD the atmosphere is — measured in degrees Celsius (°C)

  • Lowest temperatures: just after sunrise
  • Highest temperatures: 1-2 hours after midday
  • Summer = higher temps (Earth tilted toward sun)
  • Winter = lower temps
  • Instruments: THERMOMETER
Temperatures are shown on CLIMATE GRAPHS as a LINE

💧 HUMIDITY

The amount of WATER VAPOUR (moisture) held in the air

  • Hot air holds MORE moisture (higher humidity)
  • Cold air holds LESS moisture (lower humidity)
  • High humidity = feels damp/muggy
  • Low humidity = dry air
  • Near equator = very high humidity (tropical regions)
Ever noticed how on hot summer days it feels harder to breathe? That's HIGH HUMIDITY!

💨 WIND

Moving air caused by differences in AIR PRESSURE

  • Wind blows from HIGH pressure → LOW pressure areas
  • Wind direction = the direction it COMES FROM
  • Affects temperature and rainfall
  • Measured by: ANEMOMETER (speed) & WIND VANE (direction)
  • Beaufort Scale: Force 0 (calm) to Force 12 (hurricane)
Simple Beaufort: F0(Calm) | F3(Leaves move) | F6(Branches move) | F10(Trees down)

🌧️ PRECIPITATION

Any water that falls FROM the atmosphere to the ground

  • ☔ RAIN — most important, measured in mm using rain gauge
  • ❄️ SNOW — water vapour condenses below 0°C into ice crystals
  • 🌨️ HAIL — ice pellets formed in storm clouds (5-50mm dia.)
  • 🌫️ DEW/FROST — forms on the ground when air is cold
Deserts receive less than 250mm of rain per YEAR!
⭐ These 4 elements are what we measure to describe the WEATHER and CLIMATE of a place!
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THE BEAUFORT SCALE — Measuring Wind Without Instruments

You can estimate wind speed by OBSERVING what's happening around you!

FORCE
DESCRIPTION
OBSERVATION ON LAND
WIND SPEED
0
Calm
Smoke rises straight up
<1 km/h
1
Light air
Smoke drifts
1-5 km/h
2
Light breeze
Wind felt on face, leaves rustle
6-11 km/h
3
Gentle breeze
Leaves constantly moving, small flags extended
12-19 km/h
4
Moderate breeze
Loose papers blow, branches move
20-29 km/h
5
Fresh breeze
Small trees sway
30-39 km/h
6
Strong breeze
Large branches move, wires whistle
40-50 km/h
7
Near gale
Whole trees move, hard to walk
51-61 km/h
8
Gale
Twigs break, cars veer
62-74 km/h
9
Strong gale
Some roof damage
75-87 km/h
10
Storm
Trees blown over, building damage
88-101 km/h
11
Violent storm
Widespread damage
102-119 km/h
12
Hurricane
Most buildings damaged/destroyed
120+ km/h
🧠
Fun fact: Force 12 hurricane = winds faster than 120 km/h — strong enough to destroy buildings! Next time it's windy, try to estimate the Beaufort Force!
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HOW TO READ A CLIMATE GRAPH

Case Study: Bethlehem, Free State

1

Line graph details temperature (right axis)

2

Bar graph details rainfall (left axis)

3

12 months listed on the bottom axis

4

Highest bars = rainy season

5

Lowest temperature = coldest month

Bethlehem Summary

Rainy Season Oct – Mar
Dry Season May – Aug
Hottest Month January (19°C)
Coldest Month July (6.5°C)
120 100 80 60 40 20 0
30 25 20 15 10 5 0
Rainfall (mm)
Temperature (°C)
J
F
M
A
M
J
J
A
S
O
N
D
Hottest (19°C)
Coldest (6.5°C)
Rainy Season (Tall bars)
Dry Season (Minimal rain)
Climate graphs show AVERAGES — real weather can vary greatly!
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UNIT 3

CLIMATE AROUND THE WORLD

The world has 8 main climate types. Each one has different temperatures and rainfall patterns.

Tropical
Desert
Subtropical
Semi-desert
Temperate
Mediterranean
Continental
Polar

We will study each climate type — where it is, how hot/cold it gets, and how much rain it receives.

🌍 Remember: Latitude, altitude, distance from sea, ocean currents and mountains ALL influence which climate type a place has!

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WORLD CLIMATE TYPES — 1 & 2

1

🌴 TROPICAL CLIMATE

Location: 0° to 25° North and South of the Equator — within the tropics

🟢 WET TROPICAL (closer to equator)

  • High temps ALL year (25-30°C+)
  • Very high rainfall ALL year (2000mm+)
  • Only ONE season
  • Vegetation: TROPICAL RAINFOREST

🟡 DRY TROPICAL (closer to tropics)

  • Still hot all year
  • TWO seasons: Wet + Dry
  • Rain mostly in summer wet season
  • Vegetation: Savanna grasslands
WET TROPICAL GRAPH
Chart
" style="width: 100%; height: 130px; object-fit: contain;">
2

🌅 SUBTROPICAL CLIMATE

Location: 20° to 40° from equator, often on east coasts of continents

Key Features

  • Two seasons: warm summer + mild winter
  • Summer temps: above 20°C
  • Winter temps: around 15°C
  • Annual rainfall: ~1,200mm
  • Rain falls mostly in SUMMER

Examples

KwaZulu-Natal (RSA), Florida (USA), eastern China & Australia.

SUBTROPICAL GRAPH
Chart
" style="width: 100%; height: 130px; object-fit: contain;">
TROPICAL SUBTROPICAL
Location 0-25° from equator 20-40° from equator
Temperature Very hot all year Hot summers, mild winters
Rainfall Very high (2000mm+) High (1200mm), mostly summer
Vegetation Rainforest Mixed forest/grassland
🧠 KwaZulu-Natal has a SUBTROPICAL climate — that's why Durban is warm and humid with lots of summer rain!
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WORLD CLIMATE TYPES — 3 & 4
3

🌧️ TEMPERATE CLIMATE

Location: 40° to 65° North and South — typical of much of Northern Europe
  • MILD temperatures — not too hot, not too cold
  • Average annual temp: about 10°C
  • Total annual rainfall: about 1,400mm — quite rainy!
  • More rain in WINTER than summer
  • Four seasons (spring, summer, autumn, winter)
  • Cloudy, overcast skies common
  • Vegetation: Deciduous forests (trees lose leaves in autumn)
  • Examples: UK, France, Germany, New Zealand, parts of Chile
Climate summary: Cool summers (15-20°C), cold winters (2-8°C)
Precipitation
Temperature
Bars fairly even all year. slightly taller in winter. Temp gently curved (~15°C peak).
4

🏜️ DESERT CLIMATE

Definition: A desert is ANY area receiving less than 250mm of rain per YEAR

🔥 HOT DESERTS

  • Very hot days, cold nights, virtually no rain
  • Example: Sahara Desert (world's LARGEST hot desert)
  • Day temp: up to 50°C! Night temp: drops to 0°C
  • Extreme temperature RANGE between day and night!
  • Very little vegetation

❄️ COLD DESERTS

  • Cold and dry (still less than 250mm rain)
  • Example: Antarctica (world's LARGEST cold desert!)
  • Average winter temp: -40°C
  • Very little precipitation (it's simply just too cold)

Why so little rain?

  • Often caused by cold ocean currents (e.g. Benguela → Namib Desert)
  • Located in areas where air sinks and warms (doesn't rain)
  • Often on LEEWARD side of mountain ranges
MAX DAY MIN NIGHT
Extreme Swings
Almost no bars for rainfall. Huge swing represented between hot day temps & cold night temps.
🧠 Less than 250mm/year = DESERT! The Sahara is hot. Antarctica is cold. BOTH are deserts!
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WORLD CLIMATE TYPES 5 TO 8

5

SEMI-DESERT

  • 250-500mm rain/year with erratic rainfall
  • Droughts are a common occurrence
  • High day temperatures, cold nights
  • SA Example: The Karoo
6

CONTINENTAL

  • Only in the northern hemisphere (4 seasons)
  • Short, hot summers above 20°C
  • Long, freezing winters below 0°C for 3-4 months
  • Examples: Russia, Canada, Central USA
7

POLAR

  • Located near the North and South Poles
  • Warmest months rarely above 10°C
  • Almost 24hr darkness in winter, very little rainfall
  • Antarctica: winter average minus 40°C
8

MEDITERRANEAN

  • Around Mediterranean Sea and Cape Town
  • Warm, hot, dry summers & cool, wet winters
  • Popular wine and olive growing regions
  • SA Example: Cape Town

Key Insight:Cape Town has a winter rainfall Mediterranean climate while Johannesburg has a summer rainfall Subtropical climate.

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WHERE ARE THE WORLD'S CLIMATE REGIONS?

Each colour shows a different climate type

60°N
30°N
0° (Equator)
30°S
60°S

🌍 South Africa

Notice the mix of climate zones:
Subtropical (KZN)
Mediterranean (Cape Town)
Semi-desert (Karoo)
Desert (Namib edge)

Tropical
Subtropical
Desert
Semi-desert
Temperate
Mediterranean
Continental
Polar

💡 Notice how climate zones form roughly HORIZONTAL BANDS following lines of LATITUDE — because latitude controls how much sun a place receives!

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Climate Regions: Geography Factors and World Systems

Explore global climate regions, South Africa's climate factors, and weather elements like latitude, altitude, and ocean currents in this Grade 8 guide.

CLIMATE REGIONS

Grade 8 Geography • Term 2

Understanding our world's amazing climate systems 🌍

Social Sciences Learner's Book

CAPS 2026 Aligned

WHAT YOU WILL LEARN

This term we explore Climate Regions — broken into 3 units:

💡 Don't worry — we will explain everything step by step!

Unit 1: Factors That Influence Temperature & Rainfall

Unit 2: South Africa's Climate Regions

Unit 3: Climate Around the World

Latitude

Distance from Sea

Altitude

Ocean Currents

Mountains

KEY VOCABULARY — WORD BANK

📚 Learn these words — they appear in every activity and test!

THERMOMETER

A tool used to measure temperature (how hot or cold the air is)

TEMPERATURE

How hot or cold a place is, measured in degrees Celsius (°C)

ANEMOMETER

An instrument that measures wind speed

HUMIDITY

The amount of water vapour (moisture) in the air

WIND

Air that is moving over the Earth's surface

PRECIPITATION

Any water that falls from the sky: rain, hail, snow, frost

WEATHER

The daily condition of the atmosphere (changes every day, observed over hours)

CLIMATE

The average weather of a place over many years (months or years)

CONDUCTION

How heat flows through a substance like air or water

ALTITUDE

The height of a place above sea level

WINDWARD

The side of a mountain where the wind blows FROM

TEMPERATURE RANGE

Difference between warmest and coldest monthly average temperatures

🌦️ WEATHER

🌍 CLIMATE

The day-to-day condition of the atmosphere at a specific place and time.

The average weather conditions of a place over a long period of time (months or years).

Changes every day

Observed over a small area

Short time period (hours or 24 hours)

Stays generally the same over years

Observed over a large area

Long time period (30+ years of data)

Today in Johannesburg it is hot and sunny.

Johannesburg has hot wet summers and dry cold winters.

🧠 <strong style="color: #E07B39; font-weight: 800;">EASY TRICK:</strong> Weather = What's happening <span style="text-decoration: underline; font-weight: 700; color: #2D6A4F;">TODAY</span>. Climate = What <span style="text-decoration: underline; font-weight: 700; color: #2D6A4F;">USUALLY</span> happens.

UNIT 1

FACTORS THAT INFLUENCE TEMPERATURE & RAINFALL

There are 5 key factors that control how hot, cold, wet or dry a place is.

1. Latitude (Distance from the Equator)

2. Distance from the Sea

3. Altitude (Height Above Sea Level)

4. Ocean Currents

5. Mountains (Relief)

We will explore each factor one by one — with diagrams and examples!

LATITUDE

FACTOR 1

Distance from the Equator

Bangui

26°C

East London

14°C

LATITUDE & RAINFALL — What happens to rain near the equator?

Average Annual Rainfall by Latitude

Near the Equator (warm) → Rain falls as <b>LIQUID RAIN</b>

Near the Poles (cold) → Precipitation falls as <b>SNOW</b>

Middle latitudes → Rain in summer, snow in winter

The wettest places on Earth are within 25° of the equator

Wetter = closer to equator. Drier = closer to poles.

FACTOR 2:

DISTANCE FROM THE SEA

FACTOR 3: ALTITUDE

Height Above Sea Level

The HIGHER up you go, the COLDER it gets!

Temperature drops 6.5°C for every 1,000 metres you go UP

The sun heats the Earth's <strong>SURFACE</strong> first

The warm ground then heats the air <strong>ABOVE</strong> it

Higher up = less air molecules = air stays <strong>COLD</strong>

Think of climbing a mountain — the higher you go, the colder it gets! Snow is only at the top.

FACTOR 4: OCEAN CURRENTS

How moving ocean water affects our climate

WORLD OCEAN CURRENTS — Warm & Cold

🔴 Warm current → warms coast, brings rain

🔵 Cold current → cools coast, brings dry conditions

Agulhas → Durban 20.4°C

Benguela → Port Nolloth 14.4°C

Warm currents create more rainfall

FACTOR 5: MOUNTAINS (RELIEF)

How mountains affect temperature

Mountains affect HOW MUCH sunlight different areas receive.

North-facing slopes (Southern Hemisphere) → face the sun → WARMER

South-facing slopes → face away from sun → COOLER

Areas in direct sunlight for longer = higher temperatures

Areas in shadow = much cooler temperatures

In South Africa, people prefer to build houses on NORTH-FACING slopes — they get more sun and are warmer!

Same mountain — different temperatures!

South-facing slope: 13°C average

North-facing slope: 23°C average

DIFFERENCE = 10°C!

WARM — 23°C

Direct rays

COOL — 13°C

Angled rays

COLD

Always in shadow

◀ NORTH

SOUTH ▶

🧠 In South Africa: NORTH-facing slope = WARMER (faces the sun). SOUTH-facing slope = COOLER (faces away from sun).

HOW MOUNTAINS CREATE RELIEF RAIN & RAIN SHADOW AREAS

🧠 Windward side = WET (wind brings moisture up). Leeward/Rain shadow = DRY (wind has lost moisture going over mountain).

HOW MOUNTAINS AFFECT WINDS — 3 Key Effects

🧠 Mountains can: FORCE rain (ascent), CHANNEL cold winds (funneling), or BLOCK cold winds (blocking).

UNIT 2

SOUTH AFRICA'S CLIMATE

South Africa has many different climate regions because of its unique geography.

Ranges in altitude from low coastal plains to high mountains and a plateau

Stretches over 12° of latitude (north to south)

Its centre is far from the ocean

Influenced by different wind systems

East coast = warm Agulhas current | West coast = cold Benguela current

We will look at how each of the 5 factors affects South Africa specifically!

Port Nolloth

Cape Town

Johannesburg

Durban

LATITUDE IN SOUTH AFRICA

South Africa covers about 10 degrees of latitude (from 22°S to 35°S). Places further south are generally cooler.

Polokwane

23°53'S

23°C

12°C

Bloemfontein

29°06'S

22°C

7°C

Port Elizabeth

33°59'S

20°C

14°C

Polokwane is closest to equator → hottest summers. Port Elizabeth is furthest south → coolest summers.

Port Elizabeth has WARMER winters than Bloemfontein — why? → Distance from sea!

DISTANCE FROM THE SEA IN SOUTH AFRICA

Upington

400km from Atlantic Ocean

28°C

12°C

16°C

200mm/year

FAR from sea → EXTREME temperature range. HOT summers, COLD winters. Very DRY.

Durban

Right on Indian Ocean coast

24°C

16°C

8°C

1,008mm/year

NEAR the sea → MODERATE temperatures. Warm winters. Much WETTER.

🧠 Same country — VERY different climates! Location is everything.

Altitude's Effect in South Africa

Johannesburg, Mbombela, and Maputo are at SIMILAR latitudes. BUT their altitudes are very different — causing very different temperatures!

Johannesburg is 1,740m above sea level — that's why it's MUCH COLDER than coastal cities at the same latitude!

Johannesburg gets FROSTS (ground freezes) in winter — altitude makes it colder!

THE DRAKENSBERG MOUNTAIN EFFECT

The Drakensberg acts like a wall — trapping moist Indian Ocean air on the east, making the west much drier.

High altitude = colder + frost-risk. Mountains block rain = dry leeward side.

THE 4 ELEMENTS OF WEATHER

Weather is made up of these 4 main elements

⭐ These 4 elements are what we measure to describe the WEATHER and CLIMATE of a place!

🌡️ TEMPERATURE

How HOT or COLD the atmosphere is — measured in degrees Celsius (°C)

Lowest temperatures: just after sunrise

Highest temperatures: 1-2 hours after midday

Summer = higher temps (Earth tilted toward sun)

Winter = lower temps

Instruments: THERMOMETER

Temperatures are shown on CLIMATE GRAPHS as a LINE

💧 HUMIDITY

The amount of WATER VAPOUR (moisture) held in the air

Hot air holds MORE moisture (higher humidity)

Cold air holds LESS moisture (lower humidity)

High humidity = feels damp/muggy

Low humidity = dry air

Near equator = very high humidity (tropical regions)

Ever noticed how on hot summer days it feels harder to breathe? That's HIGH HUMIDITY!

💨 WIND

Moving air caused by differences in AIR PRESSURE

Wind blows from HIGH pressure → LOW pressure areas

Wind direction = the direction it COMES FROM

Affects temperature and rainfall

Measured by: ANEMOMETER (speed) & WIND VANE (direction)

Beaufort Scale: Force 0 (calm) to Force 12 (hurricane)

Simple Beaufort: F0(Calm) | F3(Leaves move) | F6(Branches move) | F10(Trees down)

🌧️ PRECIPITATION

Any water that falls FROM the atmosphere to the ground

☔ RAIN — most important, measured in mm using rain gauge

❄️ SNOW — water vapour condenses below 0°C into ice crystals

🌨️ HAIL — ice pellets formed in storm clouds (5-50mm dia.)

🌫️ DEW/FROST — forms on the ground when air is cold

Deserts receive less than 250mm of rain per YEAR!

THE BEAUFORT SCALE — Measuring Wind Without Instruments

You can estimate wind speed by OBSERVING what's happening around you!

<strong style="color: #E07B39;">Fun fact:</strong> Force 12 hurricane = winds faster than 120 km/h — strong enough to destroy buildings! Next time it's windy, try to estimate the Beaufort Force!

HOW TO READ A CLIMATE GRAPH

Case Study: Bethlehem, Free State

Climate graphs show AVERAGES — real weather can vary greatly!

UNIT 3

CLIMATE AROUND THE WORLD

The world has 8 main climate types. Each one has different temperatures and rainfall patterns.

We will study each climate type — where it is, how hot/cold it gets, and how much rain it receives.

🌍 Remember: Latitude, altitude, distance from sea, ocean currents and mountains ALL influence which climate type a place has!

WORLD CLIMATE TYPES — 1 & 2

🌴 TROPICAL CLIMATE

🌅 SUBTROPICAL CLIMATE

0° to 25° North and South of the Equator — within the tropics

20° to 40° from equator, often on east coasts of continents

TROPICAL

SUBTROPICAL

0-25° from equator

20-40° from equator

Very hot all year

Hot summers, mild winters

Very high (2000mm+)

High (1200mm), mostly summer

Rainforest

Mixed forest/grassland

🧠 KwaZulu-Natal has a SUBTROPICAL climate — that's why Durban is warm and humid with lots of summer rain!

WORLD CLIMATE TYPES — 3 & 4

🌧️ TEMPERATE CLIMATE

40° to 65° North and South — typical of much of Northern Europe

Cool summers (15-20°C), cold winters (2-8°C)

🏜️ DESERT CLIMATE

A desert is ANY area receiving less than 250mm of rain per YEAR

🔥 HOT DESERTS

❄️ COLD DESERTS

🧠 Less than 250mm/year = DESERT! The Sahara is hot. Antarctica is cold. BOTH are deserts!

WORLD CLIMATE TYPES 5 TO 8

SEMI-DESERT

250-500mm rain/year with erratic rainfall

Droughts are a common occurrence

High day temperatures, cold nights

<strong>SA Example:</strong> The Karoo

CONTINENTAL

Only in the northern hemisphere (4 seasons)

Short, hot summers above 20°C

Long, freezing winters below 0°C for 3-4 months

<strong>Examples:</strong> Russia, Canada, Central USA

POLAR

Located near the North and South Poles

Warmest months rarely above 10°C

Almost 24hr darkness in winter, very little rainfall

<strong>Antarctica:</strong> winter average minus 40°C

MEDITERRANEAN

Around Mediterranean Sea and Cape Town

Warm, hot, dry summers & cool, wet winters

Popular wine and olive growing regions

<strong>SA Example:</strong> Cape Town

Cape Town has a winter rainfall Mediterranean climate while Johannesburg has a summer rainfall Subtropical climate.

WHERE ARE THE WORLD'S CLIMATE REGIONS?

Each colour shows a different climate type