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Geography of Malaysia

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Climate

Located near the equator, Malaysia's climate is categorised as equatorial, being hot and humid throughout the year. The average rainfall is 250 centimetres (98 in) a year and the average temperature is 25.4 °C (77.7 °F). The climates of Peninsular Malaysia and the East Malaysia differ, as the climate on the peninsula is directly affected by wind from the mainland, as opposed to the more maritime weather of East Malaysia. Malaysia is exposed to the El Niño effect, which reduces rainfall in the dry season. Climate change is likely to have a significant effect on Malaysia, increasing sea levels and rainfall, increasing flooding risks and leading to large droughts.

Malaysia faces two monsoon winds seasons, the southwest monsoon from late May to September, and the northeast monsoon from October to March. The northeast monsoon brings in more rainfall compared to the southwest monsoon, originating in China and the North Pacific. The southwest monsoon originates from the deserts of Australia. March and October form transitions between the two monsoons.

Local climates are affected by the presence of mountain ranges throughout Malaysia, and climate can be divided into that of the highlands, the lowlands, and coastal regions. The coasts have a sunny climate, with temperatures ranging between 23 and 32 °C (73.4 and 89.6 °F), and rainfall ranging from 10 to 30 centimetres (4 to 12 in) a month. The lowlands have a similar temperature, but follow a more distinctive rainfall pattern and show very high humidity levels. The highlands are cooler and wetter, and display a greater temperature variation. A large amount of cloud cover is present over the highlands, which have humidity levels that do not fall below 75%.

The highest temperature was recorded at Chuping, Perlis on 9 April 1998 at 40.1 °C (104.2 °F). The lowest temperature ever recorded in Malaysia was on Mount Kinabalu at −5 °C (23 °F) on 7 April 2023. The highest rainfall recorded in a day was 608 mm (23.9 in) in Kota Bharu, Kelantan on 6 January 1967. The highest rainfall recorded in a year was 5,687 mm (223.9 in) at Sandakan, Sabah in 2006. Meanwhile, the lowest rainfall recorded in a year was 1,151 mm (45.3 in) at Tawau, Sabah in 1997. The wettest place in Malaysia is Kuching, Sarawak with an average rainfall of 4,159 mm (163.7 in) with 279 days of rain a year. The driest place in Malaysia is in Sitiawan, Perak with average rainfall of 1,787 mm (70.4 in) a year.

As Malaysia is close to the equator, snowfall is extremely rare in the country, and has only ever occurred on Mount Kinabalu in 1975, 1993, 2018, and 2022.

Climate change

Climate change is having a considerable impact in Malaysia. Increasing temperatures are likely to greatly increase the number of heatwaves occurring annually. Variations in precipitation may increase the frequency of droughts and floods in various local areas. Sea level rise may inundate some coastal areas. These impacts are expected to have numerous environmental and socioeconomic effects, exacerbating existing environmental issues and reinforcing inequality.

Malaysia itself contributes emissions given its significant use of coal and natural gas. However, the use of hydropower has expanded in the 21st century, and other potential energy sources such as solar power and biomass are being explored. The government anticipates the need to adapt in areas such as health and coastal defences, and has ratified the Paris Agreement.

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