Yak pouring into the weather sea flows

However, it seems that our planet would be correctly named not the Earth, but Water, and even land ("earth" yak taka) - just a quarter of the surface. The Іnshy space is to lay on the oceans, to become a light ocean. Itself in new, yak allow vchenі, if life has been born ... and until the whole day the ocean is rich in what means life on land. And on the right there are not only in ship-going, but also in the land of the land, in the Ribolovets industry, at the time of the year-old rich people, not only in the usual kind on the sea coast of Uzbekistan ... viznachaє klimat.

Svitovy ocean is in post-rus... Streams of water in a new - a kind of "rivers in the ocean" - are called leaks. The stench is persistent and periodic, submerged and superficial, cold and warm, tired (does not change in the hour) and tired (changes).

Reasons for creating sea ​​flows, Deliver rіznomanіtnі. Є tidal currents, especially strong shores, compensation, tied to the flood of the sea, wintry, and moreover, the last three, so that it changes directly in the desertedness throughout the season, generate the same current - the monsoon. Viklik's current and development in atmospheric vice over the surface of the ocean.

Continuously flow may be corrected. Some of them are repaired in low latitudes and collapse to high ones - the stench carries warm water, and they are navpaki, even cold currents. Oskilki the head "accumulator" of sleepy energy on our planet is the ocean, then because of the sea current it "blows up" and "blows out" the warmth of the young women of the land, it is enough to keep the weather on the Earth, and the oskilki current is postponed.

Deyakі persіynі current navіt otrimal vlasn_name- for example, Golfstrom. Heat flow from Florida to Scandinavia, Barents Sea and Pivnichniy icy ocean... The width of the current flow becomes from 70 to 90 km, and the depth of the current may reach the bottom. The heat "little river in the ocean" will change my skin for a second about 50 million cubic meters of water - more, less than the little rivers of the Earth, at once! When the ocean current brings warm water from the Mexican inflow to the sea, it carries up to 100 kcal / cm2 heat - about a stile, but it will take away from the Sunshine ocean as a whole. The very charge of the port of Murmansk does not freeze - it is unimportant to those who move the wines behind the polar stake. Pom'yakshu vin i klimat European countries, Snuggled up to the Atlantic Ocean: in Pivnichniy America at the same latitude the klimat is big suvoriy. Well, the merit of the first crossing - the Labrador one. It is, of course, colder, ale stikayuchis behind the warm Gulfstrom, vono vidhilya yogo, directing in the direction of Europe.

However, I do not diminish the role of the current climatic minds of cold and cold currents. So, everyone knows that it is hot in the paths, and there is not enough of it to be missed, how it could be more spectacular there (maybe it’s not possible to live), because it’s not colder Humboldt (won - Peruvian) Of America... The very stink of nadayuchu "cooling" flowing into the tropical region. At the same hour, pouring in the Peruvian current to "dry" the climates of Pivdennaya America, emptying empty spaces.

Sea currents pour not only on the temperature of the weather, but on the fall of the winds, only to provoke hurricanes.

Yak bachimo, ocean currents - the essence of the "factory" wait. To change the stench - to change the climate as a whole. The first changes are seen right before our eyes. So, it is no longer the first risk of charging "overwhelmed" with money Go to Europe, Pokey not call until I become right. Vcheni explain the things, how to help and achieve Golfstrom. Tied together with the process of global cooling ... well, well, cold weather itself. niyakogo global warming Nemaє - and the axis of coldness is even close to three cities, and at the very least, this is the cooling of the GolfStrum. Why is the price tied with the power of the people? The head of the Department of Rational Environmental Studies and the Ecology of Geography, Faculty of the Moscow State University, Academician A. The globally cold weather is tied to the mercy of the magnetic poles, the earth's axis and the wrinkle of sleepy activity.

The circulation of the waters of the Holy Ocean is due to the exchange of a number of speech, heat and mechanical energy between the ocean and the atmosphere, surface and clay, tropical and polar waters. Sea currents carry great masses of waters from some regions to others, often to reach the further districts. The current will destroy the latitude zonality in the temperature rise. In all three oceans - Atlantic, Indian and Pacific - there are temperature anomalies in the flow of currents: positive anomalies associated with the transferred warm waters are adequate in higher latitudes by currents, close to the possible voltage; Negative anomalies against cold leaks (from high latitudes to adequate). Negative temperature anomalies will be accepted, in addition, if clay waters on the backs of the continents, wikklicanim the stormy waters with pasatny winds.

In the flow of currents, it is not only the magnitude of the rise in average temperature values ​​that is recognized, but rather the magnitude of the temperature range. It is especially clear to manifest itself in areas where warm and cold flows are closed, there, between them, to be Atlantic Ocean in the areas of the Gulf Stream and the Labrador Current, in the Pacific Ocean, in the area of ​​the Kurosio and Kuril Islands (Oyasio).

These are injected on the rosters of the other oceanological characteristics: salinity, instead of sour, biogenic rivers, colora, progression and in. The growth of the characteristics can be a great inflow for the development of biological processes, tvarinny svit sea ​​and ocean. The minority of sea currents in the space and space, the change in the frontal zones infuses on the biological productivity of the oceans and seas.

Great inflow to curb the current on the Earth's climate. For example, in tropic areas, de perevazhaє late transfer, on backsides oceans tend to be cold, fallen off, voluptuous, and in the midst of the continents, there is a dry climate. The current is simply pouring on the vise and circulation of the atmosphere. Above the axes of warm leaks, such as, for example, Golfstrom, Pivnichno-Atlantic, Kurosio, Pivnichno-Tikhookeanske, a series of cyclones collapsing Wash the weather coastal areas in the mainland. Warmly, the winter-Atlantic stretch will help the Icelandic minimum, and, moreover, the intensive cyclonic activity in the Old Atlantic, the Baltic and the Baltic seas. Similarly, injecting Kurosio into the Aleutsky minimum region in the pivnichno-skhidny district The Pacific... Z warm leaks Penetrating in high latitudes, cyclonic circulation of the atmosphere is tied, which is associated with the fall of atmospheric fall. Above the cold leaks, navpaki, vіdrogs of a vise grow, scho wiklikє a change in the number of fallen. In areas with warm and cold streams, fog and cold weather are often associated.

There, de warm, the currents penetrate deeply into the world and the polar latitude, which flow into the climate is especially well known. Dobre vidomo scho pom'yakshu injected into the GolfStrum, the Atlantic-Atlantic Current and the Yogi Gilok on the Europe climate, the Kurosio current on climatic mind private part of the Pacific Ocean. As a sign of a greater significance in the whole of the current period of the Atlantic-Atlantic current, below the Kurosio, the same as the Atlantic-Atlantic stretch penetrates at a 40 ° level on the private to the Kurosio.

Risky prominences in the climate are set in the same way as the coast of continents or oceans is washed by cold and warm currents. So for nothing, Shidne uzberezhzhya Kanadi is located under the influx of the cold Labrador current, while the Uzbeks of Europe are washed by the warm waters of the Pivnichno-Atlantic Current. As a result, in the zone between 55 and 70 ° N. NS. The triviality of frost-free period on the Uzbek coast of Canada is less than 60 days, on the European one - 150-210 days. Let us use the butt to pour leaks into the climate and weather and let us serve the Chilean-Peruvian cold leak, the temperature of the waters is 8-10 ° lower than the waters of the Pacific Ocean. Above the cold waters of the current disastrous masi, Cool down, fix the suspicion of sharuvat-kupchastnykh chmar, as a result, in Uzbek Chile and Peru, susceptible chilliness and the appearance of fallen asleep are promoted. Pivdenno-lateral pasture in the ts'm district surface watersі from the cold clay waters. If Uzbek Peru is only in the midst of a cold current, this period is characterized by the midst of tropical storms, boards and thunderstorms, and at the same time, especially when there is more and more warm weather on the coast. runt, zhitlov_ sporudi, dams, nasipi.

pulsations ocean currents, Meandering and shifting of their axes on a daily basis, or just pouring into the climate of coastal areas. One-hour watchful for the rise in temperature in the interiors of such large-scale streams, such as Gulfstrom and Kurosio, vyavleni zivini (meanders), which may have a sickly character. The stench of the meander richok and at the viglyadі the thickening of the isotherms in the axis of the head stream is changing at once. For example, starting the axis of the Kurosio for a week and a half at a distance of 350 miles between 34 and 40 ° N. NS. The position of the fronts Kurosio - Oyasio, Gulfstrom - Labrador and the last half-month, monthly, half-month, small and large-scale flows. At the link with the cym, there is a number of climatological and meteorological factors on the Uzbek coast of the adjacent continents. Weather mind Japan to tie up the front of Kurosio, climatic minds of the Kuril ridge, Fr. Hokkaido and celebrations Honshu is known by the flowing cold current Oyashio.

LORD WEATHER

The atmosphere and the ocean are in a tight, uninterrupted interaction... Sleepy lanes, falling on the surface of the ocean, heat the water, and the ocean accumulates great reserves of thermal energy, especially in tropical waters, de interchanges fall vertically. The surface of the ocean transfers its warmth to the water vapor, as it flows up the mountain in the process of vaporization of the surface balls of water. Wager, to take revenge in the twilight, may be a significant reserve of potential energy in viglyadi warmth, as vivilnyaetsya at condensation of wager in chmaras. Energy to the ocean people They take away new streams of heat from the surface of the sea to generate new ones.

Weather and climate є a manifestation of our nature and in the meaning of the world is located in the flowing ocean.

The inflow of the Svitovoy ocean into the weather and the climate lies among the physical features of the majestic mass of water, which is located in the yogo pools.

We love the power of the ocean є the health of the water and the warmth, and sea ​​water ma great warmth - health akumulyuvati warmth... There is a majestic amount of sleepy energy, and a ten-meter ball of ocean waters, more warmth, less the whole atmosphere. Sleepy lanes with the same intensity heat the surface of the sea and land, ale water, with great warmth, glaze much more warmth at a somewhat stable temperature, at the same hour the temperature drifts strongly. As the sun sets, the land temperature drops sharply, and the sea reaches more and more.

The earth's crust, being solidified with a strong speech, only the warmth of the upper spheres, and the sea, which is located in uninterrupted Rus, changes the upper warmth and the lower, more cold balls and widens the warmth on large areas over the course of the current. Accumulate the ocean as much as possible to vaporize water from the surface I will glaze a great amount of warmth.

Accumulate and secure warmth, the ocean rules the planet's climate, Vidіlyayuchi in the new two main zone: continental and sea. The sea climate is typical for all regions of the land, which is washed by the seas, the continental one is for the land masses of the land... With a typical butt of a sea climate, you can match the climate of the British Isles: the temperature is equal to the whole rock, it is colder in summer, and the winter is soft, the sky is tightened with gloom and the boards are blowing tsiliy rik... The central regions of Siberia are becoming a continental climate: winter is cold and late summer, drylands are changing with thunderous boards. The central regions of Asia may have a very continental climate: it will take a severe frost, and a whirlwind sky and a sweltering sun will re-create everything in a snow-covered environment and saw space.

The inflow of the sea to the temperature of the rural regions of the Earth is the main reason for the winery... famous muson of the Indian Ocean to enjoy the seasonal temperature of the ocean and the majestic mass of land lying on the winter. With a stretch of speckotny, typical for the whole region of the planet, the land warms up much stronger, lower the ocean, which is a larger part of the sleepy energy of the Akumulyu. As the land is very hot, it heats up and winds up, the power of which changes, so that the zone of lowered vice becomes wider. The temperature is higher over the ocean. pіvdenno-zadnі muson, Yakі dmut from the apartment to the zhovten. The charge on land is cooler, it gets cooler, below the ocean, and the zone of high and low vice is reduced by the small ones, and when the masses go straight from the land to the sea, they pretend pіvnіchno-skіdni muson, Yakі dmut zhivtnya for a week. The growth of the continents and oceans is not enough to prevent the monks from reading them directly, rather than wrapping the earth to make their correctives directly to the outside.

Cold and warm ocean currents also pour into the climate of the planet, especially the coastal regions... Climate of the coastal regions of the Spanish Atlantic in the significant world of three flows - Gulfstrom, Labrador and Skhidno-Greenland... The warmth of the GolfStrum will arise in Mexican zatotsi i, rushing into the ocean through Florida duct, Conceal two houses with straining gilks to the coast of Europe. Cold Labrador and Greenlandic currents heading for pivden, de, zustrіchayuchis Gulfstrom, reduce the temperature to 5 - 8 ° C, which in the smallest steps take and cold pіvnіchnі vіtri. And yet Gulfstrom is to bring a significant part of its warmth to the shores of Europe, which makes the character of the climate of the region clear. The entire European coast at pivnich vid Gibraltarskoy ducts to be found in the Gulf Stream, which is like a fire to Scandinavia and reach Spitzbergen Islands, Outside the Uzbek coastline Baltic Sea near Tallinn and Riga, Roztashovane for pivden at 30 °, be covered with ice.

At the middle latitudes, when the majors collapse at the entrance to the skid, the climate is found in the flowing ocean and the western winds at once. That climat of two places - the Japanese Yokogami and the American San Francisco, which lie on the same latitude from the lower sides of the Pacific Ocean, strongly resemble one in one. In Yokohama, the temperature reaches 28 ° C, and in the climate of all rice is continental, and in San Francisco - 17 ° C and the climate is sea.

Ocean regulates the fall over the mainland... If in the atmosphere there is a failure in theology, there will be a vaporization from the oceanic surface, and a volatile mass will be sucked onto the land, bringing with them boards and cyclical storms of anger - hovering over the continents.

The majestic oceanic expanse, stealing with the atmosphere, providing uninterrupted gas exchange - the upper balls of the ocean, being sour, being seen when photosynthesis for plankton, Zbagachuyut the sour lower balls of the atmosphere. The ocean is called the "lungs" of the planet. So people can drive uzberezhzha to themselves, it’s easy to get crazy.

The ocean is not just a global inflow to the Earth's climate, but it controls the weather in a small area... In addition, there is a difference in the heat capacity of the sea and the land, there are people taking in cold weather in three sea Uzbeks - breezes. In the afternoon there is a sea breeze, then for a day everything calms down, and the coastal breeze starts blowing. An offense to the weather is more beautiful than a hostess in quiet, sleepy weather, because it doesn’t change the speed of 5 m / sec and if it’s like a winter, it’s easy to extinguish the stench. Breeze is the same muson, Only a small scale with an additional cycle in a straight line.

Ocean currents show especially low fluctuations in temperature regimes of the sea surface and they themselves pour into the temperature rise during the atmospheric circulation... The strength of ocean currents is to lead to the point where it flows into the atmosphere is not very important. The comb of isotherms on the maps of the average temperature is a direct indication of the warmth of the Gulf Stream on the climate of the secondary part of the Winter Atlantic and Western Europe.

Cold ocean currents can also appear on the middle temperature maps, depending on the type of borealis in the configuration of isotherms - cold, directed to low latitudes.

Above the areas of cold currents, there is a recurrence of fogs, winter weather in Newfoundland, and sometimes it can pass from the warm waters of the Gulf Stream to the cold waters of the Labrador current. Over the cold waters in the passate zone, convection is rising and the temperature is changing rapidly. Tse, in its own accord, is a factor, which is the way to see the so-called coastal kestrels.

Injection of snow and dewline cover to the climate

Snigovy (crying) covering the change in heat dissipation by the soil and the amount of temperature. The top cover will display sleepy radioactivity in the daytime and cool off in the nighttime, which will lower the temperature of the surface sphere by night. The hinges on the tannins of the snow cover are vitrified by a great amount of heat, which is taken from the atmosphere. In such a rank, the temperature over the tanya sigovim cover, will be close to zero. Above the snow cover, the inversion of temperature is spared: the charge is tied with the radio frequency change, the canopies are connected with the tandem of the snow. Above the permanent snow cover of the polar regions, one can see inversions or isotherms. Tanennya snigovogo pokryv zbagachu soil vologoi and maє great value for a climatic regime of warmth pore rock. A great albedo of the snow cover should be produced until the growth of radioactivity and overall radioactivity and illumination is improved.

Dense grassy covering decreases the temperature amplitude of the ground and decreases the temperature middle temperature... Also, I change the amplitude of the temperature of the meal. More foldable flow into the climat is small, which can be overshadowed by a number of falloffs, in addition to the shortness of the stylish surface.

However, the inflow of the dewline cover can in the main microclimatic meaning, as it expands over and over on the ground balls and on small areas.

Backbone of the circulation of the atmosphere

The backbone circulating atmosphere is called the system of large-scale alternating leaks over earth quake So that such flows, as for their own sizes, can be compared with the great parts of the continents and oceans. From the backward circulation of the atmosphere, there are masses of circulation, such as the breezes on the Uzbek seas, the mountain-valley in the middle, in the ice in the middle and in the ice. The cyclical circulation of the hour in the singing areas is superimposed on the backward circulation of the atmosphere.

at home synoptic maps wait, you can see that at the time of the Danes, the flow of the zalous circulation over the great areas of the Earth, or over the earthly kulei and how the whole process of growth is constantly changing. The versatility of the extravagant circulation of the atmosphere is especially due to the fact that in the atmosphere there are glorious sicknesses and vichoros that gradually evolve and change in a different way. The process of setting atmospheric storms - cyclones and anticyclones - є naybilsh characteristic feature backward circulation of the atmosphere.

However, in the outward circulation of the atmosphere, with all the versatility and unrestricted changes, it is possible to recall and do some permanent specialties, which will be repeated in a short time. Such special features are most beautifully seen behind the addition of statistical averaging, when the circulation is increased more and more smoothly.

The average size of the grip over the dermal drink decreases from the winter season to the summer season. From every day until the lime tree, drop over the wine drink by a mb; in the new season, there will be a ringing change. Alle the atmospheric grip of the doorway of the fortune, and that means, the proportionate weight of the fortune. Tse means, for that season, at any time it’s summer, as it’s the time of the day, at that winter time. This is how the seasonal exchange of food and drink can be seen. For pik z pіvnіchnoі pіvkulі 1013 tons are carried back to the first week and back.

We turn now to a more detailed view of the minds of the outward circulation in the zones.

The circulation of the waters of the Holy Ocean is due to the exchange of a number of speech, heat and mechanical energy between the ocean and the atmosphere, surface and clay, tropical and polar waters. Sea currents carry great masses of waters from some regions to others, often to reach the further districts. The current destroys the latitude zonality in the temperature rise. In all three oceans - the Atlantic, Indian and quiet, there are temperature anomalies: positive anomalies associated with the transfer of warm waters as adequate in higher latitudes in currents, such as Negative anomalies of wiklicans are protracted by cold leaks (from high latitudes to adequate). Negative temperature anomalies will be accepted, besides, by the gulf waters off the western shores of the continents, by the windy waters with windy weather. [...]

In the flow of currents, it is not only the magnitude of the rise in average temperature values ​​that is recognized, but rather the magnitude of the temperature range. It is especially clearly manifested in areas with warm and cold currents, where, between them, there is a long river, such as, for example, in the Atlantic Ocean, in the area of ​​the Gulfstream and Labrador currents, in the Pacific Ocean in the Pacific Ocean. [...]

These are injected on the rosters of the other oceanological characteristics: salinity, instead of sour, biogenic rivers, colorah, prozorosti and іn. The growth of these characteristics can be a great inflow for the development of biological processes, growing and growing light of the sea and oceans. The minority of sea currents in part and space, the change in frontal zones infuses on the biological productivity of the oceans and seas. [...]

Great inflow to curb the current on the Earth's climate. For example, in tropical areas, de-transient transfer, on the western shores of the oceans, there are more signs of coldness, fall off, vologism, and among those who are dark from the mainland, there is a dry climate. The current is simply pouring on the vise and circulation of the atmosphere. Above the axes of warm flows, such as, for example, Golfstrom, Pivnichno-Atlantichny, Kurosio, Pivnichno-Tikhookeanske, a series of cyclones collapse, which visually start the weather in the coastal regions of the mainland. Warmly, the winter-Atlantic stretch will make the Icelandic minimum squeeze, and also the intensive cyclonic activity in the Pacific Atlantic, the Baltic and the Baltic seas. Similarly, injected Kurosio into the Aleutian minimum region in the pivnichno-skidny region of the Pacific Ocean. [...]

In areas with warm and cold streams, fog and cold weather are often associated. [...]

There, de warm, the currents penetrate deeply into the world and the polar latitude, which flow into the climate is especially well known. Good luck to the flow of water to the GolfStream, the Atlantic-Atlantic current and the third party to the climate of Europe, and the Kurosio current to the climate of the winter part of the Pacific Ocean. As a sign of a greater significance in the whole of the current period of the Atlantic-Atlantic current, below the Kurosio, the same as the Atlantic-Atlantic stretch penetrates at a 40 ° level on the private to the Kurosio. [...]

Risky prominences in the climate are set in the same way as the coast of continents or oceans is washed by cold and warm currents. So, for example, the Uzbek coast of Canada is located under the inflow of the cold Labrador current, while the Uzbek coast of Europe is washed by the warm waters of the Atlantic-Atlantic leak. As a result, in the zone between 55 and 70 ° N. NS. The triviality of frost-free period on the Uzbek coast of Canada is less than 60 days, on the European one - 150-210 days. Let us use the butt to pour leaks into the climate and weather and let us serve the Chilean-Peruvian cold leak, the temperature of the waters is 8-10 ° lower than the waters of the Pacific Ocean. Above the cold waters, the flow of the masses, chilling, set up a subtle crust of dark-baked gloom, as a result, on the Uzbek coast of Chile and Peru, there is a lot of coldness and a drop in the weather. Pivdenno-lateral pasture in the central region of the zganyannya, i.e., from the coast of the surface waters and along the cold clay waters. If Uzbek Peru is only in the midst of a cold current, this period is characterized by the midst of tropical storms, boards and thunderstorms, and at the same time, especially when there is more and more warm weather on the coast. runt, zhitlov_ sporudi, dams, nasipi.