Climate Characteristics (Cambridge (CIE) IGCSE Geography)

Equatorial Climate Characteristics

World climate distribution

• Climates vary across the world

• The reasons for these climate types include:

  • Latitude

    • With distance from the equator temperatures and sunshine hours decrease as the solar radiation is more dispersed at the poles and it has to pass through a greater amount of atmosphere

  • Altitude

    •  Increases in altitude lead to decreases in temperature 

  • Continentality

    • Locations further inland heat up more quickly in the summer and cool more quickly in the winter

  • Ocean currents

    • Warm and cold currents circulate in the oceans either warming or cooling the adjacent land 

  • Aspect

    • In the northern hemisphere slopes facing south are warmer 

  • Prevailing winds

    • Winds coming from warmer areas bring warmer air, increasing temperatures

  • Pressure systems

    • Areas usually affected by low pressure such as the equator have rising air, condensation, and cloud formation leading to more precipitation

    • Areas affected by high pressure have dry conditions due to the sinking air

Equatorial climate distribution

Equatorial climate characteristics

Location

• Low latitudes

• Within the Tropics 23.5^° north and south of the equator

• Amazon in South America, New Guinea, South-east Asia, Zaire Basin

Annual precipitation

• Over 2000mm

Temperature range

• Low range of mean monthly temperatures - 26-28^°C

• Constant high temperatures 

• Diurnal range is about 7^oC

Seasons

• No seasons - hot and wet all year round

Humidity

• High, usually over 75-80%

Prevailing winds

• Winds blow into the equatorial region from high-pressure areas to the north and south. 

• The winds from the north blow from the north-east and the winds from the south blow from the south-east.

• The winds are known as the trade winds

Factors influencing the equatorial climate

• There are a range of factors that influence the climate including:

  • The midday sun is almost directly overhead all year meaning there is maximum insolation

  • Low pressure all year leads to rising air, condensation, cloud formation, and high precipitation levels

  • Dense vegetation cover leads to high levels of evaporation and transpiration 

  • The warm air stores large amounts of water vapour until the temperatures start to cool in the late afternoon which then leads to heavy, daily convectional rainfall

Hot Desert Climate Characteristics

Hot desert climate distribution

Hot desert climate characteristics

Location

• 15^° - 30^° north and south of the equator (tropical and sub-tropical)

• North Africa - Sahara, Southern Africa - Kalahari and Namib, Australia. Middle East

Annual precipitation

• Below 250mm

Temperature range

• Daytime temperatures can reach 50^°C but average around 25^°C

• Night-time temperatures below 0^°C

• The diurnal range is large up to 45^°C

• The annual range is around 15^°C

Seasons

• Summer and winter

Humidity

• Low often between 10-30%

Prevailing winds

• The winds are offshore blowing from the east across the land, so they do not collect any moisture

Factors influencing the hot desert climate

• High pressure all year means the air is descending and warming

  • Precipitation does not occur because the air is not rising

• Prevailing winds are often from over land masses which means they contain little moisture

• Some deserts are in a rain shadow so there is little rainfall

• Cold ocean currents on the west side of continents may reduce summer temperatures due to the cooling effect of the ocean

Influence of pressure systems

• Hot deserts form between 15^o- 30^o north and south of the equator as a result of the atmospheric pressure systems

  • Air rises at the equator and when it reaches the upper atmosphere it moves north and south

  • The air cools and starts to sink

  • This creates a zone of high pressure at about 30^o north and south of the equator

  • Due to the sinking air, warm air cannot rise, condense, and form clouds. This results in high aridity