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1 érosion éolienne
ветряная эрозия
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
wind erosion
The breakdown of solid rock into smaller particles and its removal by wind. It may occur on any soil whose surface is dry, unprotected by vegetation (to bind it at root level and shelter the surface) and consists of light particles. The mechanisms include straightforward picking up of dust and soil particles by the airflow and the dislodging or abrasion of surface material by the impact of particles already airborne. (Source: ALL)
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Франко-русский словарь нормативно-технической терминологии > érosion éolienne
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2 interaction air/eau
- взаимодействие "воздух-вода"
взаимодействие "воздух-вода"
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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. (Source: WATER / CEIS)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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- interaction air/eau
Франко-русский словарь нормативно-технической терминологии > interaction air/eau
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3 végétalisation
восстановление растительного покрова
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
revegetation
Planting of new trees and, particularly, of native plants in disturbed sites where the vegetation cover has been destroyed, to stabilize the land surface from wind and water erosion and to reclame the land for other uses. Revegetation practices are employed in mined lands, roadsides, parks, wetlands, utility corridors, riparian areas, etc. (Source: REVEGa / CORBIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Франко-русский словарь нормативно-технической терминологии > végétalisation
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4 processus géologique
геологический процесс
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
geological process
Dynamic actions or events that occur at the Earth's surface due to application of natural forces resulting from gravity, temperature changes, freezing and thawing, chemical reactions, seismic shaking, and the agencies of wind and moving water, ice and snow. Where and when a force exceeds the strength of the earth material, the material is changed by deformation, translocation, or chemical reactions. (Source: DUNSTE)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Франко-русский словарь нормативно-технической терминологии > processus géologique
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5 dune de sable
песчаная дюна
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
sand dune
An accumulation of loose sand heaped up by the wind, commonly found along low-lying seashores above high-tide level, more rarely on the border of large lakes or river valleys, as well as in various desert regions, where there is abundant dry surface sand during some part of the year. (Source: BJGEO)
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Франко-русский словарь нормативно-технической терминологии > dune de sable
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6 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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