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26-627: Meshchera is a plain of roughly triangular shape bounded by rivers Oka from the South, Moskva River from the Southwest, Klyazma from the North and Sudogda and Kolp /Kolpna (Колпь, Колпна) from the East. Elevation: 80–130 metres. Climate of Meshchera is humid continental with long, cold and snowy winters, and short, warm and rainy summers. Annual average temperature is +4.3 °C (39.7 °F). The coldest month

52-405: A t i o n   i n   m m 25 ) {\displaystyle (100-{\tfrac {mean\ annual\ precipitation\ in\ mm}{25}})} to 60 mm. Tropical wet and dry or savanna climate's P dry should be less than ( 100 − m e a n   a n n u a l   p r e c i p i t

78-405: A t i o n   i n   m m 25 ) {\displaystyle (100-{\tfrac {mean\ annual\ precipitation\ in\ mm}{25}})} . Tropical climates normally have only two seasons, a wet season and a dry season. Depending on the location of the region, the wet and dry seasons can have varying duration. Annual temperature changes in the tropics are small. Due to

104-504: A short dry season which almost always occurs in the winter. The tropical monsoon climate is often found within countries in the south and southeast Asia region between the latitude of 10 degrees north and the Tropic of Cancer. It can also be found in West Africa and South America. The annual temperature of regions under tropical monsoon climate is also stable. The tropical monsoon climate has

130-512: A valley, a plain is enclosed on two sides, but in other cases a plain may be delineated by a complete or partial ring of hills, by mountains, or by cliffs . Where a geological region contains more than one plain, they may be connected by a pass (sometimes termed a gap ). Coastal plains mostly rise from sea level until they run into elevated features such as mountains or plateaus. Plains can be formed from flowing lava ; from deposition of sediment by water, ice, or wind; or formed by erosion by

156-588: Is February with average temperature of −11.6 °C (11.1 °F). During severe winters, temperatures can go as low as −47 °C (−53 °F). Summers are warm, sometimes hot, with average July temperature of +19.8 °C (67.6 °F), and in extremely hot summers temperature can rise up to +40 °C (104 °F). It is covered by mixed forests, pine forests in sandy areas, with many wetlands and lakes . 55°10′58″N 40°20′00″E  /  55.18278°N 40.33333°E  / 55.18278; 40.33333 This Moscow Oblast location article

182-448: Is a stub . You can help Misplaced Pages by expanding it . This Ryazan Oblast location article is a stub . You can help Misplaced Pages by expanding it . This Vladimir Oblast location article is a stub . You can help Misplaced Pages by expanding it . Plain In geography , a plain , commonly known as flatland , is a flat expanse of land that generally does not change much in elevation , and

208-408: Is a flat expanse of land with a layer of grass that generally does not change much in elevation , and is primarily treeless. Plains occur as lowlands along valleys or at the base of mountains , as coastal plains , and as plateaus or uplands . Plains are one of the major landforms on earth, where they are present on all continents, and cover more than one-third of the world's land area. In

234-414: Is between 20 and 30 °C (68 and 86 °F). In summer, the temperature is between 25 °C and 30 °C, while in winter the temperature is between 20 °C and 30 °C, but still stays above an 18 °C mean. The annual precipitation is between 700 and 1000 mm. The driest months are generally in the winter and they have less than 60 mm of rainfall (often much less). Regions under

260-515: Is called the canopy tree layer which has trees from 25 to 40 meters tall and those trees grow closely while above is the emergent layer with sporadic trees taller than 35 meters. Tropical savanna climates , or tropical wet and dry climates, are mainly located between the 10° and 25° north-south latitudes, and often occur at the outer margins of the tropics. Typical regions include central Africa, parts of South America, as well as northern and eastern Australia. The temperature range of savanna climate

286-457: Is intense in these climates. There are three basic types of tropical climates within the tropical climate group: tropical rainforest climate ( Af ), tropical monsoon climate ( Am ) and tropical savanna or tropical wet and dry climate ( Aw for dry winters, and As for dry summers), which are classified and distinguished by the precipitation and the precipitation levels of the driest month in those regions. The Köppen climate classification

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312-399: Is one of the most widely used climate classification systems. It defines a tropical climate as a region where the mean temperature of the coldest month is greater than or equal to 18 °C (64 °F) and does not fit into the criteria for B-group climates, classifying them as an A-group (tropical climate group). A-group regions are usually found in the tropics , below 23.5 latitude in both

338-421: Is primarily treeless. Plains occur as lowlands along valleys or at the base of mountains , as coastal plains , and as plateaus or uplands . Plains are one of the major landforms on earth, being present on all continents and covering more than one-third of the world's land area. Plains in many areas are important for agriculture . There are various types of plains and biomes on them. A plain or flatland

364-506: The Earth. They are structurally depressed areas of the world that make up some of the most extensive natural lowlands on the Earth's surface. Tropical climate Tropical climate is the first of the five major climate groups in the Köppen climate classification identified with the letter A . Tropical climates are defined by a monthly average temperature of 18 °C (64 °F) or higher in

390-518: The Northern Zaire (Congo) basin of Africa, and the islands of the East Indies. The tropical rainforest climate differs from other subtypes of tropical climates as it has more kinds of trees due to its precipitation . The large number of trees contribute back to the humidity of the climate because of the transpiration, which is the process of water evaporated from the surface of living plants to

416-404: The agents from hills or mountains. Biomes on plains include grassland ( temperate or subtropical ), steppe ( semi-arid ), savannah ( tropical ) or tundra ( polar ). In a few instances, deserts and rainforests may also be considered plains. Plains in many areas are important for agriculture because where the soils were deposited as sediments they may be deep and fertile , and

442-498: The atmosphere. The warmth and abundant precipitation heavily contributes to the diversity and characteristics of vegetations under the tropical rainforest climate. The vegetations develop a vertical stratification and various growth forms to receive enough sunlight, which is unusual under other types of climate. The Köppen classification tool identifies tropical monsoon climate as having small annual temperature ranges, high temperatures, and plentiful precipitation. This climate also has

468-409: The cool dry season is from fall to late winter, the hot dry season is in the spring and the rainy or monsoon season is near or during the summer months. The tropical monsoon forest mainly consists of three layered structures. The first layer is the surface layer which is a very dense layer of shrubs and grasses. The second layer is the understory layer with trees about 15 meters tall. The top layer

494-408: The coolest month, featuring hot temperatures and high humidity all year-round. Annual precipitation is often abundant in tropical climates, and shows a seasonal rhythm but may have seasonal dryness to varying degrees. There are normally only two seasons in tropical climates, a wet (rainy/ monsoon ) season and a dry season. The annual temperature range in tropical climates is normally very small. Sunlight

520-419: The equator. Tropical rainforest climates have high temperatures: the yearly average temperature is normally between 21 and 30 °C (70 and 86 °F). The precipitation can reach over 100 inches a year. The seasons are evenly distributed throughout the year, and there is almost no drought period here. Regions that contain tropical rainforest climate mainly include the upper Amazon basin of South America,

546-595: The flatness facilitates mechanization of crop production; or because they support grasslands which provide good grazing for livestock . The types of depositional plains include: Erosional plains have been leveled by various agents of denudation such as running water, rivers, wind and glacier which wear out the rugged surface and smoothens them. Plain resulting from the action of these agents of denudation are called peneplains (almost plain) while plains formed from wind action are called pediplains . Structural plains are relatively undisturbed horizontal surfaces of

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572-420: The following main characteristic. The average annual temperature is around 27.05 °C (80.69 °F) and has an average annual temperature range of about 3.6 °C (38.5 °F). Distinction between wet and drought seasons, the tropical monsoon climate is different from other tropical climates because of its uneven precipitation throughout the year. There are three main seasons of tropical monsoon climate:

598-408: The high temperatures and abundant rainfall, much of the plant life grows throughout the year. High temperature and humidity is the most suitable environment for epiphytes to grow. In many tropical climates, vegetation grow in layers: shrubs under tall trees, bushes under shrubs and grasses under bushes. Tropical plants are rich in resources, including coffee, cocoa and oil palm. Listed below are

624-533: The southern and northern hemisphere; they include areas around the Equator, Central America, North-central portions of South America, central Africa, southern portions of Asia and parts of North Australia and the Pacific Ocean islands. In Group A, there are three types of this climate: the tropical rainforest climate (Af) , tropical monsoon climate (Am) and tropical wet and dry or savanna climate (Aw or As) . All of

650-410: The three climates are classified by their P dry (short for precipitation of the driest month). Tropical rainforest climate's P dry should be greater than or equal 60 mm (2.4 in). Tropical monsoon climate's P dry should be in the range from ( 100 − m e a n   a n n u a l   p r e c i p i t

676-669: The types of vegetation unique to each of the three climates that make up the tropical climate biome. Tropical rainforest vegetation including: Bengal bamboo , bougainvillea , curare , coconut tree , durian and banana . Tropical monsoon vegetation including: teak , deodar , rosewood , sandalwood and bamboo . Tropical wet and dry or savanna vegetation including: acacia senegal , elephant grass , jarrah tree , gum tree eucalyptus and whistling thorn . The Köppen classification identifies tropical rainforest climates (Zone Af: f = "feucht", German for moist) as usually having north and south latitudinal ranges of just 5-10 degrees from

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