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The Russian Climatologist Volodymyr Keppen has chosen a continental climate as a climatic region, which is characterized by great variations in seasonal temperatures. According to Köppen's designation of 1900, the region and its continental climate are warm in summer, as it is often booming, and sometimes even colder in winters. In addition, fall off in such climatic regions, as a rule, it is equally rosy with a stretch of rock. The very cool month of the average temperature is close to -3 ° C, at that hour the average temperature may be 10 ° C at that hour. However, the region, which is a mavologii continental climate, is not to blame for being arid or napivposushliviy. According to the Köppen system, the continental class of divisions on the Dfa, Dfb, Dwa and Dwb types, which are also called semi-realistic.
Designation of the Vologo Continental Climate
Climatic mode, which is based on average climatological characteristics of 30 rockets, vicorist trilterny code. The first letter code should always be repaired from the great letter D. A capital letter is indented: f - not visible from the classification; s - dry lit; i w - dry winter. Remaining letter: a - denotes the warmest month, the mean value of 22 ° C; b - does not resemble vimogam "a", but characterizes chotiri mіsyatsі vische 10º С.
Areas that are included in the Continental Climate
The continental climate is developed here between 30º and 60º latitude in the winter and central regions of Asia, Europe and Wine of America... Oskilki Pivdenna pivkulya is much wider oceanic territory, as well as a great sea world, as a heritage, in the whole region it is practically not possible to develop a continental climate. In such a rank, the continental climate at the same time with the continental subarctic climate is a phenomenon, which in the main view of the region Pivnіchno Pіvkulі.
The continental climate in such places as Nova Scotia, Newfoundland and Scandinavia, in the most significant world, is deposited as a sea inflow, which can be seen with a lot of frosty winters and it gets colder in summer. The American Middle East and the Old Siberian may have a much more extreme continental climate, even colder winters and more specter of summer maxima in some of the maritime regions. In such areas as Miluoki, Visconsin, the continental climate is characterized by both strong sub-arctic and sub-tropical weather conditions, but it does not lie in the middle of the season. For example, the winter is cold or the specter of the summer.
Fall off the vologo continental climate
Fall off in the main continental climatic regions, either from frontal cyclones, or from convection maltreatments, as they win, if the sea tropics turn out to be inflamed at winter behind the approaching polar front. Before such a full-fledged activity, there is a large number of regions with a particular maximum of fall off. However, it is not easy to know more one-way templates. Early summer days include strong tornadoes and menaces, especially since the polar front is overwhelmed in the early outskirts of the region. On the other side, the winter falls mostly in a snowy form, from one to the next few months, it is possible to have a strong snow cover in large regions, especially at winter. Most of the time, it starts with strong winds, when it comes from an important frontal cyclone, which can lead to the hurtovin.
Roslinnity in the Vologo Continental Climate
For viznachennyam type of rslinnosti, the most prevalent in the vologue continental climati - tse lisi. They are kindly attached to the type of climatic regime, including coniferous, leafy, green, green leaves and onions. In larger areas in the continental continental climatic regions, there is a presence of growth, such as yalitsya, alina, oak and pine, and in the main season, leafy tree species fall off leaves.
climat- the center of the lower atmosphere ball for a trivial interval of an hour.
The troposphere has been taken over by the development of the country. Given the great mind of the mind, the great volume of the troposphere, that Volodya is apparently one-sided powers and collapses as one whole.
The main powers of the skin are the temperature, the grip, the volume, the filing. The main power of the drowsy mass is the temperature, which lies in the magnitude of the sleepy radiation (the amount of sleepy heat, which comes to the Earth). A number of sleepy radioacies lie in the middle of the fall of sleepy promenades, so that in geographic latitude. More sleepy heat (sleepy radio) come to Earth. Due to the size of the sleepy radioactivity, the following types of people are growing:
1) equatorial;
2) tropical;
3) is cleaned;
4) arctic (antarctic).
The important also is the nature of the style of the surface, over which the masa is shaped; tse persh for all land or sea (ocean). Above the mainland, continental (continents) are formed, and over the ocean - sea (oceanic) emerging masi, called the subtypes. All types of children are mastered on the type, except for the equatorial one. Typi and subtype of masters are represented by letters. Whether it’s a fortune-teller, the masa will borrow an area of thousands and millions of square kilometers; All seven of the main climatic zones: equatorial, tropical (winter and early), domestic (winter and early), Arctic and Antarctic (rots in the polar latitudes). Great pouring into the mold atmospheric circulation- the regular change of the masters. In addition to the belts of the permanent transfer (the main climatic belts), there are belts, in which the two on the price (charge and charge) change: the charge of the person is one of the winners of the masa, and in the case of. Such climatic belts are called transitional, in their name the presence of the prefix "sub": subquatorial (pivnichny and pivdenny), subtropical (pivnichny and pivdenny), subarctic (abo) subantarctic; There are many transitional belts. The skin of them has a panu type climat, which is formed at latitudes that are closer to the eqvatore, and the collection is a type of climat, which are folded closer to the pole. In one and the same belt, the climate on the ocean and on the mainland is not the same. If there is a sea (oceanic) climate on the Uzbek coastline, then in the world from the distance from the Uzbek coast it becomes continental. Great inflow to the climate of the coastal territories nadayut sea flows... So, the climate in Norway, roztashanoi on the western Uzbek coast of Scandinavia, is warmer and more warm than the start of the warm current Gulfstrom: the temperature collected from the polar stake is close to Pro ° C. tsei pіvostrіv was washed by the same cold current. The most strikingly manifested in the climates of the regions, roztasvannyh in the tropical, subtropical, subarctic belts and in the world of the Pivnichnoe Pivkul, de great massif of sushi. In the lands that have been rooted in the equatorial, subquatorial, subantarctic and pomirny belts Pivdennaya pіvkulі, tsі vіdminnostі pivotіnі naagato weakly.
In such a rank, on the continents, in the middle of a series of climatic belts during Russia and from the entry into the process of developing climatic regions: the uzdovzh of the old Uzbeks - the sea climate, skidnish - along the continental, distant - continental. In some (rare) in the inner regions, in the distant and isolated from the oceans and seas, - a very continental and nareshty, on the lower Uzbeks - an oceanic monsoon climate. In addition, the climate in the mountains is to lay down all the way, to reduce the amount of heat and in theology, and to establish a flexible belt. The characteristic of the climat is given in the boundaries of the singing climatic belt For areas and including the onset of a system of climatic indicators: temperature, vice, volume, fall, wind (div.).
temperature- the leading clinical indicator, which is the beginning of the development of more types of tourism. The general regularity in the temperature rise is the decrease from the temperature to the poles. The temperature of the image on the climatic maps isotherms (lines, where points are taken from the same temperature during the singing interval of the hour). To characterize and assess the possibilities for development of tourism, it is necessary to analyze the average value of the temperature, the average value of temperatures in winter and summer, the average range of temperatures and the average temperature of the weather. Rіchny hіd temperatures - change of mid-thousand temperatures stretching through the rock. The rise in the mid-thousandth temperatures of the warmest and coldest months is called the temperature range. Chim is smaller than the normal amplitude of kolivan, tim is closer to the edge of the ocean. Most of the temperature differences may occur in the land with a very continental climate. Allow the temperature to change depending on the height; This phenomenon is called temperature inversion. Vona develop in the provinces, so there is a folding mountain relief, and above the snowy surface, high in the mountains, the temperature will rise, for winter, because at the bottom of the midges, it gets colder by the day. This anomaly is also a singing rite infused into the development of tourism. In high-mountainous areas with such anomalous winters, make sure they are most friendly for hiking tourism. rospodil atmospheric vice on the earth's surface, it also changes in latitude, from the adequate to the poles. As a result, wear the belt in a reduced vice slid in a vice(Tropical and polar). The knowledge of the magnitude of the vice is not academic, but essence practical value in tourism. The change of tourists, who are constantly living in the minds of a low vice, in the country, roztasovana in the belt of a high vice, to help healthy people in the period of adaptation, and for those who are ill, who are guarding, for example, to weaken people, it is important Indicators of the atmospheric vice of visualization on climatic maps with isobars (lines, scho to draw points, which fix the same vice). The picture is real. Over the continents and oceans, there are areas of high and low vice; the only ones to take hold of the rock: Pivnichno-Pacific, Pivnichno-Atlantic, Pivdenno-Pacific, Pivdeno-Atlantic and Pivdenno-Indian maxima and Icelandic ministerial. The only ones to be charged are: American-American, Asian and Australian maxima and Aleut minimal; or only a few: Pivdenno-American, Pivdenno-Asian, Pivdenno-American, Pivdenno-African maxims and Australian minimum. Closed area of the p_vischenny vise - maximum. The area of lowered vice is closed - minimum. Maximums and minimumi - the center of the detection of gigantic vortex flows - anticyclones and cyclones, as there may be a virtual inflow for the weather. In a closed area, which is moved by a vice, a decaying vortex is formed with a fall from the center to the periphery - an anticyclone. At the closed area of a lowered vice, a hanging vortex is formed with a collapse from the periphery to the center - a cyclone. Due to the temperature of the weather, the magnitude of the atmospheric clutch and the nature of the sleeping surface, it is also possible to lie down.
For the tourist kraynoznavchay characteristics important vіdnіvnі vologіst, ie Zmіst water bet in 1 m 3 vіrazhene in vіdtsotki. The normal indicator of the prevalence of weather is 40 -60% in fallowness in latitude. The number of fallen trees that fall under the weather conditions. Chim vische is a viable matter, tim vische vypadannya fallen. Behind the shape of the vipadannya, they fall off solid and vivid and vimiruyuyutsya a ball of water, which is established on the surface when there is a runoff and viparovannya. The number of fallen leaves, which vipali roll in millimeters (mm). The greatest number of fallen falls in the equatorial latitudes. In the tropics - a number of fallen fall, in the peaceful - to fall, and in the polar latitudes - fall. When you go into the mountains, a few fall off a couple of times to grow, then to change, it’s a cold weather, and it’s coming up here in the morning. The mode of displaying the falloff, or the daily falloff, is the price of a change in the number of times per month. Razpodil fallen on the territory of the middle of the country to lay down from the proximity to the sea, because of the temperature and the weather, because of coldness, atmospheric clutch, because of the relief, wind, when you are on the Uzbek coast of the mainland. When describing the fall, it is important to mention the number of the leaves, the flow (vypadannya mode) and form vipadannya. It’s hard to fall, but to take charge (and at high altitudes in the mountains - stretching out to the rocky rock), to set the curve, height, strength, strength and triviality of the lagoon, which is the starting point for the development of winter types of sports tourism.
viter- the process of shifting the rotation in a horizontal direction from a large vice to the least from the right in Pivnichniy pivkuli and left - in Pivdenny. Vіter is characterized by shvidkіstyu and directly. The speed of the wind rolls in meters per second, or in balls. Directly in the wind, start on that horizon, the stars dme wind. On the Earth, there is a little bit of water that is constantly dimmed by name. from tropical zones p_dvischeno vise in a straight line to the level of the middle latitudes dmut passati. From the polar belts, the grip is shifted right to the middle latitudes, the dimness of the winter-school (in the Pivdenniy pіvkulі) and the pіvdenno-wіdni (in the Pivdenniy pіvkuli) in the three. In the middle latitudes, the streams are growing and coming to the turn of the earth. Tom in outside latitudes panuyut zadnі vіtri. In such a rank, on the Earth there are three permanently dim winds: passati, retreat and pivnichno (pivdenno) shidnі. Apart from them, it is still victorious, as a result of the growth of the vice between the land and the ocean and the titles of the monarch. A grip on the mainland and from the continent to the ocean, and from the ocean to the mainland. Musoni is most characteristic on the ancient and ancient Uzbek continents. In areas of increased vice, there are also strong three, which move in different directions and may be called different names. At the same time, they are found in areas of low pressure (they are often called cyclones), they are caused by great speed and ruinous force (typhoons, hurricanes, tornadoes, tornadoes). Falsely from the minds of the world (relief, water, the height of the weather), there is a variety of winds: breezes, fenny, boru and іn. Ale in the Bagatyokh lands of the Mistsev, for example, in the empty districts of Egypt, they celebrate the hundredth inflow for the development of tourism, for which a short characteristic is needed. The weather is the camp of the lower atmosphere of the atmosphere in the dawn of the world in the dawn of the moment, or at some small time in the hour (day, dob, tizden). If you’re talking about the month, then talking about the weather will change, or about the weather type, so how can the weather change for some time. The weather is characterized by elements and phenomena. Until the elements of the wait, the temperature and the weather, the atmospheric clutch, are tolerated.
apparitions wait- viter, khmari, fall off, menace, dry land, hurricanes, etc. The weather, as it is and the climate itself, is characterized not by just taken indicators (elements and manifestations), but by its sukupnist. inflow weather minds tourism is often more significant, less injected into the climate. On a daily basis, the weather is characterized by additional abnormal temperature indicators, pressure and airiness. To assess the degree of friendliness of the weather minds, the data of additional amplitudes (drops) of temperatures, vologosti and vise are obtained. Human organism reacts to changes in temperature and vice versa. As the amplitude grows, the reaction of people often becomes painful. A good chill of temperatures is the price of a change of average temperature for an hour or so. Dobova temperature range - the price difference between the best and the lowest temperature for a period of time. Good movement of the atmospheric vice - the price of a change of the average indicator of the vice for looking at an hour. Dobova the amplitude of the vice is the price of difference between the best and the lowest indicators of the vice. The great drop in the grip is evidence of extreme instability of the weather. Wine characteristic for territories, roztashanykh on uzberezhzhі in areas of passage atmospheric fronts and close to the centers (regions) of a reduced vice. Good value for money is the price of a change in the average indicator of good value for the period of the hour. Dobova amplitude of vologosti - the price difference between the maximum and minimum indicators of the acceptable vologosti. The great drop in vologosti is evidence of the fact that the territory has been roasted either on the cordons of the climatic belts, or on the atmospheric front.
atmospheric front- tse razdil mіzh shake the masses, Who will volodyut with the powerful authorities. The front is warm and cold. The first ones bring warmth, like falling off, and the other - cold weather, getting better in the wind, fall off, menace, tornadoes. Be mindful, friendly for the frontiers, scurry in the cyclones of the surrounding latitudes. Territory, roztashovanna be-like atmospheric front, unfriendly for tourism. Hmari set up at the condensation of water steam in the rising season of the day. It’s a good idea to stay at a temperature and a good temperature. Behind the shape, feathers, sharuvats and khmari are grown. Peristi - the chain of the upper tier, such as prozor, kryzhani, which does not give fall. Sharuvati - the middle and lower tiers, and the stench itself in the main give fall, often trivial, overlaid. Kupchasti khmari - the lower tier, a little stench can reach even a greater visoti, with them tied anger, hail, menace.
Khmarnist is spinning in balls for a ten-point system. Povna hmarnost - 10 points. Naybilsha coldness in cyclones, naymensha - in anticyclones, over Antarctica and tropical heaths. Fall off at the characteristics of the weather. The boards are angry (intense, ale nontrivial), overlaid (medium intensity, equal and trivial, may be cyclonic) and drizzling (albeit trivial). For hikes: convective (during hot and light weather), frontal (when the atmospheric front is passed), orographic (on the winding girders).
There are two types of weather - cyclonic and anticyclonic. Cyclonal type wait- a frown (hmarna), nestiyka, with frequent and significant changes in temperature indicators, a vice, with clear litter, vitryana. Anticyclonic type of weather- clear (sleepy), stiyka, with small and insignificant temperature changes and vice, without falling off, bezvitryana. Nimensh is pleasant weather on the territory of udovzh line of atmospheric fronts. The types of weather and general indicators change with a stretch of fate, you can see a different type of weather for the skin season.
Vologiy Continental Climate
Vologiy Continental Climate(For poznachenya vikoristovoyutsya latin velika litera Dі small a abo b) - type of climate in Köppen's classification, Which is characterized by great seasonal temperatures during the week, with hot (or warm) vlіtku and cold charge... For the region to the regions with a large continental climate Average temperature the coldest month is to blame for being lower than -3 ° C, and we took 4 months in the middle of the month when the temperature was 10˚C.
Fall off, no doubt, by a stretch of rock. On a large part of the area, it falls over and over again, often with thunderstorms. Charging the board and the fall in the main tied with the passage cyclones and the fronts tied with them. I want klimat and it is assigned, like "vologiy", on dili middle rivn Vologosti is not so high, rather abundant, but it wouldn’t be classified as "napivposushlivi" or "dry".
Vologous continental climate is characteristic for masses, rots, as a rule, at 60 ° winter latitude, in central and rural areas Asia , Єvropiі Wine of America, I is not typical for pіvdennoї pіvkulі there is a large area of the oceans in the upper latitudes, which will help to improve the continental climate of the climate.
View of the continental climate
The continental climate is classified in fallowness during the middle temperature of the hottest month in summer and in few drops a - the middle temperature in the warmest month changes in 22 ° C (in the dry season): Dsa is in the dry season during I do not change 1/3 of the number of fallen leaves but the most recent winter month); Dwa - dry season (in the very dry winter month, the fall of the fall is not more than 1/10 of the number of fall in the most summer month); Dfa - not for clear classifications; b - the average temperature of the hottest month is 10 ° C ( warmer lito): Dsb - dry season; Dwb - dry season levied; Dfb is not for clear classification.
Dfa / Dwa / Dsa: Vologiy continental climate with hot lit
The climate of the region is classified as a logical continental climate with a hot summer at times, as the average temperature of the hottest month is 22 ° C. As a rule, such a month is linden, in some regions - sickle. The temperature of the hottest month can be up to 32 ° C, at that time the temperature of the coldest month can drop below -3.0 ° C. In the hottest month of the continent. parts Rumunia , Moldavia, Півдня Ukraine , Middle-Danish lower(Chastini Ugorshchina, Croatia and Serbia), surrounding regions of the European part Russia... In Asia - for Kazakhstan, Okremikh regions Іranu , Tureccini , Kashmiru in India, here in Pivnichno-Skhidny China, Mayzhe all Pivnichniy Korea, Zdebilsho New Koreaі Pivnіchno Japan... In Eastern Asia, the continental climate has a transitional character to the monsoons: there is a part of fallen fall, which is much larger than the part of winter fall. When injected Siberian anticyclone there are more cold winters here, but not in other regions, roztasvanih in cikh latitudes. The Pivnichniy American continental climate with a hot summer is typical for news of englandі Mid-Atlantic statesі great middle Sunset USA, Okremiy district in the Canadian province Ontario.
| Climat Chicago (norm 1981-2010) | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| exponent | Sich. | Lute. | Berezen | Kvit. | Grass | worm | Lipen | Sickle. | Sina. | Oct | Sheet. | Chest. | pik |
| The absolute maximum ° C | 19,4 | 23,9 | 31,1 | 32,8 | 36,7 | 40,0 | 40,6 | 38,9 | 38,3 | 34,4 | 27,2 | 21,7 | 40,6 |
| Average maximum, ° C | −0,6 | 1,8 | 8,1 | 15,0 | 21,1 | 26,5 | 28,9 | 27,7 | 23,8 | 16,8 | 9,0 | 1,6 | 15,0 |
| Average temperature, ° C | −4,6 | −2,4 | 3,3 | 9,4 | 15,1 | 20,5 | 23,3 | 22,4 | 18,1 | 11,4 | 4,6 | −2,4 | 9,9 |
| Average minimum, ° C | −8,6 | −6,6 | −1,6 | 3,8 | 9,1 | 14,5 | 17,7 | 17,2 | 12,4 | 6,0 | 0,2 | −6,3 | 4,8 |
| Absolute minimum, ° C | −32,8 | −29,4 | −24,4 | −13,9 | −2,8 | 1,7 | 7,2 | 5,6 | −1,7 | −10 | −18,9 | −31,7 | −32,8 |
| The rate of fall, mm | 44 | 46 | 64 | 86 | 94 | 88 | 94 | 125 | 82 | 80 | 80 | 57 | 940 |
| Dzherelo: Weather and Climat | |||||||||||||
Dfb / Dwb / Dsb: a continental climate with warm lit
Climat region clasify yak vologiy continental climate z warm litom at times, even if the average temperature of the hottest month does not exceed 22 ° C. This type of continental climate will be great for a great territory, but not a type of hot summer. У Північній America climatic zone typical for regions, rostasovanyh between 40 ° and 50 ° latitude, as a rule, on the axis towards 100 ° western latitude. However, in the region Canadian interruptions The whole type of the continental climate is defined in the masses, which are differently set at 50 ° latitude. In Europe, the continental climate with a warm summer expands right up to 61 ° winter latitude. In Europe, the type is characteristic of Central Scandinavia, the Baltic States, Eastern Austria, the surrounding regions of Nimechchynia, great Poland, Czech Republic, Slovakia, Ukraine, and Pivnichno Rumunia. The special climate of the coastal regions of central Scandinavia is characterized by a myakshi winter, which is more typical for regions with a hot summer.
For a natural continental climate with a warm summer, it is characteristic of a little summer, even in colder winters, and less than the average number of falls in regions with more hot summer, but, however, not even in the first few winter days.
Big part Mongolia and in the vicinity of the Pivdennaya region Siberia Mayut climate, close to the characteristics of the continental, however, sometimes there are fewer falloffs clasified as a region with empty or similarly empty climates.
| Klimat of Moscow: records for the entire period of caution (1879-2010 - ob'ednanі danі TSKhA + VVTs), norm 1981-2010 ( All-Russian Exhibition Center) | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| exponent | Sich. | Lute. | Berezen | Kvit. | Grass | worm | Lipen | Sickle. | Sina. | Oct | Sheet. | Chest. | pik |
| The absolute maximum ° C | 8,6 | 8,3 | 19,7 | 28,9 | 33,2 | 34,7 | 38,2 | 37,3 | 32,3 | 24,0 | 16,2 | 9,6 | 38,2 |
| Average maximum, ° C | −4 | −3,7 | 2,6 | 11,3 | 18,6 | 22,0 | 24,3 | 21,9 | 15,7 | 8,7 | 0,9 | −3 | 9,6 |
| Average temperature, ° C | −6,5 | −6,7 | −1 | 6,7 | 13,2 | 17,0 | 19,2 | 17,0 | 11,3 | 5,6 | −1,2 | −5,2 | 5,8 |
| Average minimum, ° C | −9,1 | −9,8 | −4,4 | 2,2 | 7,7 | 12,1 | 14,4 | 12,5 | 7,4 | 2,7 | −3,3 | −7,6 | 2,1 |
| Absolute minimum, ° C | −42,2 | −38,2 | −32,4 | −21 | −7,5 | −2,3 | 1,3 | −1,2 | −8,5 | −20,3 | −32,8 | −38,8 | −42,2 |
| The rate of fall, | |||||||||||||
Classification of climates is given a well-ordered system for characterizing the types of climates, their districts and cartography. Typical climates, which are rewarded on great territories, are called macroclimates. Makroklіmatichny region responsible machi bіlsh-Mensch odnorіdnі klіmatichnі minds scho vіdrіznyayut Yogo od іnshih rayonіv, Hoch i yavlyayutsya themselves lishe uzagalnenu characteristic (oskіlki not іsnuє dvoh mіsts of іdentichnim klіmatom) scho bіlshe vіdpovіdaє realіyam, nіzh vidіlennya klіmatichnih rayonіv tіlki on osnovі prinalezhnostі to designated latitudinal-geographic belt.
Climat of ice creeps Panun in Greenland and Antarctica, mid-month temperatures are lower than 0 C. At the dark winter hour, the region does not receive sleepy radioactivity, I wish there will be days and polarities there. A lot of sleepy exchanges fall on the earth's surface under a small cut, which reduces the efficiency of the program. A great part of the sleepy radio is driven by ice. As well as being charged in the summer areas of the Antarctic ice cover, the temperature is low. Climate inner regions of Antarctica on the colder climate of the Arctic, Oskilki paved mainland grow in great sizes and sizes, and Pivnichny Ice ocean pom'yakshu klimat, uninvolved on a wide expansion of pack ice. A short hour of warm drifting ice in one hour.
Fall down on the ice-covered slopes vipadayut at the viglyadі sіgu or the other part of the kryzhany fog. Internal districts can easily get 50-125 mm of fall, but on the Uzbek coast there can be more than 500 mm. Innocy cyclones bring coldness and coldness to the region. Snowfalls are often supravodzhuyutsya strong vіtra, as they carry the meaning of the snow, picking up their skel. Strong drains from the khurtovins are damp from the cold ice shield, wine grapes to the Uzbeks.
Subpolar climate manifested in the tundra regions on the northern outskirts of Pivnichnaya America and Eurasia, as well as on the Antarctic Peninsula and adjacent islands. In the schools of Canada and Siberia, the boundary between the climatic belt passes significantly more than the Polar Cola through the strong bends in the great land masses. Tse to produce until long and in the edge of cold winters. It is shorter and colder because of the average monthly temperatures, which can easily exceed + 10 ° C. Until some other days, they compensate for the nontriviality of the lith, protest on a large part of the territory of the acquired heat, which is not enough for the return of the soil. Gradually frozen soil, ranked as a permafrost, streams growing growth and filtration of water into the soil. To that, the flow of the flat dilyanka becomes swampy. At the Uzbek winter temperatures, there are trochas more, and lіtn_ - trochas lower, lower in the inner regions of the mainland. Vlіtku, if vologue seems to be above cold water anyway sea ice Fogs are often found on the arctic uzberezhzhi.
Rіchna suma fallen asleep I don’t perevychay 380 mm. A large part of the vipadє at the viglyadі I will board, or I will go down, when passing cyclones. On the Uzbeks, the main mass of fallout can be brought by winter cyclones. Even with low temperatures and clear weather of the cold season, typical for a large part of regions with subpolar climate, unfriendly for significant snow accumulation.
subarctic climate vidomy is also called "taiga climat" (according to the more important type of growth - coniferous forests). The whole climatic belt is hunted around the latitude of the Pivnichnaya pivkuly - the pivnichny regions of the Pivnichnaya America and Eurasia, roztasvani without middle on the second day of the subpolar climatic belt. Here there is a rare seasonal climatic vision through the position of a climatic belt in high latitudes near the inner parts of the continent. The winter is protracted and the edge is colder, and it’s more so, the days are shorter. Summer is shorter and cooler on newer days. The tax period with negative temperatures is even trivial, and during an hour the temperature can be changed to + 32 С. characteristic for the coastal territories, for example, from the Old Alaska or from the Old Scandinavia.
On the larger part of the climatic belt, the drop is less than 500 mm, and the number is maximal on the eastern Uzbek banks and is minimal on the inner part of Siberia. There is a little bit of charge for the weather, when there is a fall with small cyclones. Let’s call it big, moreover, the boards go mainly when passing atmospheric fronts. On the Uzbeks, fogs are often thunderous and harsh. In severe frost over the snow cover, the fog hangs.
Vologiy continental climate with a short flow characteristic for the great swamp of the surrounding latitudes of the Pivnichnoe Pivkuli. The Pivnichniy American Wonder stretches through the fringes in Central Canada to the Uzbeks Atlantic Ocean, And in Eurasia I hunt for a large part Skhidnoi Europe and deyaki districts and Central Siberia. The same type of climat is promoted in Japanese about. Hokkaido and at the Distant Descent. The main climatic features of these districts begin with overwhelming backward transfer and frequent passage of atmospheric fronts. In suvor winter mid-temperature temperatures can drop to -18 C. It is shorter and cooler, frost-free period is less than 150 days. The temperature range is not very large, as in the minds of the subarctic climate. In Moscow, the average temperature is -9 ° C, lime - + 18 ° C. Silskoy government represent spring frosts. In the coastal provinces of Canada, in the New England and on the island. Hokkaido is warm in winter, lower in the inner continental regions, so yak skidnі vіtri an hour to bring more warmth of the ocean.
The usual number of fallen falls is less than 500 mm at the inner parts of the continents up to 1000 mm on the Uzbek banks. On a large part of the area, it falls over and over again, often with thunderstorms. Winter falls, mainly in the snow, tied from the fronts of the cyclones. They are often noticed during the cold front.
Vologiy Continental Climate with Dovgy Lit. Temperatures during the summer season increase during the day in areas of the continental climate. This type of climate is manifested in the world latitudinal belt of Pivnichnaya America from the western part of the Great Plains to the Atlantic Uzbek coast, and in Pivdenno-Shidniy Europe - in the lower reaches of the Danube. Some climatic minds of turns are also in pivnichno-skidny China and central Japan. Here, too, the old transfer is overridden. The average temperature of the most warm month is + 22 С (the lower temperature can change + 38 С), lіtnі nights are warm. Winter is not so cold, as in areas of the continental climate with a short flow, even the temperature sometimes drops below 0 ° C. The usual temperature range starts to rise to 28 ° C, like, for example, in Peoria (Illinois, USA), the middle temperature at least -4 ° C, and lime - + 24 ° C. On the Uzbek coast, the temperature range changes.
Most often in the minds of a vologic continental climate with an increase in lithium vipadє from 500 to 1100 mm fallen in rіk. There is a great number of falloffs to bring lithium thunderstorms to anger during the growing season. The collection of boards and snowfalls in the main tied with the passed cyclones and the fronts tied with them.
Sea Climate of Pomirniy Latitudes the authorities of the western Uzbeks of the continent, the first for everything, of the ancient-western Europe, the central part of the Pacific Uzbek of the Indian America, the winter of Chile, the new world of Australia and New Zealand. At the turn of the day, the temperature will help you to warm up the winds through the backs of the ocean. Winter meats due to the average temperatures of the most cold month is 0 ° C, but if the Uzbeks can reach the streams of the Arctic twilight, it will be frosty. Let it warm as a whole; at the intrusion of a continental drink during the day, the temperature can for a short hour rise to + 38 С. For example, in Paris, the average temperature is + 3 С, lime - + 18 С.
In areas with a sea climate, the middle of the river, the amount of fallen falls from 500 to 2500 mm. Some of the women who were born seized the coastal mountains. In the bagatokh districts, they fall off to the end of the day, reaching out to the rock, the vignettes become pivnichno-zhidne Pacific Uzbeks of the United States in the middle of winter. Cyclones, which collapse from the oceans, bring abundant fall on the western continent outskirts. The tax, as a rule, is trimmed in bad weather with weak boards and short-hour snowfalls. On the Uzbeks, there are great fogs, especially during the fall.
Vologiy subtropic climate characteristic of shidnykh uzberez continents on private and on weekdays from paths. The main areas of expansion are the United States of America, the United States of America, the United States of America, the United States of America, the United States of America and the United States of America, the United States of America and the United States of America, the United States of America and the United States of America and the United States of America, Brazil lito u in the subtropics trivial and hot, with the same temperatures as in the paths. The average temperature of the warmest month is + 27C, and the maximum is + 38C. Winter meats, with average monthly temperatures of 0C, a little bitter frost, make a bitter infusion on the plantation of vegetables and citrus fruits.
In the middle subtropics of the middle of the day, the fall falls from 750 to 2000 mm; The collection of boards and snowfalls is carried by the head rank by cyclones. A bit of fall off is mainly caused by thunderstorms, tied with the possible influx of warm and natural oceanic food, characteristic of the monsoon circulation of the world. Hurricanes (or typhoons) are manifested in the end of the summer and the fall, especially in the Pivnichniy Pivkul.
Subtropical climate with dry lith typical for the backward Uzbek continents for winter and weekdays from paths. In Pivdenniy Europe and Pivnichniy Afritsa, such climatic minds are characteristic of the Uzbeks of the Sered-land Sea, which served as a drive for naming the climates also in the Middle-Seas. The same classroom is in the Pivdennii California, the central regions of Chile, in the extreme Peasants of Africa and in a number of districts in the Pivdennii Australia. In all cikh regions there is no summer and no winter. Yak and in vologic subtropics, it will be freezing cold. In the inner regions, the temperature is high, but not on the Uzbek banks, and often also, like in tropical heistlands. In general, the weather is clear. Vlіtku on uzberezhzhih, bіlya yak pass ocean currents, There is a lot of fog. For example, in San Francisco it is chilly and foggy, and the warmest month is spring.
The maximum loss of dressings from the passage of cyclones is charged, if the back-to-back streams change right up to the adequate level. The inflow of anticyclones and downturns flowing through the oceans add to the dryness of the summer season. The average number of falloffs in the minds of a subtropical climate range from 380 to 900 mm and reach the maximum values on Uzbeks and grains of weight. A little bit of falloff does not grow out for normal tree growth, and therefore a specific type of green chagarnikova growth develops there, such as maquis, chaparral, mali, macchiya and Finbosh.
Forward to the Pastel of the Around Latitudes(Synonym - steppe climate) characteristic of the most important for inland regions, from far from the oceans - dzherel vologi - and growing in the boardwalk of high mountains. The main districts with the seven-year climates are the municipalities and the Great Rivnini of the Great America and the steppe of Central Eurasia. Specterly summer and cold winter amumbled with an inland camp in the latitudes. Take one winter month, the average temperature is below 0 С, and the average temperature of the warmest summer month perevischuє + 21 C. The temperature regime and the triviality of frost-free period fluctuates frequently in fallowness from latitude.
The term "semicarid" is used to characterize the whole climate, that is, it’s dry mensh, but not very dry. The middle rychna sum of fallen leaves is less than 500 mm, ale more than 250 mm. Oscillations for the development of steppe height in the minds of higher temperatures, a larger number of fall is needed, latitude-geographic and variable position of the place to start the climate change. For a semi-detached climate, there are no out-of-the-box regularities of the growth of the fallen asleep. For example, in areas where there are subtropics with a dry flow, the maximum fall off is meant, while in areas that are close to the areas of the continental climate, the boards fall into the main flow. The cyclones of the surrounding latitudes bring a greater portion of winter fall, which often occurs at the sight of the snow, and can be supressed by strong winds. Lіtnі menace not hail hail. The number of fallen goods varies greatly from rock to rock.
Arid klimat of the littoral latitudes lured by the head rank of the Central Asian hedges, and at the entrance of the United States - deprived of small dilyankas near the middles. Temperatures are also, as in areas with seven-sided climates, protesting here is not enough for the closure of a closed natural dewline cover and mid-range sumi does not outweigh 250 mm. Yak and in the seven-year climatic minds, the number of fallen goods, which is the beginning of the aridity, lie under the thermal regime.
For the low latitude in the main typical for the outskirts of tropical kestrels (for example, the Sahari and the kestrel of central Australia), de lower streams of twilight in the subtropical zones of a high vice vyklyuyut vyadannya fallen. From the semicarid climate of the surrounding latitudes, the climates appear in an even hotter summer and warm winter. The average monthly temperature is 0 ° C, if there is a charge of frost, especially in areas that are the most distant of all types and temperatures at high altitudes. A number of fallen leaves, necessary for the development of wintry natural grassy vegetation, here is more, lower in the middle latitudes. At the equatorial smoothie boards, go to the main flow, only on the winter (winter and winter) outskirts, the kestrels have a maximum fall in the winter. Falling away from the big one, thunderous storms fall near the viewers, and cyclones bring the boards up.
Arid climate of low latitudes. There is a hot dry climate of tropical heaths, where the bridle of the Pivnichny and the Old Paths can be stretched, and there is a large part of the rock under the inflow of subtropical anticyclones. You can only know about the weather in the summer season on the Uzbek banks, where cold ocean currents are washed away, or in the mountains. On the plains of the middle summer temperatures, it is easy to twist + 32 ° C, in the winter you grow up to + 10 ° C.
On a large part of the climatic area, the middle of the village does not fall over 125 mm. Boo, so, at the meteorological stations, there are no rocky spills in the past. In the middle of the rychna sum, the fall can be up to 380 mm, and it’s still worth it for the development of empty space. The light falls off in the form of non-trivial strong thunderstorm boards, the water is brightly glistening, and the stormy floods are fierce. The most arid regions and the growth of the western shores of America and Africa, de cold ocean currents overshoot the shape of the gloom and fall. There are often fogs on the cikh Uzbeks, which pretends to be a condensation vologue in the wind over the larger cold surface of the ocean.
Winter-vological tropical climate. Areas with such a climate of growth in tropical sub-latitudinal belts, for a few degrees in the past and in the past. Tsei klimat is also called a monsoon tropical, as it is used for transporting in quiet parts of Pivdennoy Asia, as there is a lot of monsoons. The Іnshi districts with such a climate are the paths of Central and Eastern America, Africa and Pivnichnoy Australia. Average summer temperatures rise approx. + 27 ° C, and winters - approx. + 21 С. Samiy is a hot month, as a rule, before the summer season of boards.
Middle rychni sumi fall off from 750 to 2000 mm. Throughout the summer boarding season, the initial inflow into the climate is to rob the inner zone of convergence. There are often menaces here, sometimes during a trivial hour, to get a bit of a fright from the lingering planks. Winter is dry, so there are subtropical anticyclones in the whole season. In some areas, the boards do not vipadayut with a stretch of two or three winter months... In the Pivdenniy Asia, the season has a lot of garbage, which can be brought to the Indian Ocean And as a result, Asian continental dry masses are expanding.
Vologiy tropical climate, abo klimat vologikh tropical forests, Extensions in equatorial latitudes in the Amazon basins in Pivdenniy Americaі Congo in Africa, on the Peninsula of Malacca and on the islands of Pivdenno-Shіdnoi Asia. On the paths of the middle, the temperature of any month is not less than + 17 С, the temperature of the middle month is approx. + 26 C. Yak in the winter paths, through the high noon Sontsya's standing over the horizon and the same triviality of the day, the whole season of the temperature is low. As a matter of fact, the coldness and the thick, high-lane curvature overshoot the coldness and the maximum daytime temperatures are lower than + 37 ° C, higher low, lower in higher latitudes.
The average number of fall off along the paths varies from 1500 to 2500 mm; Fall off in the main link with the internal zone of convergence, as trochas grow more often. Seasonal changes of the central zone for winter and summer in some areas to produce up to two maximum fallen fall in the rock, broken by more dry periods. Today, a thousand thunderstorms will pass over the paths. At the intervals between them, the sun shines in power.
Climati Visokogir'ya. In high-rise districts, there is a great deal of versatility climatic minds it is summarized by latitudinal-geographic positions, orographic barriers, and a different exposition of seizures on the way to Sontsya and in the inconsistent wind flows. To navigate the ekvatori in the mountains there are snowfields-migrations. The lower boundary of the winter snow descends to the poles, reaching the sea level in the polar regions. Like the first and second cordon of the upper thermal zones, it decreases in the world closer to the higher latitudes. Navitryans grabbed the mountain ridges to recover more fallen. On girskih shilah, vidkritikh for the intrusion of a cold fever, it is possible to lower the temperature. In general, the high-altitude climate is characterized by a higher low temperature, a higher temperature, a higher drop rate and a higher folding wind mode, lower for a higher-latitude garden. character seasonal changes temperatures and drops in high mountains are the same as on adjacent rivers.
On a large part of the territory of Ukraine, the climate is similarly continental, with clearly varying seasons, and it is impossible to change the climate on the birch tree to subtropical. In the early and remote regions of the land, there are klimat m'yakshe, now in the winter and early ones. At the winter of Ukraine, the average temperature of the coldest month, today, becomes -7 degrees; in the central regions the won increases to -5, and in Crima, in the fallowing area, the growth changes from -0.5 to +4. During the winter period, mid-low temperatures from winter to weekday change from -9 to +1, mid-day - from -3 to +6. Summer in Ukraine is warm, with an average temperature of linden +18: 20 degrees, and in Crima - +22 degrees. In deyakі rocky, the thermometer can be increased up to +32. The average low temperature of lime in the greater part of Ukraine becomes +13 degrees, the middle day - +23 degrees. Crimu's indicators are generally equal to +20 and +26. Lose the distribution on the territory of the country even more unevenly. The greatest number of vipads in the mountainous regions. Near the Krimskie Mountains, beyond the rik of vipada, it is close to 1100 mm, in the Carpathians, the number of fallen falls reaches 1400 - 1600 mm. Naybіlsh are dry є in the winter-skidny regions of Ukraine, here the number of fallen leaves does not change 400 mm, but in the vicinity of the rocks there is dry land. On the screen in the middle, the size of the range is 600 - 700 mm. In the months of the fall, it’s okay to finish it, but in large districts (krim Crimea), you are encouraged to do it in lіtnіy period... Most of the planks є worm and linden, with a stretch of about 100 mm at the entrance, 50 mm in Crima and 60 - 80 mm on the screen of the territory. Most dry months in the whole territory of Ukraine є birch and zhovten, if the width is 30 - 40 mm.