World climatic patterns are classified as hot-wet equatorial climates, savanna climates, tropical monsoon climates, desert climates, steppe climates, Mediterranean climates, Warm Temperate Eastern Margin Climates, British type climates, taiga climates, Laurentian climates, and polar climates.
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Tropical Humid Climates
- Tropical humid climates exist between Tropic of Cancer and Tropic ofCapricorn.
- The sun being overhead throughout the year and the presence of Inter Tropical Convergence Zone (INTCZ) make the climate hot and humid.
- Annual range of temperature is very low and annual rainfall is high.
- The tropical group is divided into three types, namely
- Af – Tropical wet climate;
- Am – Tropical monsoon climate;
- Aw – Tropical wet and dry climate.
Tropical Wet Climate
- Also known as ‘The Hot, Wet Equatorial Climate’, ‘Equatorial Rainforest Climate’.
- The regions are generally referred as ‘Equatorial Rainforests’, ‘Equatorial Evergreen Forests’, ‘Tropical Moist Broadleaf Forest’, ‘Lowland Equatorial Evergreen Rainforest’.
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Distribution
- Mostly between 5° N and S of Equator. Its greatest extent is found in the lowlands of the Amazon, the Congo, Malaysia and the East Indies
- Equatorial Climate
- Dominated by Maritime Tropical air masses.
- Temperature
- Temperature is uniform throughout the year.
- The mean monthly temperatures are always around 27° C with very little variation.
- There is no winter
- Cloudiness and heavy precipitation moderate the daily temperature.
- Regular land and sea breezes assist in maintaining a truly equable climate.
- The diurnal range of temperature is small, and so is the annual range.
- Precipitation
- Precipitation is heavy and well distributed throughout the year.
- Annual average is always above 150 cm.
- In some regions the annual average may be as high as 250 – 300 cm.
- There is no month without rain (distinct dry season is absent).
- The monthly average is above 6 cm most of the times.
Equatorial Vegetation
- High temperature and abundant rainfall support a luxuriant tropical rain forest.
- In the Amazon lowlands, the forest is so dense that it is called ‘selvas’.
- Unlike the temperate regions, the growing season here is all the year round-seeding, flowering, fruiting and decaying do not take place in a seasonal pattern.
- The equatorial vegetation comprises a multitude of evergreen trees that yield tropical hardwood, e.g. mahogany, ebony, dyewoods etc.
- In the coastal areas and brackish swamps, mangrove forests thrive.
Canopy
- From the air, the tropical rain forest appears like a thick canopy of foliage, broken only where it is crossed by large rivers or cleared for cultivation.
- All plants struggle upwards (most ephiphytes) for sunlight resulting in a peculiar layer arrangement.
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Epiphyte
An epiphyte is a plant that grows harmlessly upon another plant (such as a tree) and derives its moisture and nutrients from the air, rain, and sometimes from debris accumulating around it.
- The tallest trees attain a height close to 50 m.
- The smaller trees beneath form the next layer.
- Because the trees cut out most of the sunlight the undergrowth is not dense.
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World Climatic Pattern,World Climatic Pattern
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