Drinking a lot of temperature is called. Powers and fronts

By the growing masses, they call it somewhat the same depending on the temperature and the weather of the mass, as it expands on the area in a few thousand kilometers and a few kilometers at a height.

The stench is formed in the minds of a trivial transfer to a greater extent by the one-sided surfaces of the land or the ocean. Moving in the process of the atmospheric circulation of the atmosphere in the inner regions of the Earth, we tend to transfer to the central regions and their own weather conditions. Panuvannya in this region in this particular season of singing masses has a characteristic climatic mode of performance.

Razrіznyayut chotiri basic geographic types of masters, which hunt the entire troposphere of the Earth. Tse massi arctic (Antarctic), pomirny, tropic and equatorial food. Behind the blame of the rest, in the skin they see more marine and continental patterns, which are formed over the land and the ocean.

Polar (Arctic and Antarctic) sometimes forms over the crooked surfaces of the polar regions and is characterized by low temperatures, small in terms of science and good vision. The intrusion of the continental arctic fever in the middle of the latitude is subject to severe frosts. Morskie arkticheskoe povitrya, scho to form over the ocean in the polar regions, vilnyh through the ice, see a great vologue and even more high temperature.

Pomirny povitrya is signi fi cantly more beautiful than programs; Overwhelming here by the back winds and cyclones, the sea, by and large, is transported far into the continent, not so often with litter. The continental climate is getting very cold, and the weather in the new style is clear and frosty.

Typically, it is generally characterized by high temperatures. A little over the sea, there is an immediate arc, then over land, navpaki, it is superbly dry and washed down. Oscillations of the tropic grow more and more at baric highs, but only some stars expand in the middle and the equatorial latitudes, de atmospheric grip lower.

Equatorial power is referred to as post-high temperatures and changes in the environment both over the ocean and over land. At midday there are parts of the planks.

povitryanі masi Due to the low temperatures and the environment, they are gradually changing and in the university space, they are being developed between themselves. Umovna the surface, where the dislocation of the masses, is called the atmospheric front. In case of overturning of a clear surface on the earth's surface to assert so called the line of the atmospheric front.

The surface, which is divided into the Arctic (Antarctic) and in addition to the twilight, is called the Arctic and Antarctic fronts. fortunately in the middle latitudes and paths to the polar front. Oscillations of warm weather are less, lower than cold, then the front є abducted area, as soon as it went towards the cold weather, even further small kutom (less than 1 °) to the surface of the earth. It’s colder in the morning, as it’s thicker, when it’s warm, it’s not fueling, and when it’s up, it’s wicked.

Having set up, the growth of the masi continues to collapse in the bik masi, moving at a higher speed. The frontal surfaces open up directly to the collapse of the cold and warm fronts. If it is colder and colder, it collapses more than warm, atmospheric front call yourself cold. When the cold front passes through, the atmospheric grip of growth is growing, and the volume of things is decreasing. If it is warmer when the advance comes and the front moves towards low temperatures, the front is called warm. When a warm front is passed, it is warmer, the vice will go down, and the temperature will go up.

The troposphere gradually grows, grows and knows vortexes of small growths - from small, up to giant cyclones and anticyclones in terms of area.

cyclone- we lower the area with a vice at the center (Fig. IV .4). That is why the wind in the cyclone moves along the spiral from the periphery (from the areas of the high vice) to the center (into the area of ​​the low vice) and then go up the hill, settling vishіdnі streams. In the cyclone, it collapses along the curved path and the straightening of the anti-year-old arrow in Pivnichny pivkuli and behind the year-old arrow - in the Pivdenny one (Fig. IV .4). Cyclones have tied great areas of cold and fallen, significant changes in temperature, strong in three. However, vіdomі th cyclones, as іnuyutsya stretching the rocky rock in the postіin areas of a low grip: Icelandic cyclone (minimum), rosetting in Pivnichniy Atlantitsi in the region of about. Iceland, і Aleut cyclone (minimum) in the Aleutian Islands area on the Pacific Ocean.

In the middle latitudes, cyclones are spared in tropical belt. Tropic cyclones appear only over the sea, between 10-15 ° N. і PDS When you go to land, the stench quickly goes out. There, as a rule, are not large cyclones, their diameter is close to 250 km a little further with a low grip in the center. Tropical cyclones move at a speed of 10-20 km / year in the main winter at the end, but at the same time they go towards high latitudes (for example, in Pivnichniy trees, the stench collapses during the winter). There are even tighter eddies with very strong winds (20-30 m / s, in pores up to 100 m / s and more), which are stronger than hvilyuvannya on the sea and great ruining on land. On the earth, in the middle of the year, there are more than 70 types of tropical cyclones. Smells of the best in the region of the Antilles, bilya of the ancient Uzbek coast of Asia, in the Arabian Sea, Bengal zatotsi, on the way to. Madagascar. In the rural areas, the stench may be called the name ( cyclone- in the Indian Ocean; Hurricane- in Pivnichniy and Central America; typhoon- in Skhidniy Asia). Cyclones are especially characteristic of the territory of Europe, because they move from the Atlantic to the turn and go up to 5-7 dB, so that the atmospheric pressure does not go away.

Small. IV .4. Rukh turn into the earth's surface:

a - in cyclones; b - in anticyclones

anticyclone- tse area with a vise in the center (Fig. IV .4). The staff of the anticyclone is directed towards the center (from the area of ​​a larger vice) to the periphery (in the area of ​​a larger vice). At the center of the anticyclone, it goes down, settling downstreams, and grows into the small sides, to go to the center to the periphery. At the same time, it is possible to wrap it up, but rather to wrap itself up against cyclonic ones - it’s just to see for the year-old arrow in the Winter season and against the year-old arrow - in the Pivdenny one (Fig. IV.4). Anticyclones in the middle latitudes most often follow the cyclones, the stench doesn’t often take a low-level (stationary) camp, and it also runs until it’s quiet, as long as the grip doesn’t go viral (6-9 dB). There is no cloud formation in anticyclones in anticyclones; weak vіtra and calmness. In the middle latitudes, anticyclones in the largest world widen in subtropical latitudes - in the belts of a high vise. Here it’s post_ynі, like іsnuyut stretching out the atmosphere of the atmosphere vichori (the area of ​​the high vise): Pivnichno-Atlantic(Azores) anticyclone (maximum) in the regions of the Azores and Pivdenno-Atlantic anticyclone; Pivnichno-Pacific(Canary) anticyclone in the area of ​​the Canary Islands in the Pacific Ocean Pivdenno-Pacific;Indian anticyclone (maximum) in the Indian Ocean. Yak Bachimo, all the stinks are roasted over the oceans. One taut anticyclone over the land of Vinik is charged in Asia with the center over Mongolia - Aziatsky(Siberian) anticyclone.

The size of cyclones and anticyclones of porous size: the diameter can reach 3-4 yew. Km, and the height is a maximum of 18-20 km, so that the stink is a flat vichor with a heavily heaped wrap. The stench will change from the entry to the highway from the speed of 20-40 km / year (except for stationary ones).

About The hot sea lies in the zone of the Asian-Pacific monsoon circulation of the world latitudes, due to the periodic nature of the at-mospheric processes. Musoni clearly hangs up to the latitudes of the ancient Sakhalin, over the winter season of the sea monsoon tendencies appear.
Have Vimir latitude is the arena of the most intense cyclonic activity on the Arctic and polar fronts. The Arctic front, which is the first cordon of the Arctic region (the Okhotsk Arctic front), may lie parallel to the coastline of the Sea of ​​Okhotsk. Vlіtku vіn vіdstopaє to sіvbі-ru, close to the edge of the ice of the Pivnichniy Ice Ocean.
NS The polar front, which is growing in peace and in the sea tropic of the weather (the beginning of the Pacific Ocean Polar Front), is growing in the Pacific Ocean, parallel to the Great Curve Ridge.
Before The summer-forming value may also be the Pacific Arctic Front over the Bering Sea, the Pacific polar front on the northern coast of Alaska, as well as the secondary cold front, but lie close to 40 ° N. NS.
About Mainly by the masses є the continental arctic fortune (Kav), the continental peace of the fortress (KUV), the sea peace of the fortune (MUV), the other row means the marine and continental tropical fortune (MTV).
Before the ontinental arctic turn to form over the Pivnichny Freezing ocean and the closest to the Arctic land. The bribe in the fire is formed to grow, thirsty Taimir, Kolima and Chukotka, vlitka - speed up, entering the coastal line of the Arctic basin. For caves, low temperatures are characteristic, low moisture content and a little bit of penetration. The temperature rise in the spirit over the Arctic Trochi vishche, below the Asian territory, the Siberian (Asian) anticyclone develops with dry and cold weather (CCW). In addition, the transfer of cavalry to the Polyuvan Sea during the winter period means advection of heat. This summer invasion also does not wick cold, so as the crossing over the Poluvan Sea Mouv appears to be a sign of the coldness of the Arctic fever, which was warming over the mainland in Russia. During the transitional seasons, the weather is colder due to frost and cold weather.
Before Ontіnental pіrne vіtryut over Transbaikal, Yakutієya, Verkhnіm Amur, grabbing the Lensk-Kolimsky district, de-collecting from the ground also overwhelming the field of the shifted vice-nya. Deviate from even lower temperatures, straining ground inversions and little vology. For a short hour, the formation of Kuv over the progressed continent is moving unstable, but not at all, it is possible for a short hour to set up a stratification of stratification (ground inversion) in the lowest sphere of the world. Take the pole to the cold pіvnіchnoі pіvkulі to rise in Yakutia, de mid-month temperatures can be up to -50 ° C, and at least -60 ... -70 ° C and lower. The order of the thriving continentality and the overwhelming anti-cloning nature of the weather, the strong volatility of the territory contributing to the negative formation of the relief: in the big deputy-battles of the street and the valley, the spirit is cold and cold. As a result, there are trivialities here that are even worse than low temperatures. That was the main part of the cold for the Sea of ​​Okhotsk fortune-teller to lay down at sunset, and not at winter. Continental in the midst of winter in Russia from the winter-west to the early stage of the winter monsoon with strong backward and winter-backward winters and sharp lower temperatures during the winter. Above the cold Sea of ​​Okhotsk, there is a large part of what is charged by ice, the strength of the Kuv is to be seen, because it does not fall.
B Older role is the transformation of the cavalry and the Kuv into a transitional turn, close to the authorities to the Mov, which borrows practically the entire space of the sea.
M Orskoy around the world will form over the distant seas and the old part of the Pacific, the ocean and the ever-warm and modern world.
L Litku Mov є By the turn of the lithuanian monk and mayzhe will be found in the village of Nastya Vologo. When passing over the cold pedestrian surface of the Sea of ​​Okhotsk, especially in the places when going to the surface of the cold waters of the intermediate ball, it is very cold and swelling of the strata-syphi with some types of condensation Mrya and super-dense fogs, which are collected for several days.
Zіmoy Mov bolsh is often spied over the eastern part of the sea, and on the first invasion of the sea. Zvvychay vіn come to the front part of the cyclone, roztashovany over the Sea of ​​Okhotsk, ob_yshevshi yogo from the beginning, winter and winter descent. So how's it going to come from The Pacific That, shifting over the cold surface of the Sea of ​​Okhotsk, wi-viklikayut a gloom, with the fall of the weather, rіzki warmer with positive temperatures, wіll hаvіt in the coldest time of rock.
About Chag formed by MTV is an area of ​​the Pacific subtropical anticyclone, flowing from one to the other and the Japanese Sea. Continental tropic growing up over Central China and Mongolia.
Before Ontіnental and sea tropical air (іх іні і і і рістікію here as subtropical іtryanі masi) invade the Sea of ​​Okhotsk from the cyclonic endorsed by the triviality. Zokrema, KTB, permeate on pivnich, reach in the warm sectors of cyclones up to 50 55 ° N. NS.
V on the cob lita the polar front to pass by about. Taiwan, in the middle - close about. Honshu, before the end of the summer, the world weakened the Okhotsk anticyclone to seep into a greater latitude.
Z nya the polar front to bring before the invasion of warm and vologous masses of MTV, which will bring ryasnі fall, often і angry.