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1 возрастные группы
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2 население старших возрастных групп
Русско-английский большой базовый словарь > население старших возрастных групп
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3 возрастная шкала
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4 шкала возрастных эквивалентов
Russian-english psychology dictionary > шкала возрастных эквивалентов
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5 масштаб
( фотосъемки) dimensioning полигр., scale* * *масшта́б м.
scaleбольшо́го масшта́ба — large scaleв и́стинном масшта́бе вре́мени — in real-timeв промы́шленных масшта́бах — in production quantities, on industrial scaleвыче́рчивать что-л. в масшта́бе ( без указания масштаба) — draw smth. to scaleвыче́рчивать что-л. в масшта́бе 1в [m2]100 — draw on [at] a [the] 1 100 scale, draw on [at] a [the] scale of 1 100ма́лого масшта́ба — small-scaleмасшта́б … на киломе́тр — scale … to the kilometreпока́зывать [представля́ть] в увели́ченном масшта́бе — scale upпока́зывать [представля́ть] в уме́ньшенном масшта́бе — scale downрастя́гивать масшта́б — exaggerate the scaleмасшта́б Бонжа́на мор. — Bonjean diagram, Bonjean curvesмасшта́б в да́нной то́чке — point scaleвертика́льный масшта́б — height [vertical] scaleгла́вный масшта́б — base [general, nominal, principal] scaleгоризонта́льный масшта́б — horizontal scaleграфи́ческий масшта́б — scale line, bar [graphical] scaleмасшта́б заложе́ний — scale of slopeмасшта́б изображе́ния тлв. — image scaleмасшта́б картографи́рования — plotting scaleкру́пный масшта́б — large scaleлине́йный масшта́б — scale line, bar [graphical] scaleлогарифми́ческий масшта́б — logarithmic scaleме́лкий масшта́б — small scaleосновно́й масшта́б — base [general, nominal, principal] scaleпереме́нный масшта́б — variable scaleпла́вающий масшта́б — floating scaleполулогарифми́ческий масшта́б — semi-log(arithmic) scaleмасшта́б по меридиа́ну — scale in meridian, meridional scaleмасшта́б по паралле́ли — scale in parallel, parallel scaleпопере́чный масшта́б — diagonal [transversal] scaleпостоя́нный масшта́б — fixed scaleмасшта́б построе́ния — plotting scaleмасшта́б по эква́тору — equatorial scaleпредвы́численный масшта́б — predetermined scaleприведё́нный масшта́б — corrected scaleмасшта́б расстоя́ний ( в расчёте распространения радиоволн) — scale distanceмасшта́б съё́мки — scale of surveyingмасшта́б уменьше́ния — reduction scaleуме́ньшенный масшта́б — reduced scaleуса́дочный масшта́б — shrink(age) ruleусло́вный масшта́б — representative scaleча́стный масшта́б — local [particular, relative] scaleчи́сленный масшта́б — numerical scale, representative fraction -
6 шкала возрастных эквивалентов
Aviation medicine: age scale, age-equivalent scaleУниверсальный русско-английский словарь > шкала возрастных эквивалентов
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7 в возрасте
канонический возраст, возраст рукоположения — canonical age
умственное развитие, соотносимое с возрастом — mental age
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8 возраст, по достижении которого происходит повышение
SAP. age for pay scale jumpУниверсальный русско-английский словарь > возраст, по достижении которого происходит повышение
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9 возрастная шкала
Psychology: age (equivalent) scale -
10 повышение уровня тарифа по достижении определенного возраста
SAP. pay scale jump due to ageУниверсальный русско-английский словарь > повышение уровня тарифа по достижении определенного возраста
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11 получать
(приобретать, добиваться, выигрывать) gain, obtain, receive, get, secure By rendering coalitions ineffective, males contribute to a combination of factors (e.g. low potential to gain from cooperation in contest feeding competition) that limit the benefits of female philopatry.пополнение популяции- (за счет репродукции) recruitment, recruit-stockсм. также резерв популяционныйInbelieve more complete data available for the two last seasons more accurately defines the total minimum resident population .In any event, the data suggest that population has stabilized at about 10 adults which are full-time winter residents .Inestimated a total population of 22 (локальная популяция крупных млекопитающих .область необитаемая или, в лучшем случае, малонаселённая получать - area uninhabited or at best thinly populatedэлементарная, дем получать - demeминимальная численность жизнеспособной получать - minimum viable population sizeдопустимый минимальный порог численности получать - minimum population size thresholdsрезкое сокращение численности получать - drastic population decline (since)сохранить получать - perpetuate viable population, preserve viable populationриск оказаться эксплуатируемой - existing or potential exploitation (persecution)Русско-английский словарь по этологии (поведению животных) > получать
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12 на период
1. during the terms of2. for a period3. for the term ofза прошедшие годы; в период между — in the intervening years
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13 циркуляция морской воды
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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > циркуляция морской воды
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14 циркуляция морской воды
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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-английский словарь нормативно-технической терминологии > циркуляция морской воды
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15 циркуляция морской воды
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)
[http://www.eionet.europa.eu/gemet/alphabetic?langcode=en]Тематики
EN
DE
FR
Русско-французский словарь нормативно-технической терминологии > циркуляция морской воды
См. также в других словарях:
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