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| Terms for subject Environment (24829 entries) |
| Lösung von Umweltproblemen | environmental problem solving | |
| Lösung von Umweltproblemen | environmental problem solving (The activity of finding solutions for troublesome or perplexing situations involving ecological or natural resources) | |
| Lösungsmittel | solvent (Substance, generally a liquid, capable of dissolving another substance) | |
| Lösungsmittelextraktion | solvent extraction | |
| Lösungsmittelrichtlinie | solvent directive | |
| Lösungsmittelrückgewinnung | solvent recovery (Solvent recovery is a widely practised form of recycling where spent solvents are distilled and reused. However, the cheaper solvents are often incinerated or dumped in hazardous waste landfill sites) | |
| Lotsendienst | pilotage (The service provided by a pilot, one who controls the movements of a ship or aircraft by visual or electronic means) | |
| Lotsendienst | pilotage | |
| Löwenäffchen | golden lion tamarins | |
| Löwenäffchen | golden marmosets | |
| Löwenäffchen | golden tamarins | |
| Löwenäffchen | maned tamarins | |
| lückenlose Erfassung von der Entstehung bis zur Entsorgung | life cycle | |
| lückiger basophiler oder Kalk-Pionierrasen | rupiculous calcareous or basophilic grasslands | |
| Luft | ambient air | |
| Luft | air (A predominantly mechanical mixture of a variety of individual gases forming the earth's enveloping atmosphere) | |
| Luft-Wasser-Wechselwirkung | air-water interaction | |
| Luft-Wasser-Wechselwirkung | air-water interaction (The physical processes at the air-water interface: momentum, heat and mass transfer across the air-water interface, mixing of surface water by wind stress and wave breaking, directional wave spectra and wave forces on offshore structures. The air-water interaction is measured by the turbulence and gas exchanges resulting from the mixing of the water column by wind) | |
| luftbedürftige Bakterie | aerobic bacteria | |
| Luftbewegung | air movement (Air movements within the Earth's atmospheric circulation; also called planetary winds. Two main components are recognized: first, the latitudinal meridional component due to the Coriolis force (a deflecting motion or force discussed by G.G. de Coriolis in 1835. The rotation of the Earth causes a body moving across its surface to be deflected to the right in the N hemisphere and to the left in the S hemisphere); and secondly, the longitudinal component and the vertical movement, resulting largely from varying pressure distributions due to differential heating and cooling of the Earth's surface) |