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With the onset of summer, tourists hurry closer to the sea. Everyone missed heat, through the sun and sea water. But not everyone knows where to go, and what the sea choose. Today we will talk about the Azov Sea in June. The temperature of the water this month is normal, and as tourists' reviews say, you can swim and sunbathe. And this is so necessary to everyone who during the cold months managed to miss the sea and in a hurry to catch the missed. We have photos and video materials about the Azov Sea and about the resorts that stand on the shore of this chic and the warm sea. See and wait for the summer.

The Sea of \u200b\u200bAzov is big. It has children's camps on his shore, where since the beginning of the summer, full of full-term students who spend school holidays. On the seashore there are many resort cities, many of them are known throughout the world and foreigners come here. Perhaps the most famous is the city of Yeisk's resort. Here in summer period It comes to a million tourists from all over Russia. Beautiful city, good beaches and developed infrastructure. Rest in Yeisk is nice and comfortable.

Also tourists who prefer to rest in their homeland are known to those resorts like: Kirillovka and Novokonstantinovka. These are small resorts that only live in that they take tourists in summer time of the year. This is even more village, but in the beach season there are so many tourists that the villages turn into cities with a population under two hundred thousand people.

As we said, the Azov Sea is large, so there may be absolutely at different resorts miscellaneous weather and water temperature in the sea. Look further a consolidated table on which it is shown at which resorts of the sea is the most best water In June month:

Tourist reviews.
Since tourists are resting here since May and October, they left a lot of reviews about holidays in the Azov Sea. Let's read them.

Svetlana.
"Rested with girlfriends in Kirillovka. The sea was warm, the weather is sunny. They bathed almost every day, as there was a strong rain a couple of times. Water is not very clean. On the beach, the bottom was not quite sandy, but rather an clay passable with sand. Therefore, when you go to the sea, the legs are not very nice. And if the kids run here, then the whole torture from the bottom rises up, and the water is dirty. Send from the sea, and on you black spots! There are no special excursions, but you can take a walk. We walked along the sea, evenings here beautiful landscapes. generally. Plus, here is one - the warm sea, and the rest is not very. "

Danya.
"In June, there is no place to relax on the sea. The water is cool, and on the Sea of \u200b\u200bAzov is already bathed from mid-May. We rested in Berdyansk family. Recreation turned out to be different. I liked something, something is not very. Yes, the sea warm, the weather is sunny. The beach is normal, but the rest somehow is not very. There are no excursions, there is nowhere to go. We just walked the family in the evening around the city, went out in nature and all saw all.

The sea is clean here, although they said that there will be dirt. The wind and the waves did not bring any bottles or branches, nor another garbage. The beach is sandy, the entrance is gently and the children liked. But I repeat - they rested here only because of the sea. In July, the Black Sea will become Wood, then we will go to Sochi or in Anapa. "

What do you need to know the tourist?
The Sea of \u200b\u200bAzov does not have a direct exit to the ocean. At first it is connected to the Black Sea and this compound is called Kerch Strait. Now there is a bridge, which will connect mainland Russia with the Crimea. The bridge will ride cars and trains. Currently there is a ferry crossing, thanks to which you can get into the Crimea by sea. But the sea is often a storm, and the crossing can work on actual weather.

The Azov Sea is washes the coast of Russia, Ukraine and Crimea. Self famous cities Next to the sea: Yeisk, Taganrog and Rostov-on-Don. Rostov and the Azov Sea binds the Don River. And many tourists right along the river get to the sea on boats and boats. On the shore Azov Sea Thousands of large and small resort towns, and villages. Every year in healing beach season On the shores of the sea, about a million Russians is resting.

The climate in the Sea of \u200b\u200bAzov is significantly different from the Black Sea. It is more dry due to the fact that the main water area is located among the steppes. Therefore, the Azov Sea is often hotter, and water warms up much faster.

In warm years, water in the Azov Sea warms up to 22-23 ° C in late May. But for children up to seven-ten years she may seem cold. Therefore, if there is no task to order a child, or the baby is prone to bronchopile diseases, this month is better not to ride.

The water in the Azov Sea is not so salty, as in black, so it does not hurt the skin even the smallest.

In June, the water temperature in the Azov Sea reaches 24-26 ° C, depending on the weather. In the rainy years, it warms up slower. But in June, the first vegetables and fruits are beginning to ripen, which are very useful for children. In addition, it is not so hot, as in July-August, it is very easy to wear enough. Yes, and prices for real estate in June are lower than in the second half of summer. That is why this month of the family is often choosing to relax on the Azov Sea.

The only minus of the Azov Sea is monotonous coastal landscapes. There are no beautiful mountains, like on the Black Sea. But it is more likely to upset parents than children.

In July, water in Azov becomes very warm. It reaches 27-29 ° C. Such a temperature will love very little children. They will splash on the shallow water for a long time, not at all freezing. But in the second half of July, the coast is often too hot. Therefore, resting with chest or preschoolers, should not go to the beach from twelve days to four in the evening. Kids can get a heat blow, which is accompanied by very unpleasant symptoms - strong headache, temperature, nausea and vomiting. If you want to get out of the house, the child needs to wear a headdress and smear the skin sunscreen with a high UF factor.

The end of August - September is the best time to relax with children in the Sea of \u200b\u200bAzov

By the middle of August, the heat in the Azov Sea subsides, and the water remains all the same warm. Therefore, this time is optimal for relaxing with children on the coast. Already no suffocating heat, lightweight breeze blowing from the sea. The only minus of this period is in some places on the coast begins an active growth of algae. They are not dangerous, but to enter the sea filled with a variety of plants is not very nice. Children may not like the feeling of touching something to the skin in the water. But there are always beaches, clean from algae, so you can find out before leaving, in which area it is better to stop.

The Azov Sea attracts many holidaymakers in the summer season. Quite low-cost accommodation prices allow you to spend unforgettable days from water, and the relative proximity of the major cities of the European part of Russia makes it possible to get on the coast in a matter of hours.

You will need

  • - access to the Internet.

Instruction

To rest on the Sea of \u200b\u200bAzov, you can use the services of travel agencies or search for the appropriate option. In the first case, you need to visit the tourist firms of your city and get acquainted with the list of possible options. Having bought vouchers from the travel agency, you get rid of trouble buying tickets to travel to the place of recreation and search for housing on the coast. You will be available not only to rest, but also treatment, if you decide in the medical boarding house.

Many tourists prefer to go on. Nevertheless, in this case, too, you should take care in advance to overnight. You can in the private sector or in small holiday homes, you can via the Internet. To search for suitable options, type in the search engine "Rest in the Azov Sea" request, you will get a lot of suitable links.

The choice of rest sites on the Azov Sea is large enough, but it is better to rest in traditionally resort cities - for example, Yeisk, this is one of best places on the coast. Going to the Azov-SEA website, you can get acquainted with the list of hotels and boarding houses, find out the cost of living in them. From the European part of Russia, you can get to Yeisk by train, plane (to Rostov-on-Don or Krasnodar), bus. As a rule, many tourists first get to Rostov-on-Don, after which the bus station is driving in Yeisk.

You can relax and near Eisk or Taganrog, removing the room or the outhouse in a private house. This option will be the cheapest, agree on housing and time of arrival in advance via the Internet. You can relax on almost all the coast, but the beaches in this case may be unequipped. It is worth noting that in some places the Azov Sea is characterized by the presence of sufficiently strong currents, fishing networks can be in water. Therefore, it follows on equipped beaches. The advantage of the Azov Sea is that it is shallow, on many beaches you can go to a half-kilometer deep into the water, before you can enter the water in the waist. Smallness makes the beaches of the Azov Sea very comfortable and safe for children.

Sources:

  • Accommodation in the private sector S.P. Dolzhanskaya

The warm Azov Sea annually attracts thousands of tourists. One like bathing in shallow azure waters. Other soul on the sandy beaches, stretching for kilometers. Some are interested in the opportunity to improve and relax at the same time. The bulk of tourists from former Union The Sea of \u200b\u200bAzov attracts an opportunity to relax.

What is good holiday on the Azov coast

Multi-meter sandy shores stretched along the shore. Dreamers from the vertices of rocky cliffs will be able to watch the sunsets. There is a lesson for the soul and people leading active image Life, and those who came to combine rest with treatment.

Places for inexpensive holidays

Those who cannot afford to relax on expensive resorts choose places and sanatoriums cheaper. Where you can search for:

Arabat arrow. Fans of sunbathe will enjoy the rest on the Arabat Arrow. This is a sandy braid with a length of more than 100 km, dividing the Sea of \u200b\u200bAzov and Sivash Bay. The northern part of the arrow is built up with pensions and recreation databases price category. Among them, "Coral", Azovroyal, Arabesque and other holiday destinations. The beaches belonging to them are equipped with entertainment attractions. In coastal cafes, you can refresh yourself with chilled drinks or ice cream. For those who love to relax a "savage", it is preferable to stay on the southern part of the braid. There is a lesson for cyclists and for fishermen. Room cost in the private sector from 250 rubles.

Rest in Kerch. Due to the fact that the boarding houses in the city of Kerch are not so much, gathering there to rest, it is worth bothering about booking rooms in advance. Moreover, tourists are always enough here. People attract low prices and sights of the city. If desired, you can find. Kerch - the city is quite old. Therefore, there is both ancient monuments and fortresses and the catacombs of the military years. At moments of rest between excursions can be soaked on the sunny beach. The cheapest "apartments" will cost 250 rubles. per person.

Schelkino. West Kerch is located Schelkino. It is not so famous among the resorts of the Azov coast. Therefore, the price of housing here is more than acceptable. Moreover, after the closure of the Kazantypian festival of tourists, even in the season is not very much. But here there are secluded bays with beautiful beaches. Economy recreation will cost 200 rubles.

Taganrog. Rest in Taganrog can also be relatively inexpensive. This year, one-bedroom apartment will cost 600 rubles per day. Rooms in the private sector are surreated from 350 rubles.

Yeisk. On the azov coast Yeisk is considered the largest resort. The beaches of the city are equipped with a variety of attractions. For children, it will be interesting to visit Dolphinarium and Water Park. The cost of housing begins from 350 rubles for accommodation in the private sector.

The cheapest is the rest "". Not everyone agrees to such pleasure. But but the impressions after such much more than after civilized recreation. Choose you!

For the Azov Sea, a significant temporal and spatial variability of thermal conditions is characteristic. This feature is explained geographical position on southern periphery moderate breadth (on the border of freezing and non-freezing seas), shallow water of the Azov Sea, the cutting of its shores, relatively low salinity, etc. The interaction of all these factors determines the characteristics of the thermal conditions of the Azov Sea.

The main source of heat entered on the surface of the Azov Sea is solar radiation. Amount total solar radiationabsorbed by the Azov Sea for the year, on average for perennial period It is about 4,000 MJ / m2. Of this amount of heat, 2,200 MJ / M2 is spent on evaporation, about 1500 mJ / m2 for effective radiation and 300 mJ / m2 - on the contact heat exchange with the atmosphere. In detail, the heat balance of the Sea surface is highlighted on the climate on the page dedicated to the climate.

Water exchange with the Black Sea, as well as Stoke Don and Kuban, have a slight effect on the thermal regime of the Azov Sea. On average, during the year of water, the sea cooled the sea, and the Black Sea and Kuban - sweep it. A quantitative assessment of the thermal influence of the above factors related to the entire sea water area showed that for the year the coolant of the don is about 0.8 mJ / m2, and the elap of the Kuban and Black Sea waters 2.1 and 7.5 mJ / m2, respectively.

The prevailing role of radiation factors in the formation of the thermal regime of the Azov Sea is clearly traced in the zonal distribution of average annual perennial water temperature values \u200b\u200baccording to coast stations. They gradually increase from 11.2 ° C in the northern part of the Sea of \u200b\u200bAzov to 12.2-12.4 ° C in southern, i.e. approximately 0.5 ° C per 1 ° latitude. In the long-term temperature, the temperature is not tracked by distinct trends. Visually can be distinguished by a slightly reduced background of the temperature of the Azov Sea in the second half of the 20s - in the early 1930s and elevated - in the second half of the 60s - early 70s.

The calculation of perennial linear trends from the second half of the 40s to 1986 showed almost the absence of a trend in Berdyansk and a slight positive trend (0.03 ° C) in the capes. The latter circumstance may be due to some enhancement of the sweeping effect of the Black Sea Waters in cold part The year (October-February) in connection with the construction of the Tsimlyan hydrogen and an increase in the seizures of the river drain. This is to some extent confirmed by the calculations of perennial trends of the average monthly water temperature of the Azov Sea. From this data, it also follows that the trends of monthly values \u200b\u200bare much more than annual, but in general for the year with many years of averaging they are practically balanced.

Seasonal changes in the water temperature of the Azov Sea, as well as other shallow water, moderate latitudes, are expressed very sharply. The average monthly perennial values \u200b\u200bof the water temperature on the coastal hydrometeostations of the Sea of \u200b\u200bAzov testify to the following. Scope annual stroke In different parts of the Azov Sea, 23.2-24.7 ° C are, and somewhat decreases in the direction from the north to south, mainly due to the difference between the lowest temperatures in the northern and southern areas of the Sea of \u200b\u200bAzov.

SAMI low temperature It is celebrated in January-February, and the highest - in July. During the period of the greatest warming, the temperature of the water is almost aligned throughout the Azov Sea. Since the start of cooling (August), the water temperature in the southern part of the Sea is becoming higher than the temperature in the north and central regions. From April to July, the picture becomes back. This is probably due not only to the zonal location of observation points and with the morphological features of the districts, but also with the sweeping effect of the Black Sea water to the southern regions of the Azov Sea during the cooling period, and with the cooling effect of them during the intensive warming up of the shallow Azov Sea. In open deeper areas of the Azov Sea, the maximum water temperature is celebrated in August.

The most intensive warming of the water in the spring can be traced from April to May. According to coast stations, at different points it is rounded 7-9 ° C (average of 7.9 ° C), in the open areas of the Azov Sea - 6.5-9.5 ° C (average of 8.4 ° C). The most rapid cooling of the coast ranges from September to October 6-7 ° C (average 6.5 ° C), and in the open areas of the Azov Sea from October to November - by 5.5-7.7 ° C (average 6 , 7 ° C).

The seasonal course of water temperature on coastal stations is little different from such in shallow areas of the Azov Sea and is significantly different from the seasonal stroke in deep-sea areas. Maxims of curves are shifted by about a half months; During the heat accumulation period, the temperature of the water in shallow regions is higher than in deep-water, and during the cooling period - on the contrary.

Monthly water temperature values \u200b\u200bhave significantly greater variability than the average annual. Thus, according to the data of hydrometeostations, Capesoye and Berdyansk, standard deviations in different months vary from 0.7 to 2.2 ° C. Their greatest values \u200b\u200bare coming for April and October, i.e., during the most intense seasonal temperature changes. The smallest - for the summer and the beginning of autumn, when the pace of seasonal changes in the water temperature of the Azov Sea are underestimated, as well as for January-February in Berdyansk, where ice cover contributes to the stabilization of temperature. Data on the open areas of the Azov Sea is not enough to obtain quantitative characteristics of standard deviations of the monthly values \u200b\u200bof water temperature, but their qualitative analysis In general, confirms the results obtained according to coastal stations. A certain difference is that in the open sea in May deviations are somewhat larger than in April. The highest values \u200b\u200bof water temperature, according to urgent observations on coastal stations, are celebrated in July and in different parts of the Azov Sea are 29.3-32.8 ° C. The lowest (from -2.4 ° C in the genic to -0.5 ° C in Taganrog) can be observed in any of the winter months.

The spatial distribution of the temperature of the water along the water area of \u200b\u200bthe Sea of \u200b\u200bAzov due to its small sizes and small depths is characterized by weak contrast. According to coast stations, during the greatest cooling (February), the average water temperature in the surface layer of the sea varies from 0-0.2 ° C in the northern part of the sea to 1.0-1.2 ° C in South. Data for open areas of the Azov Sea in winter is very small. However, since the heat of water here is more than in coastal areas, it should be expected that the water temperature should be somewhat higher than the specified limits.

The temperature of the temperature during the greatest waters (July-August) is also distinguished by small contrast. The average values \u200b\u200bof water temperature in the surface layer of the Sea of \u200b\u200bAzov, both in coastal areas and in the open sea are changed within 24-25 ° C. In periods of heating and cooling, temperature contrasts increase. So, in April, water off the coast warms up to 8-11 ° C, and in the open areas of the sea it is below 7 ° C (in the central part of the Sea not exceeds 5.5 ° C). In October, the water temperature of almost the entire open water area is above 14 ° C, and in coastal areas, with the exception of the most southern, is below 14 ° C.

Spatial distribution of water temperature in the bottom layer of the Azov Sea in general features Similar to distribution in the surface layer. During the cooling period, the temperature background in the bottom layers, especially in the rotten areas, is slightly higher than that of the surface, and during the warming period - on the contrary, below. From the analysis of the existing database, it follows that already starting in October, the average temperature of the water in the bottom layers in most areas becomes higher than in the surface, with the exception of the deepest areas, where, due to the greater heat capacity of the aquatic masses, their cooling and surface, And the bottom happens more slowly than on the shallow water of the Sea of \u200b\u200bAzov.

In November, apparently, a weak unstable vertical temperature stratification is universally established, which is easily destroyed by wind-wave stirring and after reaching the vertical winter convection to the bottom is replaced by homothermia. Since March-April, the restructuring of the vertical thermal structure of the Sea of \u200b\u200bAzov is beginning. Weak stable stratification is formed in most areas of the sea, with the exception of the deepest areas of the central part of the sea and southwestern squares, where the temperature of the Sea of \u200b\u200bthe Sea of \u200b\u200bAzov Sea is below the bottom of the bottom layers due to the accumulation here in the spring under the action dominant winds Drifting ice. Sustainable thermal stratification on average is maintained from May to September. The vertical temperature stratification of the Sea of \u200b\u200bAzov is usually insignificant.

The calculation of the repeatability of temperature differences in the surface and bottom layers, produced according to observations on raid stations, showed that in the predominant number of cases, the difference does not exceed 1 ° C, but in some cases, with weak winds and significant salinity gradients, can reach 5-7 ° С.

Analysis of data on selective shallow squares of the Sea of \u200b\u200bAzov with the highest number of observations (depth 4-6 m) and deeper areas (depth 10-12 m) made it possible to identify some of the features of the vertical thermal structure in different parts of the Azov Sea. First, they confirm the weak temperature stratification of the sea. The average vertical gradients in both shallow and inland areas do not exceed 0.12-0.13 ° C / m. Secondly, there is a noticeable difference in the formation of a vertical thermal structure in areas with different depths in the navigation period. In shallow areas where the warming of water in the upper and bottom layers comes with a small shift in time, gradients gradually increase and achieve the greatest values In July, when the surface layer of water is warm as possible. With the beginning of its healing, gradients are reduced, and in October, stratification becomes unstable.

In the sublubricultural areas of the Azov Sea, where the warming of the bottom layers is slower with a significant lag behind the surface layer, the greatest gradients are set already in May-June, and then begin to decrease. In April and October, homothermia or weak instability are practically established.

Significant addition to the characteristic temperature mode The Sea of \u200b\u200bAzov is the analysis of internal and external heat management. Calculation of heat-rotation, in essence, is a continuation of the calculation of the thermal balance. The external heat rotation is taken to be taken to half the absolute values \u200b\u200bof the arrival and consumables of the heat balance of the Sea surface of the Azov Sea, and the internal heat rotation is the difference between the maximum and minimum heat generation of the aqueous mass.

In the shallow Azov Sea, which occupies a small territory, there are no sharply expressed climatic areas, but here two different zones of external heat management can be distinguished. One of them is located in the central part of the Sea of \u200b\u200bAzov, the other - in the coastal shallow area, including the Taganrog Bay. The difference in external heat management of these zones for the year is 800 mJ / m2. According to the cards of external heat management, its maximum values \u200b\u200bare located in the central, deep-sea part of the Sea of \u200b\u200bAzov, and the minimum - in shallow water, and the external heat conspicue is repeated in general terms. The dependence of the external heat management against the depths of the Azov Sea is closely related to annual amplitudes thermal balance. In areas where the thermal balance amplitude is higher, the external heat turnover is greater, the minimum heat management values \u200b\u200bare located in areas with a smaller amplitude of the thermal balance. The close relationship of the heat balance of the Azov Sea with depth is due to the fact that the active layer is the whole water stratum and with an increase in depth by reducing the consuming part of the heat balance (the lower water temperature in the deep sea and the associated smaller heat loss into evaporation) the outcome value of the balance increases. Maximum and minimum values \u200b\u200bof external heat management over the year are respectively about 1200 and 400 mJ / m2.

The distribution of internal heat management in general terms repeats the distribution of external, and the depth of the Azov Sea and has a crucial value. This is due to the fact that the extremal values \u200b\u200bof the heat generation in the small and shallow Sea of \u200b\u200bthe Sea are periods when the entire mass of water has almost the same temperature, and the heatpace is determined only by the depth of which the spatial distribution of internal heat management depends on which the spatial distribution of internal heat management depends on.

The inner heat protection is somewhat less external. For the entire sea, the difference between the total values \u200b\u200bof external and internal heat management over the year is 113 MJ / m2. Following the reasoning of V. S. Samoilenko on the influence of the ice cover on the discrepancy between the values \u200b\u200bof the external and internal heat consums of the Azov Sea, the difference of this can be attributed due to the loss of heat during the gland formation. The estimated calculations of the possible ice thickness (average by sea), which should be formed by the end of the winter on the formula proposed by it, and the comparison of the obtained value with the actual data allows you to consider this assumption is legitimate.

The processes of ice formation and ice sauna are reflected not only on the inner, but also on the external heat coot of the Azov Sea. During the period of ice saving and removal of ice in the southern regions of the Sea of \u200b\u200bAzov, some decrease in the water temperature and the associated reduction in the consumables of the thermal balance, thereby affecting the external heat being.


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Azov Sea - The smallest and the warmest sea. He is considered great place For recreation with children, since the depth does not exceed 15.5 meters, but the coast of the hollow and consists of sand.

Sea water temperature in Azov Sea for months

When is it better to go to rest?

Many tourists open the season already in mid-May, going to rest at the popular resorts of the Azov Sea: Primorsko-Akhtarsk, Yeisk, Berdyansk, Stunitsa Golubitskaya and Dolzhanskayaas well as villages Kuchugury and Perepal. These resorts are ideal for recreation.

Fresh air, good climate and the sea that warms up faster than anywhere else on the resorts, allow you to choose the Sea of \u200b\u200bAzov as wonderful place For recreation already at the beginning of June. The temperature in the afternoon this month is +25 degrees, and the water is heated to + 23 ° C.

Even better to rest on the Sea of \u200b\u200bAzov in JulySince quantity sunny days It is equal to 28-30, the water in the sea is constantly warm (+28 degrees).

July for those who seek a beach holiday or plans to travel to the sea with children.

Exactly the same weather keeps here in AugustBut, unlike July, the number of tourists is a little less. Nevertheless, this month is considered to be a paradise for those who do not want to leave the sea, since the water temperature is great - +25 degrees.

The Azov Sea, as well as the resorts located along the coast, are actively developing, every year attracting more "family tourists" every year. New entertainment appear here, and beach rest always on the top.

The temperature of the water in June in the Azov Sea - in detail

June - First summer month. The water temperature in the Azov Sea in June is gradually rising. So, if the average temperature of the water at the beginning is + 21 ° C, then the average water temperature at the end of the Sea of \u200b\u200bAzov is + 25 ° C.

average temperature The air in the Sea of \u200b\u200bAzov in June is 22 ° C.

Water temperature in June in the Sea of \u200b\u200bAzov in different years

Day with the coldest sea in the Sea of \u200b\u200bAzov in Was in 2018. The average temperature of the water in the sea was only + 18.9 ° C. It was June 4, 2018

Day with the most warm sea In the Sea of \u200b\u200bAzov in 2016. The average temperature of the water in the sea reached + 27.9 ° C. It was June 27, 2016

The temperature of the water for every day in June in the Sea of \u200b\u200bAzov in for different years Presented on the chart below:

The average water temperature in the sea in June in the Sea of \u200b\u200bAzov

The coldest sea in the Azov Sea was in 2017. The average temperature of water in the sea was only + 22.3 ° C.

The Western Sea in the Azov Sea happened in 2012. The average water temperature in the sea reached + 24 ° C.

The graph of average water temperature in the sea in the Sea of \u200b\u200bAzov in June for different years shows it:

Records for water temperature in the Sea of \u200b\u200bAzov in June

Watch out the water temperature in the sea in the Sea of \u200b\u200bAzov since 2010. And, I must say, records for water temperature happen very often. It is hardly every day on one or another resort water or the coldest, or the smallest. Below are the minimum and maximum temperatures Water in the sea in the Sea of \u200b\u200bAzov in June.