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101 potentiel du sol par rapport à la terre
напряжение на поверхности земли
Напряжение между рассматриваемой точкой на поверхности Земли и относительной землей.
[ ГОСТ Р МЭК 60050-195-2005]
[ ГОСТ Р МЭК 60050-826-2009]EN
earth-surface voltage (to earth)
ground-surface voltage (to ground) (US)
voltage between a specified point on the Earth's surface and reference earth
[IEV number 195-05-08]FR
potentiel du sol par rapport à la terre
tension entre un point spécifié à la surface de la Terre et la terre de référence
[IEV number 195-05-08]Тематики
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DE
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Франко-русский словарь нормативно-технической терминологии > potentiel du sol par rapport à la terre
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102 relief
рельеф земли
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
relief (land)
The physical shape, configuration or general unevenness of a part of the Earth's surface, considered with reference to variation of height and slope or to irregularities of the land surface; the elevation or difference in elevation, considered collectively, of a land surface. (Source: BJGEO)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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форма земной поверхности
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
landform
Any physical, recognizable form or feature of the Earth's surface, having a characteristic shape and produced by natural causes; it includes major forms such as plane, plateau and mountain, and minor forms such as hill, valley, slope, esker, and dune. Taken together the landforms make up the surface configuration of the Earth's. (Source: BJGEO)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Франко-русский словарь нормативно-технической терминологии > relief
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103 Erdoberflächenpotential
напряжение на поверхности земли
Напряжение между рассматриваемой точкой на поверхности Земли и относительной землей.
[ ГОСТ Р МЭК 60050-195-2005]
[ ГОСТ Р МЭК 60050-826-2009]EN
earth-surface voltage (to earth)
ground-surface voltage (to ground) (US)
voltage between a specified point on the Earth's surface and reference earth
[IEV number 195-05-08]FR
potentiel du sol par rapport à la terre
tension entre un point spécifié à la surface de la Terre et la terre de référence
[IEV number 195-05-08]Тематики
EN
DE
FR
Немецко-русский словарь нормативно-технической терминологии > Erdoberflächenpotential
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104 напряжение на поверхности земли
напряжение на поверхности земли
Напряжение между рассматриваемой точкой на поверхности Земли и относительной землей.
[ ГОСТ Р МЭК 60050-195-2005]
[ ГОСТ Р МЭК 60050-826-2009]EN
earth-surface voltage (to earth)
ground-surface voltage (to ground) (US)
voltage between a specified point on the Earth's surface and reference earth
[IEV number 195-05-08]FR
potentiel du sol par rapport à la terre
tension entre un point spécifié à la surface de la Terre et la terre de référence
[IEV number 195-05-08]Тематики
EN
DE
FR
Русско-французский словарь нормативно-технической терминологии > напряжение на поверхности земли
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105 Oberfläche
f surface; an / unter der Oberfläche auch fig. on / below the surface; ( wieder) an die Oberfläche steigen (re)surface* * *die Oberflächetop; face; surface* * *Ober|flä|chefsurface (auch fig); (TECH, MATH) surface area; (COMPUT) (user) interfacedas Buch bleibt an der Óberfläche (fig) — the book doesn't go very deep
grafische Óberfläche (Comput) — graphical (user) interface
* * *die1) (a surface especially the front surface: a rock face.) face2) (the outside part (of anything): Two-thirds of the earth's surface is covered with water; This road has a very uneven surface.) surface3) (the outward appearance of, or first impression made by, a person or thing: On the surface he seems cold and unfriendly, but he's really a kind person.) surface4) (the upper surface: the table-top.) top* * *Ober·flä·che[ˈo:bɐflɛçə]f1. (äußere Fläche) surface2. (obere Fläche) surfaceauf [o an] der \Oberfläche on the surface* * *die surface; (Flächeninhalt) surface areadie Diskussion blieb zu sehr an der Oberfläche — (fig.) the discussion remained far too superficial
* * *Oberfläche f surface;an/unter der Oberfläche auch fig on/below the surface;* * *die surface; (Flächeninhalt) surface areadie Diskussion blieb zu sehr an der Oberfläche — (fig.) the discussion remained far too superficial
* * *(Mathematik) f.surface n. f.face n.surface n. -
106 движение воздуха
движение воздуха
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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DE
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Русско-немецкий словарь нормативно-технической терминологии > движение воздуха
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107 климат
климат
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
climate
The average weather condition in a region of the world. Many aspects of the Earth's geography affect the climate. Equatorial, or low, latitudes are hotter than the polar latitudes because of the angle at which the rays of sunlight arrive at the Earth's surface. The difference in temperature at the equator and at the poles has an influence on the global circulation of huge masses of air. Cool air at the poles sinks and spreads along the surface of the Earth towards the equator. Cool air forces its way under the lower density warmer air in the lower regions, pushing the lighter air up and toward the poles, where it will cool and descend. (Source: WRIGHT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Русско-немецкий словарь нормативно-технической терминологии > климат
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108 mouvement planétaire des masses d'air
движение воздуха
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
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Франко-русский словарь нормативно-технической терминологии > mouvement planétaire des masses d'air
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109 climat
климат
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
climate
The average weather condition in a region of the world. Many aspects of the Earth's geography affect the climate. Equatorial, or low, latitudes are hotter than the polar latitudes because of the angle at which the rays of sunlight arrive at the Earth's surface. The difference in temperature at the equator and at the poles has an influence on the global circulation of huge masses of air. Cool air at the poles sinks and spreads along the surface of the Earth towards the equator. Cool air forces its way under the lower density warmer air in the lower regions, pushing the lighter air up and toward the poles, where it will cool and descend. (Source: WRIGHT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Франко-русский словарь нормативно-технической терминологии > climat
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110 Luftbewegung
движение воздуха
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Немецко-русский словарь нормативно-технической терминологии > Luftbewegung
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111 Klima
климат
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
climate
The average weather condition in a region of the world. Many aspects of the Earth's geography affect the climate. Equatorial, or low, latitudes are hotter than the polar latitudes because of the angle at which the rays of sunlight arrive at the Earth's surface. The difference in temperature at the equator and at the poles has an influence on the global circulation of huge masses of air. Cool air at the poles sinks and spreads along the surface of the Earth towards the equator. Cool air forces its way under the lower density warmer air in the lower regions, pushing the lighter air up and toward the poles, where it will cool and descend. (Source: WRIGHT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Немецко-русский словарь нормативно-технической терминологии > Klima
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112 движение воздуха
движение воздуха
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Русско-английский словарь нормативно-технической терминологии > движение воздуха
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113 климат
климат
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
climate
The average weather condition in a region of the world. Many aspects of the Earth's geography affect the climate. Equatorial, or low, latitudes are hotter than the polar latitudes because of the angle at which the rays of sunlight arrive at the Earth's surface. The difference in temperature at the equator and at the poles has an influence on the global circulation of huge masses of air. Cool air at the poles sinks and spreads along the surface of the Earth towards the equator. Cool air forces its way under the lower density warmer air in the lower regions, pushing the lighter air up and toward the poles, where it will cool and descend. (Source: WRIGHT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Русско-английский словарь нормативно-технической терминологии > климат
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114 движение воздуха
движение воздуха
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
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Русско-французский словарь нормативно-технической терминологии > движение воздуха
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115 климат
климат
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
climate
The average weather condition in a region of the world. Many aspects of the Earth's geography affect the climate. Equatorial, or low, latitudes are hotter than the polar latitudes because of the angle at which the rays of sunlight arrive at the Earth's surface. The difference in temperature at the equator and at the poles has an influence on the global circulation of huge masses of air. Cool air at the poles sinks and spreads along the surface of the Earth towards the equator. Cool air forces its way under the lower density warmer air in the lower regions, pushing the lighter air up and toward the poles, where it will cool and descend. (Source: WRIGHT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Русско-французский словарь нормативно-технической терминологии > климат
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116 air movement
движение воздуха
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
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. (Source: WHIT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Англо-русский словарь нормативно-технической терминологии > air movement
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117 climate
климат
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[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]EN
climate
The average weather condition in a region of the world. Many aspects of the Earth's geography affect the climate. Equatorial, or low, latitudes are hotter than the polar latitudes because of the angle at which the rays of sunlight arrive at the Earth's surface. The difference in temperature at the equator and at the poles has an influence on the global circulation of huge masses of air. Cool air at the poles sinks and spreads along the surface of the Earth towards the equator. Cool air forces its way under the lower density warmer air in the lower regions, pushing the lighter air up and toward the poles, where it will cool and descend. (Source: WRIGHT)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
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Англо-русский словарь нормативно-технической терминологии > climate
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118 поверхность
жен. surface поддерживать на поверхности ≈ to buoy поднимать на поверхность ≈ to buoy плыть по поверхности ≈ to fleet совершенно гладкая поверхность ≈ dead-level опорная поверхность ≈ area of bearing рабочая поверхность ≈ work surface, effective area, worktop поверхность катания ≈ tread тех. отделывать поверхность ≈ to surface земная поверхность ≈ surface;
горн. grass гладкая поверхность ≈ smooth несущая поверхность ≈ plane авиац. внешняя поверхность ≈ outside поверхность раздела ≈ interface плоская поверхность ≈ level, flat, table зеркальная поверхность ≈ smooth/unruffled surface шершавая поверхность ≈ shaggy surface фокальная поверхность ≈ focal surface эквипотенциальная поверхность ≈ equipotential surface аэродинамическая поверхность ≈ aerofoil скользить по поверхности перен. ≈ to skim/scratch the surface of smth. всплывать на поверхность перен. ≈ to surface, to come out, to come to the surfaceБольшой англо-русский и русско-английский словарь > поверхность
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119 радиоволна
* * *радиоволна́ ж.
radio waveрадиоволна́ испы́тывает дифра́кцию — the radio wave is diffractedрадиоволна́ огиба́ет земну́ю пове́рхность — the radio wave bends around the Earth's surface, the radio wave follows the curvature of the globeрадиоволна́ распространя́ется как, напр. тропосфе́рная — the radio wave is propagated by, e. g., the tropospheric mode [as a tropospheric wave]атмосфе́рная радиоволна́ — atmospheric radio waveземна́я радиоволна́ — ground radio waveземна́я радиоволна́ распространя́ется вблизи́ от пове́рхности Земли́ — the ground radio wave travels along the Earth's surfaceпове́рхностная радиоволна́ — surface radio waveпростра́нственная радиоволна́ — ( прямая и земная) space radio wave; ( отражённая от ионосферы) sky radio waveпряма́я радиоволна́ — direct radio waveпряма́я радиоволна́ распространя́ется по прямолине́йным траекто́риям — the direct radio wave is propagated along the direct ray path, the direct radio wave is propagated in straight linesтропосфе́рная радиоволна́ — tropospheric radio wave* * * -
120 maanpinta
yks.nom. maanpinta; yks.gen. maanpinnan; yks.part. maanpintaa; yks.ill. maanpintaan; mon.gen. maanpintojen maanpintain; mon.part. maanpintoja; mon.ill. maanpintoihinground (noun)surface of the earth (noun)* * *• surface of the earth• earth's surface• ground
См. также в других словарях:
Water masses at the Earth's surface — ▪ Table Water masses at the Earth s surface reservoir volume (in millions of cubic kilometres) percent of total oceans 1,370.0 97.25 ice caps and glaciers 29.0 2.05 deep groundwater* (750–4,000 metres) 5.3 0.38 shallow groundwater (less than 750… … Universalium
Earth's surface — noun the outermost level of the land or sea (Freq. 1) earthquakes originate far below the surface three quarters of the Earth s surface is covered by water • Syn: ↑surface • Derivationally related forms: ↑surficial (f … Useful english dictionary
The Earth is Enough — is the most well known novel by author, Harry Middleton. It was published in March 1995 by the Pruett Publishing Company.The book chronicles Middleton s young life growing up in the rural Ozark mountains. Reviews Annie DillardThis is a grand true … Wikipedia
Surface of the Earth (band) — Surface of the Earth is a band from New Zealand. They formed in the 1990s, and played an instrumental role in the free noise movement of the mid 1990s. They released material on labels such as Corpus Hermeticum and Fusetron. The band has… … Wikipedia
The Day the Earth Stood Still — For the remake, see The Day the Earth Stood Still (2008 film). For soundtracks, see The Day the Earth Stood Still (soundtrack). The Day the Earth Stood Still Colorized reprint of the 1951 poster … Wikipedia
The Earth Fighter Rayieza — Infobox VG title = The Earth Fighter Rayieza caption = developer = Enix publisher = Enix Nintendo (Famicom port) designer = Makoto Kuba Shintaro Majima Go Nagai Yukihiro Takahashi released = Enix releases vgrelease|JP=1985Famicom… … Wikipedia
bowels of the earth — the center of the earth, deep beneath the earth s surface … English contemporary dictionary
History of the Earth — For the history of modern humans, see History of the world. Geological time put in a diagram called a geological clock, showing the relative lengths of the eons of the Earth s history The history of the Earth describes the most important events… … Wikipedia
Clouds and the Earth's Radiant Energy System — Artist representation of CERES instruments scanning Earth in Rotating Azimuth Plane mode. Clouds and the Earth s Radiant Energy System (CERES) is on going[update] NASA climatological experiment from Earth … Wikipedia
Dipole model of the Earth's magnetic field — Plot showing field lines (which, in three dimensions would describe shells ) for L values 1.5, 2, 3, 4 and 5 using a dipole model of the Earth s magnetic field The dipole model of the Earth s magnetic field is a first order approximation of the… … Wikipedia
Poles of the earth — Pole Pole, n. [L. polus, Gr. ? a pivot or hinge on which anything turns, an axis, a pole; akin to ? to move: cf. F. p[^o]le.] 1. Either extremity of an axis of a sphere; especially, one of the extremities of the earth s axis; as, the north pole.… … The Collaborative International Dictionary of English