world+surface

в розовом свете, в радужном свете — (to see smth.) through rose-colored glasses, to have a rosy outlook on smth., to look/seem rosy

чуть свет — at daybreak, at dawn, at first light, (get up) with the sun

в истинном свете — in its true light, in its true colors

в наилучшем свете — in the best possible light

представить что-л. в выгодном свете — to show smth. to the best advantage, place smth. in a good light

объехать вокруг света — to go round the world

предвещающий конец света — apocalyptic, apocalyptical

весь свет — the whole world

по всему свету — all over the world

страны света — the cardinal points, cardinals

белый свет — this/the world, the (whole) wide world, the wide, wide world, the great wild world

вывозить в свет — to bring smb. out (into) society

выезжать в свет — to come out (into society), to enter the social scene

выпуск в свет — publication, printing, issuance

выпускать в свет — to publish, to bring out

выход в свет — publication, printing

выходить в свет — to come out, to be published, to appear in print

извлекать на свет — to take/pull out, to dig up/out

производить на свет — to bring into the world, to give birth to smb.

больше всего на свете — above all/everything

выводить на свет божий — to unmask, to bring smth. out into the open, to blow the whistle on smth., to take the wraps the wraps off smth.

ни за что на свете! — not for the world!

ругаться на чем свет стоит — to swear like nothing on earth, swear like hell; curse blue

вне́шняя стена́ — outer wall

вне́шний вид — (outward) look/appearance; exterior

вне́шний мир — the outside world

вне́шние усло́вия — outward conditions

вне́шний при́знак — outward sign

вне́шний у́гол — exterior angle

вне́шние поврежде́ния — external injuries

вне́шнее споко́йствие — outward calm

вне́шнее схо́дство — superficial resemblance

вне́шний лоск — surface polish

вне́шнее дружелю́бие — surface friendliness

вне́шняя поли́тика — foreign policy

циркуляция морской воды
—
[ 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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]

Тематики

• охрана окружающей среды

EN

• sea circulation

DE

• Meereskreislauf

FR

• circulation maritime

циркуляция морской воды
—
[ 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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]

Тематики

• охрана окружающей среды

EN

• sea circulation

DE

• Meereskreislauf

FR

• circulation maritime

циркуляция морской воды
—
[ 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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]

Тематики

• охрана окружающей среды

EN

• sea circulation

DE

• Meereskreislauf

FR

• circulation maritime

внешний вид — (outward) appearance

внешняя часть — outside

внешнее сходство — outward / superficial / formal resemblance

внешний рейд — outer harbour

внешний лоск — surface polish, gloss

внешний осмотр — superficial examination

внешняя политика — foreign policy

внешний рынок — foreign market

внешняя торговля — foreign trade

внешние сношения — foreign relations

вне́шний вид — (outward) appearance

вне́шняя часть — outside

вне́шнее схо́дство — similarity in appearance; outward resemblance

вне́шний лоск — surface polish / gloss

вне́шний осмо́тр — superficial / visual examination

вне́шняя поли́тика — foreign policy

вне́шний ры́нок — foreign market

вне́шняя торго́вля — foreign / external trade

вне́шние сноше́ния — foreign relations

вне́шний мир — outside / outer world

использование ресурсов морского дна
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]

EN

sea bed exploitation
Marine mineral resources extend far beyond those presently exploited; minerals are derived from two separate types of marine sources: from sedimentary deposits underlying the continental shelves and from inshore deposits on the surface of the continental shelves. By far the most valuable of the mineral resources exploited from marine environments is petroleum. Offshore placer deposits on the surface of the continental shelves yield gold, platinum, and tin. On the floors of the world's oceans manganese nodules are found as a result of pelagic sedimentation or precipitation; they are small, irregular, black to brown, friable, laminated concretionary masses consisting primarily of manganese salts and manganese-oxide minerals. (Source: PARCOR / BJGEO)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]

Тематики

• охрана окружающей среды

EN

• sea bed exploitation

DE

• Ausbeutung des Meeresgrundes

FR

• exploitation des fonds marins

климат
—
[ 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

• охрана окружающей среды

EN

• climate

DE

• Klima

FR

• climat

использование ресурсов морского дна
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]

EN

sea bed exploitation
Marine mineral resources extend far beyond those presently exploited; minerals are derived from two separate types of marine sources: from sedimentary deposits underlying the continental shelves and from inshore deposits on the surface of the continental shelves. By far the most valuable of the mineral resources exploited from marine environments is petroleum. Offshore placer deposits on the surface of the continental shelves yield gold, platinum, and tin. On the floors of the world's oceans manganese nodules are found as a result of pelagic sedimentation or precipitation; they are small, irregular, black to brown, friable, laminated concretionary masses consisting primarily of manganese salts and manganese-oxide minerals. (Source: PARCOR / BJGEO)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]

Тематики

• охрана окружающей среды

EN

• sea bed exploitation

DE

• Ausbeutung des Meeresgrundes

FR

• exploitation des fonds marins

климат
—
[ 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

• охрана окружающей среды

EN

• climate

DE

• Klima

FR

• climat

использование ресурсов морского дна
—
[ http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]

EN

sea bed exploitation
Marine mineral resources extend far beyond those presently exploited; minerals are derived from two separate types of marine sources: from sedimentary deposits underlying the continental shelves and from inshore deposits on the surface of the continental shelves. By far the most valuable of the mineral resources exploited from marine environments is petroleum. Offshore placer deposits on the surface of the continental shelves yield gold, platinum, and tin. On the floors of the world's oceans manganese nodules are found as a result of pelagic sedimentation or precipitation; they are small, irregular, black to brown, friable, laminated concretionary masses consisting primarily of manganese salts and manganese-oxide minerals. (Source: PARCOR / BJGEO)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]

Тематики

• охрана окружающей среды

EN

• sea bed exploitation

DE

• Ausbeutung des Meeresgrundes

FR

• exploitation des fonds marins

климат
—
[ 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

• охрана окружающей среды

EN

• climate

DE

• Klima

FR

• climat