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1 autorité de l'arbitre
Pouvoir dont dispose l'arbitre de veiller à l'application des Lois du Jeu pour le match qu'il est appelé à diriger, dès l'instant où il pénètre sur le terrain de jeu et jusqu'à ce qu'il le quitte.Power given to the referee to enforce the Laws of the Game in connection with the match for which he has been appointed, from the moment he enters the match venue until the time he leaves.Dictionnaire Français-Anglais (UEFA Football) > autorité de l'arbitre
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2 arbre
дерево
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
tree
Any large woody perennial plant with a distinct trunk giving rise to branches or leaves at some distance from the ground. (Source: CED)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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классификационное дерево
Совокупность классификационных цепей, имеющих общий подчиняющий класс.
[ГОСТ 7.74-96]Тематики
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Франко-русский словарь нормативно-технической терминологии > arbre
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3 foręt de feuillus
лиственный лес
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
deciduous forest
The temperate forests comprised of trees that seasonally shed their leaves, located in the east of the USA, in Western Europe from the Alps to Scandinavia, and in the eastern Asia. The hardwood of these forests have been exploited since the 16th century. The trees of deciduous forests usually produce nuts and winged seeds. (Source: WRIGHT)
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Франко-русский словарь нормативно-технической терминологии > foręt de feuillus
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4 déchet de jardin
растительные отходы сада
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
garden waste
Natural organic matter discarded from gardens and yards including leaves, grass clippings, prunings, brush and stumps. (Source: DMG)
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Франко-русский словарь нормативно-технической терминологии > déchet de jardin
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5 circulation maritime
циркуляция морской воды
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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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Франко-русский словарь нормативно-технической терминологии > circulation maritime
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