láncirányítás |
chain management (The administration, organization and planning for the flow of materials or merchandise through various stages of production and distribution, involving a network of vendors, suppliers, manufacturers, distributors, retailers and other trading partners) |
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láp |
moor (A tract of unenclosed waste ground, usually covered with heather, coarse grass, bracken, and moss) |
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láp |
marsh (An periodically inundated area of low ground having shrubs and trees, with or without the formation of peat) |
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láp |
bog (A commonly used term in Scotland and Ireland for a stretch waterlogged, spongy ground, chiefly composed of decaying vegetable matter, especially of rushes, cotton grass, and sphagnum moss) |
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láp |
fen (Waterlogged, spongy ground containing alkaline decaying vegetation, characterized by reeds, that may develop into peat. It sometimes occurs in the sinkholes of karst region) |
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léghólyag |
alveolus (A tiny, thin-walled, capillary-rich sac in the lungs where the exchange of oxygen and carbon dioxide takes place. Also called air sac) |
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légi biztonság |
air safety (Any measure, technique or design intended to reduce the risk of harm posed by either moving vehicles or projectiles above the earth's surface or pollutants to the earth's atmosphere) |
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légi forgalmi szabályozás |
air traffic regulation |
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légi közlekedés |
air traffic (Aircraft moving in flight or on airport runways) |
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légi közlekedési törvény |
air traffic law (International rules and conventions relating to air transportation) |
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légi szállítás |
air transportation (The use of aircraft, predominantly airplanes, to move passengers and cargo) |
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légifotó |
aerial photograph (An image of the ground surface made on a light-sensitive material and taken at a high altitude from an aircraft, spacecraft or rocket) |
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légifénykép |
aerial photography (No definition needed) |
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légkondicionálás |
air conditioning (A system or process for controlling the temperature and sometimes the humidity and purity of the air in a house, etc.) |
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légkör összetevő |
atmospheric component (The Earth's atmosphere consists by volume of nitrogen (79,1%), oxygen (20,9%), carbon dioxide (about 0,03%) and traces of the noble gases (argon, krypton, xenon, helium) plus water vapour, traces of ammonia, organic matter, ozone, various salts and suspended solid particles) |
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légkör összetétel |
atmospheric composition (The chemical abundance in the earth's atmosphere of its constituents including nitrogen, oxygen, argon, carbon dioxide, water vapour, ozone, neon, helium, krypton, methane, hydrogen and nitrous oxide) |
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légkörfizika |
atmospheric physics (The study of the physical phenomena of the atmosphere) |
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légköri aeroszol |
atmospheric aerosol (Particulate matter suspended in the air. The particulate matter may be in the form of dusts, fumes, or mist. Aerosols in the atmosphere are the form in which pollutants such as smoke are dispersed) |
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légköri folyamat |
atmospheric process (Atmospheric processes are distinguished in physical and chemical processes and both types may be operating simultaneously in complicated and interdependent ways. The physical processes of transport by atmospheric winds and the formation of clouds and precipitation strongly influence the patterns and rates of acidic deposition, while chemical reactions govern the forms of the compounds deposited) |
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légköri inverzió |
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) |
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