Description of the variable rain forests of South America. Zone of variable humid subtropical forests

Monsoon forests are vast green areas with lush vegetation and rich wildlife. During the rainy season, they resemble equatorial evergreen forests. Found in subequatorial and tropical climate. They attract tourists and photographers with a variety of picturesque landscapes.

Description

Monsoon rainforests are most common in the tropics. Most often they are located at an altitude of 850 meters above sea level. They are also called deciduous due to the fact that the trees lose their leaves during periods of drought. Heavy rains return them to their former richness and color. The trees here reach a height of twenty meters, the leaves on the crowns are small. Evergreen species and many lianas and epiphytes are common in the undergrowth. Orchids grow in the monsoon zone. They are found in the Brazilian coastal mountain ranges, the Himalayas, Malaysia, Mexico, and Indochina.

Peculiarities

Monsoon forests in the Far East are famous for their diversity of plants and animals. Warm and humid summers and an abundance of plant food create favorable conditions for habitat of insects, birds, mammals. Conifers and broadleaf trees. Among the inhabitants of the forests, sable, squirrel, chipmunk, hazel grouse, as well as animals rare for climate zone Russia. Characteristic inhabitants of monsoon forests - Ussuri tiger, black bear, sika deer, wolf, raccoon dog. There are many wild boars, hares, moles, and pheasants on the territory. Reservoirs subequatorial climate are rich in fish. Some species are protected.

Rare orchids grow in the humid forests of Brazil, Mexico, and Indochina. About sixty percent are sympodial species, well known among gardeners. The red-yellow soils of monsoon areas are favorable for ficus, palm trees, and valuable tree species. The most famous ones include teak, satin, tallow, and iron. For example, it is capable of forming a dark grove from its trunks. In Indian botanical garden a huge banyan tree grows, which has almost two thousand (!) trunks. The crown of the tree covers an area of ​​twelve thousand square meters. Variable rain forests become a habitat for bamboo bears (pandas), salamanders, tigers, leopards, poisonous insects and snakes.

Climate

Which predominates monsoon forests? Winters here are mostly dry, summers are not hot, but warm. The dry period lasts three to four months. Average temperature air is lower than in humid tropics: absolute minimum -25 degrees, maximum - 35 with a "+" sign. The temperature difference ranges from eight to twelve degrees. Characteristic feature climate - long rainfalls in summer and their absence in winter. The difference between the two opposite seasons is huge.

Monsoon forests are known for their morning fog and low clouds. This is why the air is so saturated with moisture. By noon bright sun completely evaporates moisture from vegetation. In the afternoon, a foggy haze forms in the forests again. High air humidity and cloudiness persist for a long period of time. In winter, precipitation also falls, but rarely.

Geography

IN subequatorial belt due to loss large quantity precipitation and its uneven distribution, high temperature contrast, monsoon forests develop. On the territory of Russia, they grow in the Far East, have a complex topography, and a rich flora and fauna. There are humid forests in Indochina, Hindustan, the Philippine Islands, Asia, North and South America, and Africa. Despite the long rainy seasons and prolonged drought, the fauna in the monsoon forest areas poorer than in humid equatorial regions.

The most pronounced phenomenon of monsoons is on the Indian continent, where a period of drought is replaced by heavy downpours, the duration of which can be seven months. This change in weather is typical for Indochina, Burma, Indonesia, Africa, Madagascar, northern and eastern Australia, and Oceania. For example, in Indochina and the Hindustan Peninsula, the dry period in forests lasts seven months (from April to October). Trees with large crowns and arches grow in vast monsoon areas. irregular shape. Sometimes forests grow in tiers, which is especially noticeable from above.

Soil

Monsoon wet soils are characterized by a red tint, granular structure, and low humus content. The soil is rich in useful microelements such as iron and silicon. Sodium, potassium, magnesium, calcium in wet soil very little. On the territory Southeast Asia Zheltozems and red soils predominate. Central Africa and are distinguished by dry black soil. Interestingly, as the rains stop, the concentration of humus in monsoon forests increases. The reserve is one of the forms of protection wildlife in an area rich in valuable plants and animals. It is in humid forests that many species of orchids are found.

Plants and fauna

Monsoon forests in subequatorial climate Hindustan, China, Indochina, Australia, America, Africa, Far East(Russia) are characterized by a variety of fauna. For example, in Southeast Asia, teak trees are common in variable humid zones, as are Indochinese laurel and ebony. There are also bamboo, vines, butea, and cereals. Many trees in forests are highly valued for their healthy and durable wood. For example, teak bark is dense and resistant to destruction by termites and fungi. Sal forests grow at the southern foot of the Himalayas. IN monsoon areas Central America has many thorny bushes. Grows in humid climate and valuable jat wood.

In subequatorial climates, fast-growing trees are common. Palms, acacias, baobab, spurge, cecropium, entandrophragma, ferns predominate, and there are many other types of plants and flowers. The humid climate zone is characterized by a wide variety of birds and insects. Woodpeckers, parrots, toucans, and butterflies are found in the forests. Among the terrestrial animals found in monsoon forests are marsupials, elephants, different representatives cat family, freshwater, amphibians, frogs, snakes. This world is truly bright and rich.

The subequatorial climate zone is transitional and occurs in the northern and southern hemispheres, from to tropical zones.

Climate

In summer, in the zones of the subequatorial belt, the monsoon type of climate prevails, which is characterized by a large number precipitation. Its characteristic feature is the change air masses from equatorial to tropical depending on the season of the year. In winter, dry trade winds are observed here.

The average monthly temperature varies between 15-32º C, and the amount of precipitation is 250-2000 mm.

The rainy season is characterized by high rainfall (almost 95% of the year) and lasts about 2-3 months. When tropical easterly winds prevail, the climate becomes arid.

Countries of the subequatorial belt

The subequatorial climate zone passes through the countries of: South Asia (the Hindustan Peninsula: India, Bangladesh and the island of Sri Lanka); Southeast Asia (Indochina Peninsula: Myanmar, Laos, Thailand, Cambodia, Vietnam, Philippines); southern part North America: Costa Rica, Panama; South America: Ecuador, Brazil, Bolivia, Peru, Colombia, Venezuela, Guyana, Suriname, Guiana; Africa: Senegal, Mali, Guinea, Liberia, Sierra Leone, Ivory Coast, Ghana, Burkina Faso, Togo, Benin, Niger, Nigeria, Chad, Sudan, Central African Republic, Ethiopia, Somalia, Kenya, Uganda, Tanzania , Burundi, Tanzania, Mozambique, Malawi, Zimbabwe, Zambia, Angola, Congo, DRC, Gabon, as well as the island of Madagascar: Australia;

Natural zones of the subequatorial belt

Map of natural zones and climate zones of the world

The subequatorial climate zone includes the following natural zones:

  • savannas and woodlands (South America, Africa, Asia, Oceania);

And woodlands are predominantly found in the subequatorial climate zone.

Savannas are mixed grasslands. The trees here grow more regularly than in the forests. However, despite the high density of trees, there are open spaces covered with herbaceous vegetation. Savannas cover about 20% of the Earth's land area and are often in the transition zone between forests and deserts or grasslands.

  • altitudinal regions (South America, Africa, Asia);

This natural zone is located in mountainous areas and is characterized by climate change, namely a decrease in air temperature by 5-6 ° C as the altitude increases above sea level. In areas of altitudinal zonality, there is less oxygen and reduced atmospheric pressure, as well as increased ultraviolet radiation.

  • variable-humid (including monsoon) forests (South America, North America, Asia, Africa);

Variably humid forests, along with savannas and open forests, are mainly found in the subequatorial zone. The flora is not distinguished by a wide variety of species, unlike wet equatorial forests. Since this climate zone has two seasons (dry season and rainy season), the trees have adapted to these changes and are mostly broad-leaved deciduous species.

In the subequatorial zone, moist equatorial forests are not as widespread as in the equatorial zone. They are characterized complex structure forests, as well as a wide variety of flora, which is represented by evergreen tree species and other vegetation.

Soils of the subequatorial belt

This belt is dominated by red soils of variable rainforests and tall grass savannas. They are characterized by a reddish tint, granular structure, and low humus content (2-4%). This type of soil is rich in iron and has negligible silicon content. Potassium, sodium, calcium and magnesium are found here in negligible quantities.

Mountain yellow earth, red earth and lateritic soils are common in Southeast Asia. In South Asia and central Africa, black soils of dry tropical savannas are found.

Animals and plants

The subequatorial climate zone is home to fast-growing trees, including balsa trees and members of the cecropia genus, as well as trees that grow longer (more than 100 years), such as sweetenia and various types entandrophragm. Gabonese mahogany trees are common in humid tropical forests. Here you can find baobab, acacia, various types of palm trees, milkweed and parkia, as well as many other plants.

The subequatorial climate zone is characterized by a variety of fauna, especially birds (woodpeckers, toucans, parrots, etc.) and insects (ants, butterflies, termites). However, there are not many terrestrial species, these include.

Variably moist forests grow in those areas of the Earth where precipitation in the form of rain does not fall all year round, but the dry season does not last long. They are located in Africa north and south of the equatorial rain forests, as well as in northeastern Australia.

Look geographical location zones of variable humid forests on the map of natural zones.

The life of variable humid forests is closely related to seasonal climate changes: during the dry season, under conditions of moisture deficiency, plants are forced to shed their leaves, and during wet season dress again in foliage.

Climate. IN summer months temperature in areas variable-humid forests reaches 27 degrees Celsius, in winter months The thermometer rarely drops below 21 degrees. The rainy season comes after the hottest month. During the summer rainy season there are frequent thunderstorms, and there may be continuous cloud cover for several days in a row, often turning into rain. During the dry period, some areas may not receive rain for two to three months.

Variably humid forests are dominated by yellow earth and red earth forests. soil. The structure of the soil is granular-lumpy, the humus content gradually decreases downwards, on the surface - 2-4%.

Vegetation.

Among the plants of variable humid forests, evergreen, coniferous and deciduous trees are distinguished. Evergreens include palm trees, ficus, bamboo, all kinds of magnolia, cypress, camphor tree, tulip tree. Deciduous trees are represented by linden, ash, walnut, oak, and maple. Among the evergreens, fir and spruce are often found.

Animals.

The fauna of the variable humid forests is rich and varied. The lower tier is home to many rodents, large animals include elephants, tigers and leopards; monkeys, pandas, lemurs, and all kinds of felines find refuge among the tree branches. Meet Himalayan bears, raccoon dog and wild boar. The variety of birds is represented by pheasants, parrots, partridges and black grouse. Pelicans and herons live on the banks of rivers and lakes.

Man has destroyed a significant part of the variable rain forests. In place of cleared forests, rice, tea bushes, mulberries, tobacco, cotton, and citrus fruits are grown. It will take a long time to restore lost forest areas.

Variably wet forests. The zone of variable wet (including monsoon) forests extends in the east and south of Eurasia. The vegetation here is represented by conifers and deciduous trees(cedar, pine, oak, walnut, gingko) and evergreens (palms, ficus, bamboo and magnolias), which grow mainly on red-yellow soils. Animal world also characterized by significant species diversity: monkeys, tigers, leopards, as well as endemics - bamboo bear(panda), gibbon, etc.

Slide 11 from the presentation « Natural areas Eurasia". The size of the archive with the presentation is 643 KB.

Geography 7th grade

summary other presentations

“Natural zones of Eurasia” - Among the impenetrable thickets here you can find orangutans, leopards, and tapirs. Main animals: reindeer, arctic foxes, some species of birds. The latter predominates in the Asian taiga, in extremely cold conditions continental climate. Zone arctic deserts. Mixed and broad-leaved forests. The desert zone stretches across three geographical zones. The fauna here is represented by elephants, tigers, and rhinoceroses. Many reptiles and reptiles, as well as various insects. Along the mountain ranges of Siberia, tundra vegetation penetrates far to the south.

“Sights of Paris” - See Paris - and die! Arc de Triomphe in 1836 by Louis-Philippe. Place de la Star is officially called Place Charles de Gaulle. The Sorbonne was founded in 1253 by Robert de Sorbonne. Georges Pompidou - Beaubourg. The Pantheon is a monument containing the tombs of great people of France. The Eiffel Tower is the symbol of Paris. The Louvre is one of the largest and richest museums in the world fine arts. Goal: get to know the sights of Paris.

“Geographical position of the southern continents” - On plains composed of sedimentary rocks. Questions: To which oceans do the rivers of Africa and South America carry water? Why? Slide 7. Soil map. Igneous: ores of ferrous and non-ferrous metals, diamonds, noble and rare metals. General Features climate and inland waters. Slide 4. Minerals southern continents. In which climatic zones largest network rivers and many lakes?

"Geographical envelope of the Earth" - Modern look planet Earth. 1. Altitudinal zone zonation... 6. The lithosphere is... Students of class 7A Matrosova A.E. A. state of the troposphere B. long-term weather regime C. state of the troposphere at at the moment. A. on the plains B. in the mountains C. in the oceans 2. Geographical envelope– this is... Test work. Correct answers.

“Water in the World Ocean” - Without water, a person cannot live for more than eight days. Thanks to water and in water, life arose on Earth. Next, deadly dehydration occurs. You can't grow crops without water. We start studying water shell Earth - hydrosphere. Fundamental question: “Water! Group 2: Compare the area of ​​land and ocean. What is the temperature at different levels ocean?

“Savannahs” - Branched acacias rise like huge umbrellas among the tall grasses. Animal world. Savannah. Economic activity people. The average temperature in July and January is +22C. Soils. Geographical location. Climatic conditions. Umbrella acacia. Savannas are located in the subequatorial belt.

The tundra occupies such areas as the coastal outskirts of Greenland, the western and northern outskirts of Alaska, the coast of Hudson Bay, and some areas of the Newfoundland and Labrador peninsulas. In Labrador, due to the severity of the climate, the tundra reaches 55° N. sh., and in Newfoundland it drops even further south. The tundra is part of the circumpolar Arctic subregion of the Holarctic. The North American tundra is characterized by permafrost, highly acidic soils, and rocky soils. Its northernmost part is almost completely barren or covered only with mosses and lichens. Large areas are occupied by swamps. In the southern part of the tundra, a rich herbaceous cover of grasses and sedges appears. Some dwarf tree forms are characteristic, such as creeping heather, dwarf birch (Betula glandulosa), willow and alder.

Next comes the forest-tundra. It reaches its maximum size west of Hudson Bay. Woody forms of vegetation are already beginning to appear. This strip forms northern border forests in North America dominated by species such as larch (Larix laricina), black and white spruce (Picea mariana and Picea canadensis).

On the slopes of the Alaska mountains, lowland tundra, as well as on the Scandinavian Peninsula, gives way to mountain tundra and char vegetation.

In terms of species, the vegetation of the North American tundra is almost no different from the European-Asian tundra. There are only some floristic differences between them.

Coniferous forests temperate zone occupy most of North America. These forests form the second and last vegetation zone, which stretches across the entire continent from west to east and is latitudinal zone. Further to the south, latitudinal zonality is preserved only in the eastern part of the continent.

On the Pacific coast, taiga is distributed from 61 to 42° N. sh., then it passes through the lower slopes of the Cordillera and then spreads to the plain to the east. In this territory the southern border of the zone coniferous forests rises north to a latitude of 54-55° N, but then it descends back to the south to the territories of the Great Lakes and the St. Lawrence River, but only its lower reaches.<

Coniferous forests along the line from the eastern slopes of the Alaska mountains to the Labrador coast are distinguished by significant uniformity in the species composition of the species.

A distinctive feature of the coniferous forests of the Pacific coast from the forest zone of the east is their appearance and composition of species. So, the forest zone of the Pacific coast is very similar to the eastern regions of the Asian taiga, where endemic coniferous species and genera grow. But the eastern part of the continent is similar to the European taiga.

The “Hudson” eastern taiga is characterized by the predominance of fairly developed coniferous trees with a high and powerful crown. This composition of species includes such endemic species as white or Canadian spruce (Picea canadensis), Banks pine (Pinus banksiana), American larch, balsam fir (Abies balsamea). From the latter, a resinous substance is extracted, which finds its way into technology - Canada balsam. Although conifers predominate in this zone, there are still many deciduous trees and shrubs in the Canadian taiga. And in burnt areas, of which there are many in the Canadian taiga region, even deciduous trees predominate.

Deciduous tree species in this coniferous zone include: aspen (Populus tremuloides), balsam poplar (Populus balsamifera), paper birch (Betula papyrifera). This birch has white and smooth bark, which the Indians used to build their canoes. It is characterized by a very diverse and rich undergrowth of berry bushes: blueberries, raspberries, blackberries, black and red currants. This zone is characterized by podzolic soils. In the north they turn into soils of permafrost-taiga composition, and in the south they become soddy-podzolic soils.

The soil and vegetation cover of the Appalachian zone is very rich and diverse. Here, on the slopes of the Appalachians, rich broadleaf forests grow in species diversity. Such forests are also called Appalachian forests. These forests are very similar to the genera of East Asian and European forests, in which the dominant role is dominated by endemic species of noble chestnut (Castanea dentata), may beech (Fagus grandifolia), American oak (Quercus macrocarpa), red sycamore (Platanus occidentalis). A characteristic feature of all these trees is that they are very powerful and tall trees. These trees are often covered with ivy and wild grapes.