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, whereas areas affected by high pressure have dry conditions due to the sinking air
Equatorial climate distribution
Distribution of the Equatorial Climate
Equatorial climate characteristics
Characteristics | Equatorial Climate |
Location |
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Annual Precipitation |
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Temperature Range |
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Seasons |
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Humidity |
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Prevailing winds |
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Climate graph for Iquitos, Peru
Factors influencing the equatorial climate
- There are a range of factors which influence the climate including:
- The midday sun is almost directly overhead all year meaning there is maximum insolation
- Low pressure all year which 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 late afternoon which then leads to heavy, daily convectional rainfall