What affects the temperature of ocean water. Temperature and salinity of sea water
It has long been known that ocean waters cover most of the surface of our planet. They constitute a continuous shell of water, which accounts for more than 70% of the entire geographical plane. But few people thought that the properties of ocean waters are unique. They have a huge impact on climate conditions and economic activity of people.
Property 1. Temperature
Ocean waters can accumulate heat. (about 10 cm deep) retain a huge amount of heat. As the ocean cools, it warms the lower layers of the atmosphere, causing average temperature Earth air is +15 °C. If there were no oceans on our planet, the average temperature would barely reach -21 °C. It turns out that thanks to the ability of the World Ocean to accumulate heat, we have a comfortable and cozy planet.
The temperature properties of ocean waters change abruptly. The heated surface layer gradually mixes with deeper waters, resulting in a sharp temperature drop at a depth of several meters, and then a smooth decrease to the very bottom. The deep waters of the World Ocean have approximately the same temperature; measurements below three thousand meters usually show from +2 to 0 ° C.
As for surface waters, then their temperature depends on geographic latitude. The spherical shape of the planet determines the sun's rays to the surface. Closer to the equator, the sun gives off more heat than at the poles. For example, the properties of the oceanic waters of the Pacific Ocean directly depend on average temperature indicators. The surface layer has the highest average temperature, which is more than +19 °C. This cannot but affect the surrounding climate and underwater flora and fauna. Next comes the surface waters, which are warmed up to an average of 17.3 °C. Then the Atlantic, where this figure is 16.6 °C. And the lowest average temperatures are in the Arctic Ocean - approximately +1 °C.
Property 2. Salinity
What other properties of ocean waters are modern scientists studying? they are interested in the composition sea water. Ocean water - a cocktail of dozens chemical elements, and salts play an important role in it. The salinity of ocean waters is measured in ppm. It is indicated by the “‰” icon. Permille means thousandth of a number. It is estimated that a liter of ocean water has an average salinity of 35‰.
When studying the World Ocean, scientists have repeatedly wondered what the properties of ocean waters are. Are they the same everywhere in the ocean? It turns out that salinity, like the average temperature, is heterogeneous. The indicator is influenced by a number of factors:
- quantity atmospheric precipitation- rain and snow significantly reduce the overall salinity of the ocean;
- stock of large and small rivers- salinity of the oceans washing the continents with big amount deep rivers below;
- ice formation - this process increases salinity;
- melting of ice - this process reduces the salinity of water;
- evaporation of water from the surface of the ocean - salts do not evaporate along with the waters, and salinity increases.
It turns out that the different salinity of the oceans is explained by the temperature of surface waters and climatic conditions. The highest average salinity is found in the Atlantic Ocean. However, the saltiest point, the Red Sea, belongs to the Indian Sea. The Arctic Ocean has the lowest rate. These properties of the oceanic waters of the Arctic Ocean are most strongly felt near the confluence of the deep rivers of Siberia. Here the salinity does not exceed 10‰.
Interesting fact. The total amount of salt in the world's oceans
Scientists do not agree on how many chemical elements are dissolved in the waters of the oceans. Supposedly from 44 to 75 elements. But they calculated that in total there is an astronomical amount of salts dissolved in the World Ocean, approximately 49 quadrillion tons. If you evaporate and dry all this salt, it will cover the surface of the land with a layer of more than 150 m.
Property 3. Density
The concept of “density” has been studied for a long time. This is the ratio of the mass of matter, in our case the World Ocean, to the occupied volume. Knowledge of the density value is necessary, for example, to maintain the buoyancy of ships.
Both temperature and density are heterogeneous properties of ocean waters. The average value of the latter is 1.024 g/cm³. This indicator was measured at average temperatures and salt content. However, in different parts of the World Ocean, density varies depending on the depth of measurement, the temperature of the area and its salinity.
Let us consider, as an example, the properties of the oceanic waters of the Indian Ocean, and specifically the change in their density. This figure will be highest in the Suez and Persian Gulf. Here it reaches 1.03 g/cm³. In the warm and salty waters of the northwestern Indian Ocean, the figure drops to 1.024 g/cm³. And in the desalinated northeastern part of the ocean and in the Bay of Bengal, where there is a lot of precipitation, the figure is the lowest - approximately 1.018 g/cm³.
The density of fresh water is lower, which is why it floats in rivers and other fresh water Oemah is somewhat more complicated.
Properties 4 and 5. Transparency and color
If you fill a jar with sea water, it will seem transparent. However, as the thickness of the water layer increases, it acquires a bluish or greenish tint. The color change is due to the absorption and scattering of light. In addition, the color of ocean waters is affected by suspended matter of various compositions.
bluish color clean water- the result of weak absorption of the red part of the visible spectrum. When there is a high concentration of phytoplankton in ocean water, it becomes blue-green or green color. This occurs because phytoplankton absorbs the red part of the spectrum and reflects the green part.
The transparency of ocean water indirectly depends on the amount of suspended particles in it. In field conditions, transparency is determined using a Secchi disk. A flat disk, the diameter of which does not exceed 40 cm, is lowered into water. The depth at which it becomes invisible is taken as an indicator of transparency in that area.
Properties 6 and 7. Sound propagation and electrical conductivity
Sound waves can travel thousands of kilometers underwater. The average propagation speed is 1500 m/s. This figure for sea water is higher than for fresh water. The sound always deviates a little from the straight line.
It has more significant electrical conductivity than fresh water. The difference is 4000 times. This depends on the number of ions per unit volume of water.
1. What determines the salinity of ocean waters?
The world ocean, the main part of the hydrosphere, is a continuous shell of water globe. The waters of the World Ocean are heterogeneous in composition and differ in salinity, temperature, transparency and other characteristics.
The salinity of water in the ocean depends on the conditions of evaporation of water from the surface and the influx of fresh water from the land surface and from the " precipitation. Water evaporation occurs more intensely in equatorial and tropical latitudes and slows down in temperate and subpolar latitudes. If we compare the salinity of the northern and southern seas, we can establish that the water in southern seas more salty. The salinity of water in the oceans also varies depending on the geographical location, however, in the ocean the mixing of water occurs more intensely than in more closed seas, therefore the difference in the salinity of ocean water masses will not be too sharp, as in the seas. The most saline (more than 37% o) are the ocean waters in the tropics.
2. What are the differences in ocean water temperature?
The water temperature in the World Ocean also varies depending on geographic latitude. In tropical and equatorial latitudes, the water temperature can reach +30 °C and above; in the polar regions it drops to -2 °C. At lower temperatures, ocean water freezes. Seasonal changes in ocean temperature are more pronounced in temperate regions. climatic zone. The average annual temperature of the World Ocean is 3 °C higher than the average land temperature. This heat is transferred to land using atmospheric air masses.
3. In what areas of the ocean does ice form? How do they affect the nature of the Earth and human economic activity?
The waters of the World Ocean freeze in the Arctic, subarctic and partly in temperate latitudes. The resulting ice cover affects the climate of the continents and makes it difficult to use cheap sea transport in the north to transport goods.
4. What is called water mass? Name the main types of water masses. What water masses are found in the surface layer of the ocean?
You will find a definition of the concept of water masses in the textbook (9).
Water masses, by analogy with air masses, are named according to the geographical zone in which they formed. Each water mass (tropical, equatorial, arctic) has its own characteristic properties and differs from the others in salinity, temperature, transparency and other characteristics. Water masses vary not only depending on the geographic latitude of their formation, but also depending on their depth. Surface waters differ from deep and bottom waters. Deep and bottom waters are practically not affected by sunlight and heat. Their properties are more constant throughout the oceans, in contrast to surface pods, the properties of which depend on the amount of heat and light received. There is much more warm water on Earth than cold water. Residents of temperate latitudes spend their New Year holidays with great pleasure on the coasts of those seas and oceans where the water is warm and clean. Sunbathing under the hot sun, swimming in salty and warm water, people restore strength and improve their health.
1. What determines the salinity of ocean waters?
The world ocean, the main part of the hydrosphere, is a continuous water shell of the globe. The waters of the World Ocean are heterogeneous in composition and differ in salinity, temperature, transparency and other characteristics.
The salinity of water in the ocean depends on the conditions of evaporation of water from the surface and the influx of fresh water from the land surface and with atmospheric precipitation. Water evaporation occurs more intensely in equatorial and tropical latitudes and slows down in temperate and subpolar latitudes. If we compare the salinity of the northern and southern seas, we can establish that the water in the southern seas is saltier. The salinity of water in the oceans also varies depending on the geographical location, however, in the ocean the mixing of water occurs more intensely than in more closed seas, therefore the difference in the salinity of the ocean water masses will not be too sharp, as in seas. The most saline (more than 37% o) are the ocean waters in the tropics.
2. What are the differences in ocean water temperature?
The water temperature in the World Ocean also varies depending on geographic latitude. In tropical and equatorial latitudes, the water temperature can reach +30 °C and above; in the polar regions it drops to -2 °C. At lower temperatures, ocean water freezes. Seasonal changes in ocean water temperature are more pronounced in the temperate climate zone. The average annual temperature of the World Ocean is 3 °C higher than the average land temperature. This heat is transferred to land using air masses in the atmosphere.
3. In what areas of the ocean does ice form? How do they affect the nature of the Earth and human economic activity?
The waters of the World Ocean freeze in arctic, subarctic and partly in temperate latitudes. The resulting ice cover affects the climate of the continents and makes it difficult to use cheap sea transport in the north to transport goods.
4. What is called water mass? Name the main types of water masses. What water masses are found in the surface layer of the ocean? Material from the site
Water masses, by analogy with air masses, are named according to the geographical zone in which they were formed. Each water mass (tropical, equatorial, arctic) has its own characteristic properties and differs from the rest in salinity, temperature, transparency and other characteristics. Water masses differ not only depending on the geographic latitude of their formation, but also depending on their depth. Surface waters differ from deep and bottom waters. Deep and bottom waters are practically not affected by sunlight and heat. Their properties are more constant throughout the world's oceans, in contrast to surface waters, the properties of which depend on the amount of heat and light received. There is much more warm water on Earth than cold water. Residents of temperate latitudes spend their New Year holidays with great pleasure on the coasts of those seas and oceans where the water is warm and clean. Sunbathing under the hot sun, swimming in salty and warm water, people restore strength and improve their health.
Didn't find what you were looking for? Use the search
On this page there is material on the following topics:
- "The world's oceans are the main part of the hydrosphere" answers
- short message about the world's oceans
- what water masses are released in the surface layer of the ocean
- transparency of equatorial water masses
- report on the geography of the world's oceans
Instructions
The average salinity level of the World Ocean is 35 ppm - this is the figure most often cited in statistics. A little bit more exact value, without rounding: 34.73 ppm. In practice, this means that in every liter of theoretical ocean water, about 35 g of salt should be dissolved. In practice, this value varies quite a lot, since the World Ocean is so huge that the waters in it cannot quickly mix and form something homogeneous in terms of chemical properties space.
The salinity of ocean water depends on several factors. Firstly, it is determined by the percentage of water evaporating from the ocean and precipitation falling into it. If there is a lot of precipitation, the level of local salinity drops, and if there is no precipitation, but the water evaporates intensively, then the salinity increases. Therefore, in the tropics, in certain seasons, the salinity of water reaches record values for the planet. The largest part of the ocean is the Red Sea, its salinity is 43 ppm.
Moreover, even if the salt content on the surface of the sea or ocean fluctuates, usually these changes practically do not affect the deep layers of water. Surface vibrations rarely exceed 6 ppm. In some areas, the salinity of the water decreases due to the abundance of fresh rivers flowing into the sea.
The salinity of the Pacific and Altantic oceans is slightly higher than the rest: it is 34.87 ppm. Indian Ocean has a salinity of 34.58 ppm. The Arctic Ocean has the lowest salinity, and the reason for this is melting polar ice, which occurs especially intensely in the Southern Hemisphere. The currents of the Arctic Ocean also influence the Indian Ocean, which is why its salinity is lower than that of the Atlantic and Pacific Oceans.
The further from the poles, the higher the salinity of the ocean, for the same reasons. However, the saltiest latitudes are from 3 to 20 degrees in both directions from the equator, and not the equator itself. Sometimes these “stripes” are even said to be salinity belts. The reason for this distribution is that the equator is a zone of constant heavy tropical rainfall, which desalinizes the water.
Video on the topic
note
Not only the salinity changes, but also the temperature of the water in the World Ocean. Horizontally, the temperature changes from the equator to the poles, but there is also a vertical change in temperature: it decreases towards depth. The reason is that the sun is not able to penetrate the entire water column and heat the ocean waters to the very bottom. Water surface temperatures vary greatly. Near the equator it reaches +25-28 degrees Celsius, and near the North Pole it can drop to 0, and sometimes even a little lower.
The area of the World Ocean is approximately 360 million square meters. km. This is about 71% of the entire planet's territory.
10. Temperature in the ocean.
© Vladimir Kalanov,
"Knowledge is power".
You can often hear the expressions “warm sea” or “cold, icy sea.” If we keep in mind only the temperature of the water, it turns out that the difference between the warm and cold sea is completely insignificant and concerns only the upper, relatively thin layer of water. Therefore, the mentioned expressions can only be perceived as a literary image, as a familiar speech cliche.
The world's oceans as a whole are a colossal reservoir of cold water, on top of which, and even then not everywhere, there is a thin layer of slightly warmer water. Water warmer than 10 degrees makes up only about 8 percent of the total water reserves of the world's oceans. This warm layer on average reaches a thickness of no more than 100 meters. Below it, at great depths, the water temperature ranges from one to four degrees Celsius. 75% of ocean water has this temperature. In deep-sea trenches, as well as in the surface layers of the polar regions, the water has an even lower temperature.
The temperature regime of the ocean is exceptionally stable. If in on a global scale the absolute difference in air temperatures reaches 150°C, then the difference between the maximum and minimum surface temperature There is, on average, an order of magnitude less water in the ocean.
In absolute values, this difference in different areas of the World Ocean ranges from 4-5°C to 10-12°C during a year. For example, the temperature fluctuation of the surface waters of the Pacific Ocean in the area of the Hawaiian Islands during the year is no more than 4°C, and in the area south of the Aleutian Islands - 6-8°C. Only in shallow coastal areas of the seas of temperate climate zones can these fluctuations be greater. For example, off the northern coast of the Sea of Okhotsk, the difference in average surface water temperatures between the warmest and the warmest cold months year reaches 10-12°C.
Concerning daily fluctuations surface water temperature, then in the open sea they are only 0.2-0.4 degrees. Only in clear sunny weather in the warmest month of summer can they reach 2 degrees. Daily temperature fluctuations affect a very thin surface layer of ocean water.
Solar radiation warms the water in the ocean, even in the equatorial zone, to a very small depth (up to 8-10 meters). Into deeper layers thermal energy The sun penetrates only due to the mixing of water masses. The most active role in mixing sea water belongs to the wind. The depth of wind mixing of water is usually 30-40 m. At the equator, provided there is good wind mixing, the Sun warms the water to a depth of 80-100 m.
In the most restless ocean latitudes, the depth of thermal mixing is much greater. For example, in the South Pacific, in the strip of storms between the 50th and 60th parallels, the wind mixes water to depths of 50-65 meters, and south of the Hawaiian Islands - even to a depth of 100 meters.
The intensity of thermal mixing is especially high in areas of powerful ocean currents. For example, south of Australia, thermal mixing of water occurs to a depth of 400-500 m.
In this regard, we must clarify some terms used in oceanology.
Mixing, or vertical water exchange, comes in two types: frictional And convective . Frictional mixing occurs in a moving stream of water due to differences in the speed of its individual layers. This mixing of water occurs when exposed to wind or tide (low tide) in the sea. Convective (density) mixing occurs when, for some reason, the density of the overlying layer of sea water turns out to be higher than the density of the underlying layer. At such moments in the sea there is vertical water circulation . The most intense vertical circulation occurs in winter conditions.
The density of ocean water increases with depth. The normal increase in density with depth is called direct stratification of ocean waters . It also happens reverse density stratification , but it is observed as a short-term phenomenon in the ocean.
The temperature of surface water is most stable in the equatorial zone of the ocean. Here it is within 20-30°C. The sun in this zone brings approximately the same amount of heat at any time of the year, and the wind constantly mixes the water. Therefore, a constant water temperature is maintained around the clock. In the open ocean the most high temperatures surface water is observed in the zone from 5 to 10 degrees north latitude. In bays, water temperatures can be higher than in the open ocean. For example, in the Persian Gulf in summer the water warms up to 33°C.
The surface water temperature in the tropical zone is almost constant throughout the year. It never drops below 20°C, and in the equatorial zone it approaches 30 degrees. In shallow water near the shore during the day, the water can warm up to 35-40°C. But in the open sea the temperature is maintained with amazing constancy (26-28 degrees) around the clock.
In temperate zones, the temperature of surface waters is naturally lower than in near-equatorial zones, and the difference between summer and winter temperatures is already noticeable and reaches 9-10 degrees. For example, in Pacific Ocean in the area of 40 degrees north latitude, the average surface water temperature is about 10 degrees in February, and about 20 in August.
Sea water heats up as a result of its absorption of solar energy. It is known that water does not transmit the red rays of the solar spectrum well, and long-wave infrared rays, which carry the bulk of the thermal energy, penetrate only a few centimeters into the water. Therefore, heating of the deeper layers of the ocean occurs not due to the direct absorption of solar heat, but due to vertical movements of water masses. But even in the equatorial zone, where the sun's rays are directed almost at right angles to the surface of the ocean, and the wind actively mixes the water, it remains constantly cold deeper than 300 meters. There are almost no seasonal variations depths of the sea. In the tropics, under a layer of warm water there is a zone 300-400 meters thick, where the temperature quickly drops with depth. The area of rapid temperature drop is called thermocline. Here, every 10 meters of depth, the temperature drops by about 1 degree. IN next layer 1-1.5 km thick. the rate of temperature decline slows down sharply. At the lower boundary of this layer, the water temperature does not exceed 2-3°C. In deeper layers, the temperature drop continues, but occurs even more slowly. Layers of ocean water, starting from a depth of 1.2-1.5 km, no longer respond at all to changes in external temperatures. In the bottom layer of water, the temperature rises slightly, which is explained by the influence of the heat of the earth’s crust. The monstrous pressure existing at great depths also prevents a further drop in water temperature. Thus, the water of the polar regions, cooled at the surface, dropping to a depth of 5 km, where the pressure increases 500 times, will have a temperature 0.5 degrees higher than the original.
The circumpolar region, like equatorial zone, is a zone of stable surface water temperature. Here the sun's rays fall at an acute angle to the surface of the ocean, as if sliding above the surface. A significant part of them does not penetrate into the water, but is reflected from it and goes into outer space. In the polar regions, the temperature of surface waters in summer can rise to 10 degrees, and in winter drop to 4-0 or even minus 2 degrees. As is known, sea water can be in a liquid state even at negative temperatures, because she represents enough saturated solution salts, which reduces the freezing point of pure water by about 1.5 degrees.
The Weddell Sea off the coast of Antarctica is considered the coldest region of the world's oceans. Here the ocean water has the lowest temperature. The waters of the Southern Hemisphere as a whole are significantly colder than the waters Northern Hemisphere. This difference is explained by the warming effect of the continents, the area of which in the Southern Hemisphere of the Earth is significantly smaller. Therefore, the so-called thermal equator of the World Ocean, i.e. the line of highest surface water temperatures is shifted relative to the geographic equator to the north. The average annual surface temperature of the ocean at the thermal equator is about 28°C in open waters and about 32°C in closed seas. Such temperatures remain stable and constant for many years, centuries, millennia and probably millions of years.
Geographers and astronomers, taking as a basis the height of the Sun above the horizon, theoretically divided the Earth's surface using two tropics and two polar circles into five geometrically regular belts or climatic zones.
In the World Ocean, generally speaking, the same climatic zones are distinguished. But such a formal division is not always consistent with the interests of specific types of science and practice. For example, in oceanology, climatology, biology, as well as in practice Agriculture, zones established only on the basis of geographic latitude often do not coincide with real climatic zones, with the actual zonality of distribution of precipitation, plants, animals. For marine biologists, navigators, and fishermen, it is not the Arctic Circle itself that is important; they are primarily interested in the border of floating ice.
Climatic zones (belts) in the World Ocean.
Scientists from different specialties do not have a common opinion, for example, on the question of what is considered the tropical zone of the ocean, where it begins and where it ends. Some experts consider the tropical zone of the ocean only that belt north and south of the equator in which coral reefs can exist. Others believe that such a zone covers the distribution area sea turtles etc. Some scientists consider it necessary to distinguish special subtropical and subarctic zones.
Climatologists and weather forecasters, who in their work must take into account the influence of numerous natural factors - temperature, humidity, strength and direction of prevailing winds, amount of precipitation, proximity of the ocean, length of seasons, etc., divide the Earth into as many as 13 zones: one equatorial and two each of subequatorial, tropical, subtropical, temperate, subpolar and polar.
These examples show a completely normal situation in science, when each special discipline requires special initial, basic conditions for solving the problems it faces and obtaining specific results. The main thing that we must note in the issue of zonation of the Earth and the World Ocean is that, firstly, the latitudinal zonation of both land and ocean has little or no relation to temperature conditions the ocean depths and the physical and biological processes occurring there. Secondly, any zonal division of the Earth and the ocean is conditional and cannot be universal for all branches of science and practice.
The main source of data is ARGO buoys. The fields were obtained using optimal analysis.
Our website contains a map of surface temperatures of the World Ocean, which shows the water temperature at a specific point in the ocean at each this moment in real time. Information about the temperature of ocean water is transmitted to the weather service of many countries from several thousand ship and stationary weather stations, as well as numerous sensors - buoys that are installed at anchors or drifting in various areas of the World Ocean. This entire system was created by the combined efforts of dozens of countries around the world. The value of such a system is obvious: it is an important element of the World Weather Watch and, together with weather satellites, contributes to the production of data for global weather analyzes and forecasts. And everyone needs a reliable weather forecast: scientists, drivers of ships and aircraft, fishermen, tourists.
© Vladimir Kalanov,
"Knowledge is power"
Loading...
