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21 знать, почём сотня гребешков
разг., шутл.cf. know what is what; know a thing or two; know beans; know chalk from cheeseВ наших кинокартинах Тосины соотечественницы творили такие дела малость поскромней, но тоже сразу было видно, что они не лыком шиты и распрекрасно знают, почём сотня гребешков. (Б. Бедный, Девчата) — In our movies the girls did those things on a less grand scale, but even then you could see at once that they were no novices and knew what was what only too well.
Русско-английский фразеологический словарь > знать, почём сотня гребешков
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22 вторгаться в личную жизнь
духовный мир, духовная жизнь — the world of spirit
Русско-английский большой базовый словарь > вторгаться в личную жизнь
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23 излом
1. м. fractureвид излома характеризует ряд механических свойств материала — fracture gives an indication of some mechanical properties of the material
2. м. bend, breakСинонимический ряд:изгиб (сущ.) извив; извилина; извилину; изворот; изгиб -
24 поддерживать жизнь
духовный мир, духовная жизнь — the world of spirit
Русско-английский большой базовый словарь > поддерживать жизнь
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25 проведение плана в жизнь
духовный мир, духовная жизнь — the world of spirit
Русско-английский большой базовый словарь > проведение плана в жизнь
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26 коэффициент
коэффициент сущ1. coefficient2. factor аэродинамический коэффициентaerodynamic coefficientВПП с низким коэффициентом сцепленияslippery runwayзамеренный коэффициент сцепленияmeasured friction coefficientкоэффициент атмосферного поглощенияatmospheric absorption rateкоэффициент валютного регулированияcurrency adjustment factorкоэффициент доплеровского смещенияDoppler shift factorкоэффициент доходной загрузкиbreak-even load factorкоэффициент загрузки1. cargo load factor2. load factor 3. weight load factor коэффициент загрузки воздушного суднаaircraft load factorкоэффициент замедленияmoderation ratioкоэффициент занятости пассажирских креселpassenger load factorкоэффициент запаса длиныlength factorкоэффициент заполнения воздушного винтаpropeller solidity ratioкоэффициент затуханияattenuation rateкоэффициент затухания звукаsound attenuation coefficientкоэффициент звукоизоляцииsound insulation coefficientкоэффициент использования аэродрома1. aerodrome utilization factor2. aerodrome usability factor коэффициент использования воздушного суднаaircraft usability factorкоэффициент использования ВППrunway usability factorкоэффициент лобового сопротивленияdrag coefficientкоэффициент отраженияground reflection coefficientкоэффициент перегрузки воздушного суднаaircraft acceleration factorкоэффициент пересчетаconversion factorкоэффициент пикаcrest factorкоэффициент поглощенияatmospheric absorption coefficientкоэффициент поглощения звукаsound absorption coefficientкоэффициент поглощения шумаnoise absorption coefficientкоэффициент подъемной силыlift coefficientкоэффициент полезного действияoutput factorкоэффициент полезной загрузкиrevenue load factorкоэффициент полезной нагрузкиuseful load factorкоэффициент помехsignal-to-noise ratioкоэффициент пульсацииpulsation coefficientкоэффициент рассеиванияscatter coefficientкоэффициент расходаmass flow rateкоэффициент скольженияslip ratioкоэффициент сцепления1. friction Mu-factor2. friction coefficient коэффициент теплопередачиcoefficient of heat transferкоэффициент торможенияbraking coefficientкоэффициент тренияfriction factorкоэффициент усиленияamplification factorкоэффициент экранированияshielding factorмасштабный коэффициент девиацииdeviation scale factorпоправочный коэффициентadjustment factorрасчетный коэффициентdesign factorтарифный коэффициентtariff level factorэксплуатационный заправочный коэффициентoperating correction factor -
27 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
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Русско-английский словарь нормативно-технической терминологии > циркуляция морской воды
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