in
French Polynesia in
Malaysia Many tropical areas have both a dry and a wet season. The
wet season, rainy season or green season is the time of year, ranging from one or more months when most of the average annual
rainfall in a region falls. Areas with wet seasons are disseminated across portions of the tropics and
subtropics, some even in
temperate regions. Under the
Köppen climate classification, for
tropical climates, a wet-season month is defined as one or more months where average precipitation is or more. Some areas with pronounced rainy seasons see a break in rainfall during mid-season when the
Intertropical Convergence Zone or
monsoon trough moves poleward of their location during the middle of the warm season; Typical vegetation in these areas ranges from moist
seasonal tropical forests to
savannahs.When the wet season occurs during the warm season, or
summer,
precipitation falls mainly during the late afternoon and early evening hours. The wet season is a time when
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 Köppen climate classification, much of the area within the geographical tropics is classed not as "tropical" but as "dry" (
arid or
semi-arid), including the
Sahara Desert, the
Atacama Desert and
Australian Outback. Also, there are
alpine tundra and snow-capped peaks, including
Mauna Kea,
Mount Kilimanjaro,
Puncak Jaya and the
Andes as far south as the northernmost parts of
Chile and
Peru.
Climate change The climate is changing in the tropics, as it is in the rest of the world. The effects of steadily rising concentrations of
greenhouse gases on the climate may be less obvious to tropical residents, however, because they are overlain by considerable natural variability. Much of this variability is driven by the
El Niño-Southern Oscillation (ENSO). The Tropics has warmed by 0.7–0.8 °C over the last century—only slightly less than the global average—but a strong
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 ==