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1 взаимосвязь Земли и Солнца
взаимосвязь Земли и Солнца
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
Earth-Sun relationship
The Earth depends on the sun for its existence as a planet hospitable to life, and solar energy is the major factor determining the climate. Hence, conditions on the sun and conditions on Earth are inextricably linked. Although the sun's rays may appear unchanging, its radiation does vary. Many scientists suspect that sunspot activity has a greater influence on climatic change than variations attributed to the greenhouse effect. (Source: WRIGHT)
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Русско-французский словарь нормативно-технической терминологии > взаимосвязь Земли и Солнца
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2 космос (астрон.)
космос (астрон.)
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
space (interplanetary)
Space extending between the sun and the planets of the solar system. Interplanetary space is not empty, but contains dust, particles with an electric charge, and the magnetic field of the sun (also called the IMF, or Interplanetary Magnetic Field). (Source: CED / WINDOW)
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Русско-французский словарь нормативно-технической терминологии > космос (астрон.)
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3 циркуляция морской воды
циркуляция морской воды
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sea circulation
Large-scale horizontal water motion within an ocean. The way energy from the sun, stored in the sea, is transported around the world. The currents explain, for example, why the UK has ice-free ports in winter, while St. Petersburg, at the same latitude as the Shetland Islands, needs ice breakers. Evidence is growing that the world's ocean circulation was very different during the last ice age and has changed several times in the distant past, with dramatic effects on climate. The oceans are vital as storehouses, as they absorb more than half the sun's heat reaching the earth. This heat, which is primarily absorbed near the equator is carried around the world and released elsewhere, creating currents which last up to 1.000 years. As the Earth rotates and the wind acts upon the surface, currents carry warm tropical water to the cooler parts of the world. The strength and direction of the currents are affected by landmasses, bottlenecks through narrow straits, and even the shape of the sea-bed. When the warm water reaches polar regions its heat evaporates into the atmosphere, reducing its temperature and increasing its density. When sea-water freezes it leaves salt behind in the unfrozen water and this cold water sinks into the ocean and begins to flow back to the tropics. Eventually it is heated and begins the cycle all over again. (Source: MGH / WRIGHT)
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Русско-французский словарь нормативно-технической терминологии > циркуляция морской воды
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4 Сунь Цзы
vgener. Sun Tzu -
5 анодный блок магнетрона типа восходящее солнце
adjradio. anode de type rising-sunDictionnaire russe-français universel > анодный блок магнетрона типа восходящее солнце
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6 магнетрон типа восходящее солнце
nradio. (разнорезонаторный) magnétron "rising-sun", (разнорезонаторный) magnétron "soleil levant"Dictionnaire russe-français universel > магнетрон типа восходящее солнце
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7 разнорезонаторный анодный блок магнетрона
adjradio. anode de type rising-sunDictionnaire russe-français universel > разнорезонаторный анодный блок магнетрона
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8 атмосферная инверсия
атмосферная инверсия
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
atmospheric inversion
A temperature inversion in the atmosphere in which the temperature, instead of falling, increases with height above the ground. With the colder and heavier air below, there is no tendency to form upward currents and turbulence is suppressed. Inversions are often formed in the late afternoon when the radiation emitted from the ground exceeds that received from the sinking sun. Inversions are also caused by katabatic winds, that is cold winds flowing down the hillside into a valley, and by anticyclones. In inversion layers, both vertical and horizontal diffusion is inhibited and pollutants become trapped, sometimes for long periods. Low-level discharges of pollutants are more readily trapped by inversions than high level dischargers, hence the case for high stacks. Furthermore, high level discharges into an inversion tend to remain at a high level because of the absence of vertical mixing. (Source: GILP96)
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Русско-французский словарь нормативно-технической терминологии > атмосферная инверсия
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9 бриссоль
- brise–soleil
бриссоль
Постоянное солнцезащитное устройство в виде решётчатого козырька, устанавливаемого над проёмами с внешней стороны здания
[Терминологический словарь по строительству на 12 языках (ВНИИИС Госстроя СССР)]Тематики
- архитектура, основные понятия
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- brise–soleil
Русско-французский словарь нормативно-технической терминологии > бриссоль
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10 горный климат
горный климат
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
mountain climate
Very generally, the climate of relatively high elevations; mountain climates are distinguished by the departure of their characteristics from those of surrounding lowlands, and the one common basis for this distinction is that of atmospheric rarefaction; aside from this, great variety is introduced by differences in latitude, elevation, and exposure to the sun; thus, there exists no single, clearly defined, mountain climate. Also known as highland climate. (Source: MGH)
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Русско-французский словарь нормативно-технической терминологии > горный климат
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11 отопление на основе солнечной энергии
отопление на основе солнечной энергии
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
solar heating
A domestic or industrial heating system that makes direct use of solar energy. The simplest form consists of a collector through which a fluid is pumped. The circuit also contains some form of heat storage tank and an alternative energy source to provide energy when the sun is not shining. The collector usually consists of a black surface through which water is piped, the black surface being enclosed behind glass sheets to make use of the greenhouse effect. (Source: UVAROV)
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Русско-французский словарь нормативно-технической терминологии > отопление на основе солнечной энергии
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12 прилив
прилив
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
tide
The periodic rise and fall of the water resulting from gravitational interaction between the sun, moon and earth. In each lunar day of 24 hours and 49 minutes there are two high tides and two low tides. (Source: LANDY)
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Русско-французский словарь нормативно-технической терминологии > прилив
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13 продолжительность солнечного дня
продолжительность солнечного дня
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
duration of sunshine
Period of the day during which the sun is shining. (Source: RAMADE)
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Русско-французский словарь нормативно-технической терминологии > продолжительность солнечного дня
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14 сезон
сезон
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season
One of the four equal periods into which the year is divided by the equinoxes and solstices, resulting from the apparent movement of the sun north and south of the equator during the course of the earth's orbit around it. These periods (spring, summer, autumn and winter) have their characteristic weather conditions in different regions, and occur at opposite times of the year in the N and S hemispheres. (Source: CED)
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Русско-французский словарь нормативно-технической терминологии > сезон
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15 технология использования солнечной энергии
технология использования солнечной энергии
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
solar energy technology
Solar energy can be converted to useful work or heat by using a collector to absorb solar radiation, allowing much of the sun's radiant energy to be converted to heat. This heat can be used directly in residential, industrial, and agricultural operations; converted to mechanical or electrical power; or applied in chemical reactions for production of fuels and chemicals. (Source: PARCOR)
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Русско-французский словарь нормативно-технической терминологии > технология использования солнечной энергии
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16 тропики
тропики
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
tropics
The region of the earth's surface lying between two parallels of latitude on the earth, one 23а27' north of the equator and the other 23а27' south of the equator, representing the points farthest north and south at which the sun can shine directly overhead and constituting the boundaries of the Torrid Zone. (Source: AMHER)
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Русско-французский словарь нормативно-технической терминологии > тропики
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