Tropics

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Tropical zone
)
World map with the intertropical zone highlighted in crimson
Areas of the world with tropical climates

The tropics are the regions of Earth surrounding the Equator. They are defined in latitude by the Tropic of Cancer in the Northern Hemisphere at 23°26′10.1″ (or 23.43613°) N and the Tropic of Capricorn in the Southern Hemisphere at 23°26′10.1″ (or 23.43613°) S. The tropics are also referred to as the tropical zone and the torrid zone (see geographical zone).

In terms of climate, the tropics receive sunlight that is more direct than the rest of Earth and are generally hotter and wetter as they aren't affected as much by the solar seasons. The word "tropical" sometimes refers to this sort of climate in the zone rather than to the geographical zone itself. The tropical zone includes deserts and snow-capped mountains, which are not tropical in the climatic sense. The tropics are distinguished from the other climatic and biomatic regions of Earth, which are the middle latitudes and the polar regions on either side of the equatorial zone.

The tropics constitute 39.8% of Earth's surface area

global warming, the weather conditions of the tropics are expanding with areas in the subtropics,[3] having more extreme weather events such as heatwaves and more intense storms.[4][3] These changes in weather conditions may make certain parts of the tropics uninhabitable.[5]

Etymology

The word "tropic" comes via Latin from Ancient Greek τροπή (tropē), meaning "to turn" or "change direction".[6]

Astronomical definition

Relationship of Earth's axial tilt (ε) to the tropical and polar circles: the Tropic of Cancer is a subsolar point only at the June solstice, and the Tropic of Capricorn is only at the December solstice[7]

The tropics are defined as the region between the Tropic of Cancer in the Northern Hemisphere at 23°26′10.1″ (or 23.43613°) N and the Tropic of Capricorn in the Southern Hemisphere at 23°26′10.1″ (or 23.43613°) S;[8] these latitudes correspond to the axial tilt of the Earth.

The Tropic of Cancer is the Northernmost latitude from which the

solar year. Thus the maximum latitudes of the tropics have equal distances from the equator on either side. Likewise, they approximate the angle of the Earth's axial tilt
. This angle is not perfectly fixed, mainly due to the influence of the moon, but the limits of the tropics are a geographic convention, and their variance from the true latitudes is very small.

Seasons and climate

Aerial view of Bora Bora, French Polynesia
Tropical sunset over the sea in Kota Kinabalu, Malaysia

Many tropical areas have both a dry and a wet season. The

air quality improves, freshwater quality improves and vegetation grows significantly due to the wet season supplementing flora, leading to crop yields late in the season. Floods and rains cause rivers to overflow their banks, and some animals to retreat to higher ground. Soil nutrients are washed away and erosion increases. The incidence of malaria
increases in areas where the rainy season coincides with high temperatures. Animals have adaptation and survival strategies for the wetter regime. The previous dry season leads to food shortages into the wet season, as the crops have yet to mature.

However, regions within the tropics may well not have a tropical climate. Under the

Perú
.

Climate change

The climate is changing in the tropics, as it is in the rest of the world.

El Niño
made 1998 the warmest year in most areas, with no significant warming since. Climate models predict a further 1-2°C warming by 2050 and 1-4°C by 2100.

Ecosystems

Coconut palms in the warm, tropical climate of northern Brazil

Amazon Rainforest territories of several South American countries, Madagascar dry deciduous forests, the Waterberg Biosphere of South Africa, and eastern Madagascar rainforests. Often the soils of tropical forests are low in nutrient content, making them quite vulnerable to slash-and-burn deforestation techniques, which are sometimes an element of shifting cultivation
agricultural systems.

In biogeography, the tropics are divided into Paleotropics (Africa, Asia and Australia) and Neotropics (Caribbean, Central America, and South America). Together, they are sometimes referred to as the Pantropic. The system of biogeographic realms differs somewhat; the Neotropical realm includes both the Neotropics and temperate South America, and the Paleotropics correspond to the Afrotropical, Indomalayan, Oceanian, and tropical Australasian realms.

Flora