Tropical climate

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Tropical climate refers to the climate typical of regions situated within the Earth's tropics, near the Equator. These regions experience warm weather throughout the year, with minimal temperature variation between seasons. The primary characteristic of a tropical climate is that temperature in these regions is consistently high, with the average monthly temperatures at or above 18°C (64°F) year-round.

Characteristics[edit | edit source]

Tropical climates are often divided into three main types: tropical rainforest (Af), tropical monsoon (Am), and tropical savanna (Aw or As). Each of these climates is distinguished by their unique precipitation patterns.

Tropical Rainforest Climate[edit | edit source]

The tropical rainforest climate, also known as an equatorial climate, experiences significant rainfall throughout the year, with no distinct dry season. This climate is found in areas close to the equator and is characterized by high humidity and dense rainforest vegetation.

Tropical Monsoon Climate[edit | edit source]

The tropical monsoon climate features a short dry season, but is predominantly wet. The monsoon rains are typically concentrated in the high-sun season, resulting in distinct wet and dry periods. This climate is influenced by the movement of the Intertropical Convergence Zone (ITCZ) and monsoon winds.

Tropical Savanna Climate[edit | edit source]

Tropical savanna climates have a pronounced dry season, with the majority of rainfall occurring during the summer months. These regions are characterized by a mix of grasslands and trees, and the dry season can be quite severe, leading to issues such as droughts and wildfires.

Distribution[edit | edit source]

Tropical climates are found in a belt around the equator, typically within 10 to 25 degrees latitude in both the northern and southern hemispheres. Major areas include the Amazon Basin in South America, the Congo Basin in Africa, and various regions in Southeast Asia, including Indonesia and the Philippines.

Biodiversity[edit | edit source]

Tropical climates support a wide range of biodiversity. The warm temperatures and high levels of precipitation create ideal conditions for the growth of lush vegetation and the survival of a diverse array of animal species. Tropical rainforests, in particular, are home to more than half of the world's plant and animal species.

Human Impact[edit | edit source]

Human activities, such as deforestation, agriculture, and urbanization, have significant impacts on tropical climates. Deforestation in the Amazon and other tropical regions contributes to climate change by reducing the Earth's capacity to absorb carbon dioxide. Urbanization leads to the creation of heat islands, further exacerbating the warmth of tropical climates.

Adaptation and Mitigation[edit | edit source]

Adapting to and mitigating the effects of climate change in tropical regions involves protecting and restoring ecosystems, implementing sustainable land management practices, and reducing greenhouse gas emissions. Efforts to preserve tropical forests and peatlands are crucial in combating climate change.

See Also[edit | edit source]

Template:Climate

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Contributors: Prab R. Tumpati, MD