the back regions

the Arctic Region - Арктика, арктический регион

few unknown regions are left on the Earth - на земле осталось мало неизученных мест

the aquatic regions of the Earth - водные пространства земли

every region of science - каждая область науки

the region of mythology [of metaphysics] - сфера /область/ мифологии [метафизики]

in the region of - а) в сфере, в области; б) поблизости

Moscow [Tver] Region - Московская [Тверская] область

the city was divided into seven regions - город делился на семь районов

the abdominal region - область живота, абдоминальная область

a pain in the region of the heart - боль в области сердца

the region is indicated on the diagram - это место указано /обозначено/ в диаграмме

the back regions (of a house) - кухня; подсобное помещение

the upper regions - небо

the nether /the lower/ regions - ад, преисподняя

the region beyond the grave - загробное царство

celestial regions - небесные сферы

to abandon power — отказываться от власти

to assume power — брать власть в свои руки; приходить к власти

to attain power — добиваться власти

to be endowed with wide powers — быть облаченным широкими полномочиями

to be in a position of power — занимать руководящую должность

to come back into power — возвращаться к власти

to come to power — приходить к власти; брать власть в свои руки

to conspire to seize power — организовывать заговор с целью захвата власти

to demilitarize atomic power — переключать использование атомной энергии с военных на мирные цели

to disturb the balance of power — нарушать равновесие сил

to enhance the power of Parliament — усиливать власть парламента

to establish power — устанавливать власть

to exercise power of influence — оказывать воздействие

to fall from power — лишаться власти

to gain power — захватывать власть; приходить к власти

to have power — иметь власть

to hold military power — контролировать вооруженные силы

to hold the reins of power — удерживать бразды правления

to indulge in an orgy of state power — упиваться государственной властью

to jockey for power — пробиваться к власти

to maintain an overall grip on power — прочно удерживаться у власти

to move out of power — лишаться власти

to overthrow the power — свергать власть

to phase out the use of nuclear power — постепенно отказываться от использования атомной энергии

to prejudice the power — ограничивать права

to reach power — достигать власти

to reinforce presidential power — усиливать президентскую власть

to relinquish power — отказываться от власти

to remain in power — оставаться у власти

to renew powers — возобновлять полномочия

to resume power — возвращаться к власти

to stay in power — оставаться у власти

to strengthen police powers — усиливать полномочия полиции

to struggle for power — бороться за власть

to take over power — приходить к власти; захватывать власть

to upset the balance of power — нарушать равновесие сил

to usurp power — узурпировать власть

to vie for power — бороться за власть

to win power — захватывать / завоевывать власть; приходить к власти

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