adsby.ru → Russia

Yak are called the main masi. Atmospheric fronts - is it all right? Yakim stink

disastrous masi

disastrous masi- a great deal of trouble, there may be horizontal dimensions in a lot of hundreds or a few thousand kilometers and vertical dimensions in a few kilometers, which are characterized by an approximately uniform temperature and a horizontal path.

The uniformity of the powers of the given mass can be reached by the formations above the one-sided polystyle surface in the different minds of the thermal and radio balance.

In addition, it is necessary to have such a circulating mind, when the people were drunk, it would take a trivial hour to circulate in the region. The value of meteorological elements in the boundaries of the windmill varies insignificantly - the horizontal gradients are small. There is a rise in the growth of gradients of meteorological values, or at least a change in the size of the gradients in the transition zone between two masses - the zone of the atmospheric front.

Objects, which appear in the troposphere as a result of the intermode of withering masses - transition zones (frontal surfaces), frontal worm systems and dullness and fall, cyclonic damping, may be of the same order of magnitude, but sometimes mainland or oceans, hour of the day - more than 2 dib.

In the face of the formation of the wandering masses, let the region rise, by and by, descend, and then expand horizontally - the whole range of anti-cyclonic systems. Anticyclones are often, less cyclones, they are low-ruffled, therefore, the formation of masses of depressions is called and seen in the great low-ruff (quasi-stationary) anticyclones. In addition, the vimogam of the fire is perceived to be slightly destructible and growing in thermal depression, so that they appear over the heated sushi dishes. Nareshty, the formation of the polar twist, floats in small parts in the upper spheres of the atmosphere in little-ruffled, great and glib central cyclones in high latitudes. In cych baric systems, there is a transformation (reincarnation) of the tropic twist, drawn into the high latitudes in the upper spheres of the troposphere, into the twilight.

The masses are classified, the first for everything, in the middle of the formation in the fallowness of the growth in one of the latitudinal belts. It is a well-known geographic classification, the growing masi can be based on the main geographic types according to these latitudinal zones, in which they are spread out in the middle:

Arctic or Antarctic weather (AB),
Pomirniy povitrya (UV),
Tropicheskiye povitrya (TB).

Besides, it is possible to go to sea (m) and continental (k).

As a practice, I show the practice, I think about it, I mean the meridional length (in the SND, approximately from 45-48 ° to 60-65 ° in winter latitude), and the most important geographic areas To that, it is more correct to use a moderated VM on two independent ones - to a personal peace (SUV) and to a virtual peace (SUV).

Transformation of the masters

With the relocation of the powers that be, the masters will start changing their power - it’s not just from the powers of the government, but from the powers of the power of the past, but from the powers of the power of the strongest surface, often povitryanoi masi. The change in temperature can change as a result of the increase in the added warmth, or the heat exchange with the surface, which is built up.

The process of the wake of the power of the devout mass is called a transformation or a revolution. Transformation, tied with the ruff of the poets, is called dynamical. The speed of the change of the winding mass on the winter heights will be growing, the manifestation of the speed of the change of the wind is the turbulent change. As the lower balls get heated up, then the inconsistency and convective mixing develop. Call the process of transformation of the food mass in the form of 3 to 7 dB. I get to know the end of the day and the temperature of the temperature on a skin day like a close earthly surface, So i on the sides.

Thermodynamic Classification of Worshipers

Warm (cold) I call the masu, as it is warmer (colder) than the colder middle ground, and in this area it’s going to cool down (heat up), the pragmatists get close to the heat wave. pid navkolishnіm middle here the nature of the stylish surface, the thermal mill, as well as the suspicious masi, rises.

If it is necessary, it will cool down or warm up if the weather is in a given area, then for a few days it will take Tmax (the maximum daily surface temperature in the evening) or T850 (the temperature at the level of 850 hPa, close to 1.5 km.

Mistseviy (neutral) wandering masoyu call masu, how to be in the warmth of their middle class, so that day after day they take over their power without a few changes (Tmax dent ... ... In such a rank, the transformation of the mass can be both warm and cold, and upon completion of the transformation, it becomes a monstrous one.

On the AT-850 card, the cold weather is shown as the area is closed to cold (in the cold), warm - the crest or in the heat. Poor masa can be characterized as unstable, as well as unstable and equitable. One of the most important results in heat exchange is a vertical temperature rise and a more consistent view of a vertical heat exchange. With the strong (COM) and unstable (NVM) wandering masses, they tied the singing mind you wait. Neutral (miscellaneous) masses in any season can be as strong, as unstable in the fallowness of the cob authorities and in the direct transformation of this potent masses, for which the masters were approved.

Staykoy I will call the masu, in which the re-ferrying is vertically equal, so that in the main, the vertical temperature gradient is less than the humid-adiabatic one. Thermal convection in the UVM does not develop, and the dynamic is weakly developed. The mean value of the vertical temperature gradient in the UVM is less than 0.6 ° / 100 m. There are balls of inversion and isothermia (catch the balls). IN WHOM there can be a glimmer of turbulent exchange - sharuvat and sharuvat-cumulus. If the level of condensation lies in the upper boundary of a turbulent ball, then the weather is clear. Significant falloffs in the UVM are not spared, because of the sharuvate gloom, which have reached significant vertical pulling, drizzling falloff can occur in the row of falloffs, and a weak snowfall from the sharuvate-purchasers. In the case of a weak vertical exchange, in the UVM, try to avoid dimming, and in the row of fog and fog.

The heat wave of the mass over the continents is spared, as a rule, in the cold half of the rock, and comes to the Danish region in the warm sectors of cyclones and adjacent to them in the winter outskirts of anticyclones. In the vicinity of the drop, the vertical pressure of the sharuvate gloom grows on the floor, how the stench is transformed into the sharuvate-board and fix it to cover the fall. Vertical temperature rise is represented by balls of inversion and isotherm, or small temperature gradients up to a height of 3-4 km.

The cold stance of the mass spasters over the continents, in the main, is charged. The main type is frosty, cold weather, sometimes with radio fogs. Dodatkovy type - meaning і sutsіlnа sharuvat і sharuvato-kupchastі hmarnіst, inіnі weak sіgopadi.

An unstable (NVM) is called a poppy mass, in the main it is overgrowing a humid unstable stratification, which, with sufficient vologosti, can lead to the formation of convective gloom.

For NVM, there are typical buying and buying parts and planks of wood, and the collection - sharuvato-buys with some flat plate-and-planks. The ground airiness of the wind is in the unstable weather at the same and the same magnitude of the baric gradation is higher, lower in the stiffness. The weather is often buoyant, and when the bucket-boards are passed through, squalls are thrown for an hour. Naybіlsh yaskravo nonstіity is manifested in the illumination of rosy bourgeois-woody chimars, vypadannі zlivovy fallen, the development of thunderstorms. What is more, there is more strength in the food, more than the height of the reach of the upper border of the bush-board.

The warmth of the war over the continents is spared to flow, close to the Uzbek seas can be spared and charged. The warmth of the mass can be unstable in the warm sectors of cyclones and on the western periphery of anticyclones: The vertical temperature gradient in the significant sphere of the atmosphere is more humid and abatic.

Cold nasty people are spared to stay in the tilted parts of the cyclones behind the cold fronts and in the adjoining environs of anticyclones: they are spared to buy-to-buy, to buy-to-board gloom, to angry fall, often in bagatora, repeated. The good news of meteorological elements is great. The cold weather is especially characteristic of the overhang - "winter weather", since in the winter zone of the middle latitudes there is no more space, and in the new zone the soil is still warm.

Especially great inflow into the style of the potent mass of powers of the stylish surface. If the mass is warmer than the stylish surface, then it will cool down in the ground sphere. The Earth's temperature can be lower, lower by higher viskih pivnyakh... At any rate in the atmosphere, you can pretend to catch the shari. The mass becomes stiff, at least in the lower sphere of the atmosphere.

As soon as the mass is colder than the stylish surface, then in the ground sphere it warms up, increases the contrasts of the temperature between the lower balls of the atmosphere and the emergence of food and opens up with a friendly mind for development: convection

Div. also

posilannya

Wikimedia Foundation. 2010 rock.

Wonderful so also "Povitryani Masi" in the following dictionaries:

great encyclopedic vocabulary

Great illumination in the lower spheres of the troposphere, as it is possible to move beyond the horizontal dimensions to the parts of the continents and the oceans to change as one goal and volodyut by one-sided authorities. Turned out to be accompanied by atmospheric fronts and start in ... Morskiy Vocabulary

Great one-sided (horizontally straight) parts of the troposphere. Pod_lyayutsya atmospheric fronts. In the system of external circulation of the atmosphere, the weights are shifted as if they were the same, but in the meaning of the world the mode of the weather. Razr_znyayut ... ... encyclopedic vocabulary

Parts of the lower sphere of the troposphere atmosphere (Div. Troposphere), the horizontal space of some parts of the great parts of the continent and oceans. The skin is turned into a masa of the Volodya singing uniqueness of the authorities and to move as a whole in ... ...

Great one-sided (in the horizon. Directly) parts of the troposphere. Atm is added. fronts. In the system of the backward circulation of the atmosphere of the V. m. It is changing as a single whole, but in meaning. step mode wait. Razr_znyayut masi arktic. (Abo antarktich.) ... Natural science. encyclopedic vocabulary

The masses, which are formed over Antarctica and tied with it high-latitude parts of the oceans. Continental A. m Velyka Radianska Encyclopedia

Povitryani masi, scho to form over the Arctic (Div. Arctic). It is characterized by low temperatures, malim and great insight. With cyclones. dіyalnosti A. v. m. can move to greater low latitudes, wicked in them ... ... Velyka Radianska Encyclopedia

The masses, which are formed over Antarctica and tied with it high-latitude parts of the oceans. Continental Antarctic twists and turns are formed over the mainland itself, even though the lowest temperatures are close to the earth ... ... Vikipedia

Tsya side of vimag of ustotnoy processing. You can, її need to update, add or rewrite. Explanation of the reasons and discussion on the side Vіkіpedіya: Until polіpshennya / 13 April 2012 Date of staging until 13 February 2012 The date ...

Koli Geissler (1855) and Sprengel (1865) for vikachuvannya by now they froze mercury (div. Mercury pumps) and tsi put, all right (Teplera, Poggendorf, Joule, Mendelev, Spring, Devil. Encyclopedic Dictionary of F.A. Brockhaus і І.А. Efron

povitryana masa- the obsyag of the synoptic scale, that Volodya is approximately one-sided authorities. The horizontal dimensions of the rotary masses are stored in thousands of kilometers, and the vertical dimensions - the entire number of kilometers. Often times, they are used to quilting right up to the Tropopause. Masses are moving in the system of the atmosphere circulation.

Characteristics of the power supply: temperature, visibility, vision, filthiness, coldness, visibility, atmosphere.

Seed formulation of povitryanoy masi- physical-geographic region with a uniformly one-sided surface, scho pidstyla, the main power of the fortune-teller is being formed.

Transformation of the power- Changes in characteristics - to be seen when shifting the sleepy mass from the head of its form to the second floor, in the second physical-geographical region, in the middle of increasing the sleepiness.

geographic classification The fortune-tellers are based on the geographical position of the fortune-teller. The formation of weather minds on the territory of Russia is seen in the flow of arctic, world and tropical people, which can be continental and maritime.

Morska arktichna povitryana to form over the wilderness of the ice in the aquatorium of the Pivnichny Ice Ocean.

continental arctic- over the edge of the aquatorium of the Pivnichniy Ice Ocean.

Morska Pomirna povitryana - over the Atlantic Ocean in outside latitudes.

continental- over the continental regions of the surrounding latitudes.

morska tropical- over the aquatorium Atlantic Ocean in the tropical zone.

continental tropical- over the continental areas of the tropical zone.

thermodynamic classification The wind masses are based on the change in the temperature of the atmospheric wind along the horizontal and vertical lines. Falling as the temperature changes horizontally, you can see the cold, warm and cold weather.

Mistseva povitryana masa- a masa, yak, perebuva in the middle of his form, change of his power, heat up or cool down fallen out of time.

The heat of the disastrous masa- turned out to be a masa, scho to move to the cold underlying surface.

The masa is cold- to move to the warm surface

3. Stylish and unstable people.

Regularly, as the temperature changes vertically, the change in the temperature increases.

Steyka povitryana masa it is characterized by the fact that in the lower spheres (approximately lower than 1 km) there is a tendency of atmospheric stratification. With a stable stratification of the atmosphere, the vertical gradient of temperature is less than the adiabatic gradient. If it is filled with water vapor, then the adiabatic gradin is to the humid and abatic gradin. At the same time, the adiabatic gradient goes to the dry adiabatic gradient. Signs of a stylish povitryanoy mass - inversion, isothermia, fog, dimka and sharuvat hmarnist. The warmth of the masa, percolating on the cold surface and cooling from the bottom, becomes a stiff pooper.

Nestiyka povitryana masa it is characterized by the fact that in the lower spheres (approximately lower than 3 km), the atmosphere is not stratified. With a non-rigid stratification, the vertical gradient of temperature in the heating mass to the level of condensation is greater than the dry adiabatic gradient, while the level of condensation is greater than the humid and abatic gradient. In a non-stable mass with sufficient vologosti, the development of convection with the adoption of vertical development is observed, the turbulence is prevented, strong porous wind, angry, menace.

Cold poop masa, collapsing on the greater warmth of the stealthy surface and progrivayutsya from below, the old, as a rule, unstable povtryana masoyu.

1. VM stack: Levy - inversion, serpanok, fog. Hmari low, nasty visibility, the pre-cloudy ball is significant, the pre-cloudy ball and the dimness of the lower edge of the gloom are significant to speed up the landing and bad PS and good luck on small heights. nigirshi Wash the weather for people to be spared to go to the gloom in the sphere of the earth to the bottom of the border. Here the visibility is lost, maybe there is a small amount of money, and sometimes the fog gets angry with the gloom. In the chimneys and before them, in the event of hypothermia, there may be frostbite, especially if the upper cold weather, before inversion, or in the zone of hypothermia.

The flight over the chimars is spokyno, in the minds of a good visibility, a clear sky, or a small gloom of the upper or middle tier. If necessary, punch the gloom down, by the last sight of the upper edge, you can judge about the hanging of the lower border. If the upper boundary is small enough to wag the surface, then the lower boundary can sink to the ground or it is not very high. If the surface of the cordon has a humpbacked surface, with some protruding peaks, then the lower boundary lies at a height not lower than 200-300m from the ground. Hmari may have a slight vertical pulling, as when hovering over them on the gloomy surface, they spontaneously appear like a litter of rainbow dice. When the chill is broken, the KOM goes from bottom to top, the chilliness of chmariness grows to the top of the line. Close to the upper edge of the sun, a small bow can be repaired.

Vlіtku - the weather is not cold, the visibility is good, it can be set around the khmari kupchastі. 2. Nestiyka VM (vologa, heat) In NVM, visibility, as a rule, is good, so it is useful to supervise the bows of yak in chmaras, both in front of them and in front of them.

The on-demand purchases are not safe for use. The stench is strongly rosy up the hill and the stench of the mountains with chaotically piled up bilimous domes. The lower boundary should be extended at H = 600-1000m, the vertical force is to become 4-5 km. When used in chmaras, there is a strong bovine, at the upper part, de t = 0 * and lower, it can be prevented from freezing.

Naybilsha is not safe for the users to represent kupchasto-boards (thunderstorms) khmari. The polity easily grows along the peaks, but it can be seen as a giant mite (kovadlo), and it is built from feathery and bushy-planks. From the thunderous gloom in the earthly sphere, strong squalls of wind and evil are awakened. When you use the NVM at the middle heights, it is possible to create some high-quality burgundy and puffy chimneys, roztashovani at 2000-6000m. Їх singing in the rank of godini - a sign of a mighty menace in the daytime. When a thunderstorm is closer than an hour, when the peaks are more or less plastіvtsі.

Naybilsh friendly mind the use in NVM to prevent the growth of the tops of cumulus globes, or in the wide open spaces between them. Schob unicuti zustrіchі from bovtanki, discharges of blisks, kuchasto-boards khmari go around on visible from them not less than 10 km. It is possible to fly over the chimneys as needed, it is possible to work only during the day over the valley and the humped masses there, there are no less visible smogs in the fall, so that the hovering over the moss and under the chimneys of the bullet is not less than 200m.

Sposter for the serpents, wait a little more. The dawn changes like a board, boards - a dream, and above all, there is a sound of sound. The children of the wicked are buried and podiv, the older people have a sense of the mechanism of the process. Let's try to see how the weather is shaped and the atmospheric fronts are tied.

Cordon of the Masters

In a zvichny spryyatty "front" is the term vіyskovy. There is a line on which to see the closure of enemy forces. And the understanding of the atmospheric fronts is the center of the interlocking of the two wandering masses, which form over the majestic areas of the surface of the Earth.

By the will of nature, humanity denied the power of life, evolution and settlement of all great territories. The troposphere - the lower part - will keep us sour and stay in uninterrupted Russia. All won’t be built up from okremikh povіtryaniyu masses, about'єdnanih zagalnye vyniknennyy and similar indicators. Among the main indicators of the circulation are mass, temperature, pressure and volume. Pid hour to ruu різні masi You can get close and sticky. However, the smell of nikoli does not consume your cordons and does not shrink from yourself. - prices for small races, de-contacting and seeing fast races.

Trishki іstorії

The concept of "atmospheric front" and "frontal surface" is not by itself. Їх vev in meteorology of the Norwegian teachings J. Bjerknes. Became tse in 1918 rotsі. Bjerknes didv, scho atmospheric fronts - the main Lanka circulation of the atmosphere in the high and middle balls. However, until the early days of the Norwegian, back in 1863, Admir Fitzroy started up and baked atmospheric processes to fix it in the sky and go from the other sides to the light. Ale at that moment naukovoe spirituality not brutalizing respect for tsi sparing.

The Bergensky school, a representative of what is called Bierknes, didn’t just carry out the power of caution, but it didn’t just buy up all the knowledge and support, it was caught by the most early sponsors and educated people, and it’s announced the last time.

Behind the designation, I will abduct the surface, which is the area of transition between the rotational currents, called the frontal surface. And the axis of the atmospheric fronts is the image of the frontal surfaces on the meteorological map. Call the area of the atmospheric front to tie up at the surface of the Earth and go up the hill to quiet heights, on which the visibility changes between the wandering masses. Most of the time is from 9 to 12 km from the warehouse.

warm front

Atmospheric fronts are booming. The stench to lie down as a result of direct oversaturation of warm and cold masses. There are three types of fronts: cold, warm and occlusion, statements in the midst of winter fronts. The lectures are easy to understand and represent warm and cold atmospheric fronts.

Warm front - such a collapse of the withers, when it is colder, it turns into a warm wad. In order to increase the temperature, dry out, grow on the territory, de panuvali cold winters. Krym tsyogo, I must walk up the hill of the transition zone. At the same time, the temperature gradually decreases, through which condensation appears to be in a new water steam. So pretend to be.

The main signs, behind which you can see a warm atmospheric front:

rіsko padaє atmospheric grip;
growthє;
the temperature increases;
there are feathers, at the bottom of the pinnate-sharuvats, and the pislya - the visco-sharuvats of the hmari;
victoriously turned into power and become strong;
khmari flock with sharuvato-board;
vipadayut fall off the increase in intensity.

Silence the falling warm weather, a little bit cold front, the cold front collapses even more quickly and the warm atmospheric front.

cold front

Such a special feature is made possible: a warm front leads to heaving towards the ruin, and a cold one - to the opposing one. If the fronts collapse, it is colder to wedge into the warm, vishtovuyuchi uphill. Cold atmospheric fronts lead to lower temperatures and colder temperatures in significant areas. In the world of awakening, the warm addicts of the masvologist began to condense into coldness.

The main signs, behind which there may be a cold front:

in front of the front, the grip falls, behind the line of the atmospheric front, to move rapidly;
to pretend to be khmari;
z'yavlyayutsya porvchasty viter, with a sharp snake straight behind the year's arrow;
to repent of anger with a thunderstorm or hail, the triviality of the fall is close to two years;
temperature drops sharply, sometimes by 10 ° С at once;
behind the atmospheric front, there is a number of clarifications.

For mandrivniks, going through a cold front is not easy. In some cases it is brought to the end of whirlwinds and squalls in the minds of filthy visibility.

occlusion front

I have already said that the atmospheric fronts are growing, as the warm and cold bolsh-mensh everything zoosuly, then the front of the occlusion of the vicious masu nutrition. Formation of subtle effects is seen in the cold and warm fronts. It’s warmer when you get up the hill. The main activity is to be seen in cyclones at the moment, if the strong cold front is warmer. As a result, there is a collapse of atmospheric fronts and three winding masses, two cold and one warmth.

The main signs, behind which you can see the front of the occlusion:

hmari і fall off the storm type;
quick changes without a strong change in performance;
I will smoothly change the vice;
visibility of high temperature drops;
cyclone.

The front of the occlusion lies in front of it and behind the line. It grows cold and warm fronts of occlusion. Nayskladnіshі think about being spared at the moment without the front zmikannya fronіv. In the world of warm weather, the front is growing, the weather is growing.

Cyclone and anticyclone

Oskilki in the inventory of the front of the occlusion was implanted in the understanding of the "cyclone", then the need for development, well for the phenomenon.

As a result of an unsettled rise in the surface of the balls, a zone of high and low vice becomes established. The zone of a high vice is characterized by an overworldly bit of mischief, a low one - a lack of it. As a result of overflowing between zones (from excess to deficiency), a wind becomes established. A cyclone is a dilenk of a low vice, like a tightening, like a funnel, like a defect in food and coldness from zones, de smelly in excess.

Anticyclone - dilyanka z in a vice, Yakiy vitisnyaє excess of povitrya in the zone of low vice. The main characteristic is that the weather is clear, and there are some splinters of gloom from the central zone.

Geographical subdivisions of atmospheric fronts

Fallow climatic zones, Above which are formed atmospheric fronts, they are distributed along geographic knowledge on:

Arctic, which comes from the cold arctic winds up from around the world.
Polar, who grows up between the world and the tropical masses.
Tropic (pasatny), which is divided between tropical and equatorial zones.

Injection of a stylish surface

On the physical power of the minds, the mass is infused with radioactivity and the view of the Earth. Oskilny character of such a surface can be flashy, then rubbing about it is seen unevenly. foldable geografichesky relєf You can deform the line of the atmospheric front and change the effect. For example, there is a drop in atmospheric fronts when crossing the mountain ridges.

The windswept and atmospheric fronts bring forecasters innocent surprises. They stand and live straight ahead of the whims of cyclones (anticyclones), stink graphs and forecasts, like people who are often cursed, not preoccupied with time, how great is the price for the cyclones.

An analysis of the entire vicious show that the troposphere cannot be physically one-sided in all its parts.

False because of the fact that over what kind of dilenko earthly surface it was trivial to roar the masa, it was cold or warm, vology or dry, clouded or clouded by a glimpse. G іншого side, as a result of an uninterrupted collapse of the atmosphere in the horizontal and vertical strands of the power of the wanderers, can not be permanent. It is fair to respect that the troposphere, does not cease to be one and the same, is distributed in the middle of the world, and one of the same signs is seen, and the fact that the whole thing is connected with the collapse of the atmosphere.

The horizontal dimensions of the winding masses reach thousands of kilometers. Shake the masses to roztashovuyutsya either by order, or alone over the іnshoyu, can be time-consuming in peace, or most of the time it’s oversupplied. Skin masa cleverly vvazhaєtsya one-tier. It means that one should be promoted in the old parts, one kind of the same, changes in temperature, vologosti and so on. Steps and small steps. Then the transition from one of the poets to the beginning of the journey is quick; zones are called fronts, or frontal zones. visibility in physical power Worshiping the masses on the offense of the sides to the front beckon the great, and the wake of the powers that be seen quickly.

Obviously, the formulation of the masses, that is. earthly coo, Devoted masi are found pidlyagaє. It’s trivial to move in the same area, and to adjust the temperature, the level of health and the level of vision, geographic latitude and the nature of the stylish surface. Naybilsh friendly for singers characteristic signs Former masses of the region of persistent abo trivial anticyclones.

If in that vognischі, the deformity of the masa that underlies the surface is the sea, then it turns out to be called the sea; The land underlying the surface, ice or snow, is sometimes called continental.

If the masa is oversupplied, win your own geographic location, I also change the character of the stylish surface. Once a quick change of the primordial power has taken place, it is more likely to be transferred to other regions of the Earth with little change. With the general Russian, the masa has already risen along the way to change its signs literally. Having clawed at a new term in a new area, the fortune-tellers reborn here again and appear with a new combination of specialties; the triviality of such transformation - from 3 to 9 dB.

When Russia is fiercely warm, the strength of the stratification (as it progresses from below) changes to a greater warmth on the surface, and when it is more cold, it changes. If you do not see the condensation of water betting along the way, then the rest of the day in the morning after the hour of the hour of the fortune-teller mass will take for a drive in the road from the stylish surface of all the new portals of the vology. In Russia from winter to weekday (in winter season), the pressure of the old people grows smaller, so that the growth of the meridians in the “channel” has to grow wider. Girski ridges, which stand on the back, the wanderers want to bypass, altogether and load through them.

In Danish hour, it was accepted that the Masi followed the month of formulation. The geographic classification є immediately and genetically, the fragments of the power of the fortunate mass in the meantime are formed by the whole geographic situation of the city. Razr_znyayut such basic types of children by weight.

1. Arctic and Antarctic Powers to form over the snows and ice of the polar lands (the main rank before the hour of the polar night) from the inflow in the upper balls of the atmosphere of the polar and tropical (div. lower). With a lot of chilling in the minds of the polar night, it is very cold and hanging, with the statements of the straining surface temperature inversion; Its characteristic power is low temperature, low volume, high vision. The intrusion of the whole meal will lead to the sharp drop in temperature in the area, as the bullets come in bulk. Arctic povitrya, if it is to come to Europe through the Barents and Karske seas, to be called continental; to the new head rank and the characteristic is introduced. Arkticheski povitrya, how to go from the area, which is connected to Greenland and Spitsbergen, to be called marine; passing over the warm sea currents, the wine has risen to the bottom; ascend and overhang, if the continents are still warmer, the instability of the polar sea wind will be able to cope with the vertical circulation in new and vypadaniya angry fallen; The charge is unstable, and when the sea is invaded, the weather is clear and frosty.

2. Between latitudes, For the names of the polar ones, for example, for the proposition of L. Berg, boreal, to form in the anticyclones of the lower latitudes from the arctic winds and winds, which come (at the upper balls) from the paths.

In anticyclones over land - over forests and steppes pomirny belt, A charge over the ground, pokrit_y s_gom, pretend to be continental polarity, hot vlіtku, even colder vіtrya. V Go to Europe wine penetrates from the USSR, Finland and Scandinavia. Morsky, on the other hand, settles in the lower latitudes above the ocean - in the middle part of the oceans above warm leaks, In the wilderness over the cold. Material for yo formulation, except for arctic and tropical food, serve as a continental polarity. V winter hour The continental polar and the arctic turn into the process of the formation of the sea polar wind heats up and grows larger, the Arctic warms up, and the continental polar cools down. Povitrya Morske Polar, why come to Europe for a charge from the middle and high latitudes Wine of America, And a drop from the high latitudes of the Atlantic, to bring in the winter hour long, cold weather.

3. tropic good to settle in the anticyclones of the subtropical belt - the sea over the oceans (and in the western part of the oceans, the sea flows, In the cold), continental over the steppes and heaths. In the form of a tropical weather, take the fate of anti-passati, going down in dynamic anticyclones, as well as sea and continental polarity. Anti-passati in falling currents are adiabatically heated; as the stench sinks over the sea, then the heat is seen from the polystyle surface, as well as over the land, then the additional progression from the polystyle surface is the weather. Obviously, it’s a lot of money to come to Europe with high temperatures. Until the vіn yde u viglyadі passatіv abo musonіv.

Occasional coverage of the tropical seafood, which is important for the European weather and climate, the subtropical regions of the ancient part of the Atlantic Ocean, the continental life is shaped over pіvnіchnіy Africa, Arabia, Little Azerbaijan, the European part of the USSR, Kazakhstan and Middle Asia.

4. equatorial turn, Performances of anti-passages, as well as passats, if the stench overwhelms the ekvator and gets into the іnshu pіvkulya, to form over the ocean. tropical forest in the smoothies of calmness from the tropic food of the pasats and at the same time it is very perturbed.

In such a rank, the incidence of leakage, the condemnation of those is accompanied by a significant world of thermal reasons, є carriers of heat and cold, that is, they pour themselves on the temperature, and then on the atmospheric grip and the circulation of the atmosphere. The heat from the equatorial areas in high latitudes is transferred not only from the weather (like heat), but from the water vapor, but the rest, condensing de facto, seeing the warmth of the steam room. So sleepy warmth will rise in price on krill on the face of the Earth.

Yaksho vi knew the mercy, be weasel, see a fragment of the text and natisnit Ctrl + Enter.