Musson is a seasonal stream that is subdivided into warmer seasons of the air masses near the surface of the nearby troposphere. 
The wind direction changes from 120 to 180Âº . The main reason for Monson's appearance is the unevenness of the crocodile and the ocean.  Because of the formation of cyclone, anticyclone zones in the atmosphere, uneven warming and cooling of the continent and the sea, the pressure difference between them, the heat changes in the air twice a year. When the summer moist (oceanic) monsoon brings cool, wet air from the ocean, the winter (continental) monsoon transports cold, dry air to the ocean from the continent. Musons are divided into tropical and non-tropical. Tropical monsoon direction and high speed, strong impact; They are typical of South and South-East Asia, where the moisture is a few thousand mm rainfall. Tropic monsoon is typical of East Asia. The influence of the monsoon here is insignificant. The winter dry monsoon leads to the very cold climate of Siberia on the coast of the Pacific Ocean; The summer moist monsoon rains abundant rains on the ocean coast. Mousson plays an important role in the overall atmosphere of the atmosphere and has a significant impact on the economies of the monsoon climate. 
Mousson's cyclones and anticyclons are most stable and form in areas where the season is sharply different. Moussons are divided into two groups, both tropical and tropical (equatorial) monsoons.
Non-tropical monsoons are associated with an uneven warming of continents and oceans during the year. They are mostly visible in the northern hemisphere. The east coast of the continents is influenced by the musson circulation in the coastal and subtropical islands. Because of the influence of western winds in these areas, the difference between temperature and pressure between the continent and the oceanic crust is the reason for the appearance of seasonal hotspots (monsons). Summer mussels, which are opposite the direction of the western winds in the brown latitudes, cause rainfall on the continent and significantly reduce air temperature.
The most stable and clearly visible monsoons appear on the tropics. During the year, passages dominate the tropical latitudes of Pacific and Atlantic oceans. Therefore, tropical mussons are only visible in the western part of the Pacific Ocean and its adjacent East Asian and Indonesian coasts. Moussonian circulation involves large areas of the Indian Ocean Valley, which are located on tropical latitudes. This is due to the fact that the Indian Ocean is positioned between the two largest islands and in two hemispheres. The subtropic antikspantones and the equatorial low pressure array affect the tropical (equatorial) In July, an equatorial low pressure arc deployed to the higher hemisphere of the northern hemisphere, and in January, in contrast to the southern hemisphere. Subtropical antiklinos are also shifted in this direction. In the adjacent regions of the equator there is a change in the direction of the priority winds, due to the fact that the centers of the centers have a sharp displacement depending on the seasons. The tropic mussons are also caused by the uneven warming of the two half balls throughout the year
The winter, the monsoon passes in the eastern direction correspond to the direction of passers. During winter mousse, the air from the mainland to the ocean causes the dry period to correspond to that period. In the summer months when the direction of the passageway is opposite, the weather is oriented from the ocean to the mainland, so the rainy period basically corresponds to the summer season.
In general, about 70 tropical cyclones are formed annually on the planet on average. The duplication of tropical cyclones corresponds to the summer and autumn of the same hemisphere. In South Asia cyclones are observed in spring and autumn. The lines are stable. The east coast of the tropical belt is characterized by a great deal of climatic conditions. The temperature is much higher than in the west because of the sluggish flow along the coast, and there is plenty of rainfall. On the slopes there are 1500-2000 mm of precipitation per year
The background of the subtropical belt is very similar to the tropical belt, with the predominance of the antidillon. In contrast to the tropical belt, subtropics receive about 20% of solar radiation (from 2 1 00 to -102 - 25 up to 20 -102J / cm2), so the seasonal nature of the climate is noticeably greater. Cyclone actions are often repeated during winter. From the west to the east, climate differences are intensified. The western coast is characterized by a subtropic Mediterranean climate characterized by dry summers and winters. As the continent enters the continent, the climate is continental (find the major desert that is characteristic of such climatic conditions). On the west coast of the continents climate changes to the monsoon nature. The winter is relatively cold and dry, and the summers are hot and humid.
Winter is relatively cold and dry, but hot and humid in summer. The climate zone is particularly volatile in the northern hemisphere, so the radiation balance rises to 1200-102 J / cm 2 in the north to 2100102 J / cm2 in the south. The temperature varies from north to south and from west to east. Particularly winter temperatures are sharply lower in the interior of the continent due to the anticyclone regime. Under the influence of this, in Eurasia there is a cold pole of the left hemisphere (determine the location and temperature of the map).
The annual amount of precipitation is generally quite abundant in the belt, however. There are moisture in western continents, which is associated with the transfer of wet air masses in the oceans through the western winds. The East is deprived of moisture, it is continental, and the rainfall decreases dramatically. Depending on the ocean's influence on the east coast of the continent, precipitation increases. From the West to the East, the following features are clearly distinguished from the west: the moderate sea, the continental continental, the continental, the continental continental, the musson.
Subarctic and subanarctic bands are surrounded by the polar regions of the two hemispheres. Here, the annual radiation balance varies from 630-102 J / cm2 to 924-102 J / cm 2. Arctic and Antarctic air masses dominate in the summer, in the winter. Summer is relatively warm, but short, winter is very strict. Not too large in the amplitude of the year. The annual precipitation is less than 200 mm, usually heavily loaded.
Arctic and Antarctic strips are surrounded by two poles of the poles. In these strips the radiation balance is about 294-102 J / cm 2. 
â†‘ a b Encyclopedia of Kazakhstan, VI volume â†‘ Sectoral scientific explanatory dictionary of the Kazakh language terms. Water conservation. - Almaty, School, 2002.
â†‘ Geography: Overview of the World. CIS countries. Tutorial on the 10th grade of the Natural-Mathematical School of Secondary Education Beisenova, K. Kajmuldinova, S. Abylkimhinova and others. - Finished, complete. CHAPTER 2 - ĞĞ»Ğ¼Ğ°Ñ‚Ñ‹: ĞœĞµĞºÑ‚ĞµĞ¿, 2010. - 304 Ğ±., Ğ¡ÑƒÑ€.ISBN 978-601-293-170-9
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