Climate
Malaysia lies along the 1st parallel north to the 7th parallel north circles of latitude, roughly equal to Roraima (Brazil), the Democratic Republic of the Congo and Kenya. According to the Köppen climate classification system, Malaysia has a tropical rainforest climate due to its proximity to the equator. The country is hot and humid all year round, with an average temperature of 27 °C (80.6 °F) and almost no variability in the yearly temperature.
The country experiences two monsoon seasons, the Northeast Monsoon and the Southwest Monsoon. The Northeast Monsoon brings heavy rainfall to the east coast of Peninsular Malaysia and western Sarawak, while the Southwest Monsoon signifies dryer conditions throughout the country except Sabah. During the Southwest Monsoon, most states experience minimal rainfall due to the stable atmospheric conditions in the region and the Sumatran mountain range, which brings about the rain shadow effect. Sabah experiences more rainfall because of the tail effect of typhoons in the Philippines.
The urban heat island effect is caused by overdevelopment and general human activities in the cities of Malaysia.
Read more about this topic: Environment Of Malaysia
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