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41 высота подъёма
1. с. -х. lifting height2. clearance height3. hoisting height, height of liftвысота центров — swing; height of centers
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42 индикатор гремучего газа
Русско-английский научный словарь > индикатор гремучего газа
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43 area
area nобластьacceleration areaучасток разгонаactive thunderstorm areaрайон активной грозовой деятельностиadvisory areaконсультативная зонаaerodrome approach areaзона подхода к аэродромуaerodrome graded areaспланированный участок аэродромаaerodrome movement areaзона движения воздушных судовair intake hazard areaопасная зона перед воздухозаборникомairport construction areaзона застройки аэропортаairport prohibited areaзапретная зона аэропортаairport service areaслужебная зона аэропортаair-route areaрайон воздушных трассairspace restricted areaзона воздушного пространства с особым режимом полетаair traffic control areaзона управления воздушным движениемalert areaзона повышенного вниманияalighting areaместо посадкиapproach areaзона захода на посадкуapproach area hazardпрепятствие в зоне захода на посадкуarea chartкарта районаarea controlуправление в зонеarea control centerрайонный диспетчерский центр управления движением на авиатрассеarea density calculationрасчет удельной нагрузки на поверхностьarea flight controlрайонный диспетчерский пункт управления полетамиarea forecastзональный прогнозarea forecast centerцентр зональных прогнозовarea forecast planплан зональных прогнозовarea forecast systemсистема зональных прогнозов(погоды) area navigationзональная навигацияarea navigation capabilityтехнические характеристики зональной навигацииarea navigation equipmentбортовое оборудование зональной навигацииarea navigation routeмаршрут зональной навигацииarea navigation systemсистема зональной навигацииarea of coverageзона действияarea of coverage of the forecastsрайон обеспечения прогнозамиarea of occurenceрайон происшествияarea of responsibilityзона ответственностиarea watchконтроль в зонеbaggage break-down areaзона обработки прибывающего багажаbaggage-claim areaместо востребования багажаbaggage delivery areaместо выдачи багажаbearing areaнесущая поверхностьboarding areaместо загрузкиboundary of the areaграница зоныbreak-in areaместо вырубанияbuild-in areaзона застройкиcircling approach areaзона захода на посадку по кругуclimb-out areaзона начального этапа набора высотыcone effect areaзона конусного эффектаcongested areaзона интенсивного воздушного движенияdanger areaопасная зонаdanger areas chartкарта опасных зонdead areaмертвая зонаdeparture areaзона торможенияdesign wing areaрасчетная площадь крылаdirect transit areaзона прямого транзитаdrag areaплощадь сопротивленияend safety areaконцевая зона безопасностиen-route areaзона маршрутаentry areaзона подходаEurocontrol areaзона Евроконтроляextended end safety areaпродленная концевая зона безопасностиfacsimile area forecast chartфаксимильная карта зональных прогнозовfog-prone areaрайон скопленияgases shear areaзона среза активной струиgrass landing areaпосадочная площадка с травяным покрытиемgross wing areaплощадь крыла, включая подфюзеляжную частьhard-core areaзона высокой интенсивностиholding areaзона ожиданияinterference-free areaзона, свободная от помехland areaместо посадкиlanding area facilitiesоборудование зоны посадкиleave a parking areaвыруливать с места стоянкиlifting surface areaнесущая поверхностьliftoff areaзона отрываloading areaместо загрузкиload per unit areaнагрузка на единицу площадиlow air areaнижнее воздушное пространствоlow control areaнижний диспетчерский районmaintenance areaзона технического обслуживанияmake-up areaместо комплектованияmaneuvering areaплощадь маневрирования(manoeuvring area) noncritical areaнеопасная зонаnozzle exit areaвыходное сечение соплаoceanic area control centerокеанический районный диспетчерский центрoceanic control areaокеанический диспетчерский районopen-water areaнадводный районoperational areaзона полетовoverrun areaзона выкатыванияoverrun safety areaзона безопасности при выкатыванииparking areaместо стоянкиpassenger assembly areaместо сбора пассажировpolar areaполярный районpoleward areaприполярный районprepared landing areaподготовленная посадочная площадкаprimary area boundaryграница основной зоныprohibited areaзапретная зонаpropeller disk areaплощадь, ометаемая воздушным винтомradar control areaзона действия радиолокатораradar service areaзона радиолокационного обслуживанияrecovery areaрайон обнаруженияreserved areaзапасная зонаrestricted areaзона ограниченияrestricted use areaзона ограниченной эксплуатацииrouting areaрайон прохождения маршрутаrun-up areaплощадка для опробованияrunway end safety areaконцевая зона безопасности ВППrunway end safety area lightsогни концевой зоны безопасности ВППsearch and rescue areaрайон поиска и спасанияsecondary area boundaryграница дополнительной зоныsensitive areaзона чувствительностиservice areaзона обслуживанияsignal areaсигнальная площадкаspeed control areaзона выдерживания скоростиsupporting areaнесущая поверхностьtailpipe areaместо расположения выхлопных трубtakeoff areaзона взлетаtakeoff flight path areaзона набора высоты при взлетеtemporary restricted areaзона временного ограниченияterminal areaзона аэродромаterminal area streamlineсхема зоны аэродромаterminal area surveillance radarрадиолокатор обзора зоны аэродромаterminal area taxi sequenceочередность заруливания к зданию аэровокзалаterminal control areaузловой диспетчерский районticket check areaместо проверки билетовtraining areaзона тренировочных полетовtransit areaтранзитная зонаtransit passenger areaзона для транзитных пассажировturnaround areaзона разворота на обратный курсundershoot areaзона перед порогом ВППunobstructed landing areaзона приземленияupper advisory areaверхняя консультативная зонаupper air areaверхнее воздушное пространствоupper area control centerдиспетчерский центр управления верхним райономupper control areaверхний диспетчерский районupper level control areaверхний район управления эшелонированиемvariable area nozzleсопло с регулируемым сечениемwarning areaзона предварительного оповещенияwing areaплощадь крылаWorld area forecast centerВсемирный центр зональных прогнозов -
44 климат
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
EN
DE
FR
Русско-немецкий словарь нормативно-технической терминологии > климат
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45 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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46 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
EN
DE
FR
Франко-русский словарь нормативно-технической терминологии > climat
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47 circulation maritime
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
Франко-русский словарь нормативно-технической терминологии > circulation maritime
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48 Klima
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
EN
DE
FR
Немецко-русский словарь нормативно-технической терминологии > Klima
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49 Meereskreislauf
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
Немецко-русский словарь нормативно-технической терминологии > Meereskreislauf
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50 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
EN
DE
FR
Русско-английский словарь нормативно-технической терминологии > климат
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51 циркуляция морской воды
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
EN
DE
FR
Русско-английский словарь нормативно-технической терминологии > циркуляция морской воды
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52 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
EN
DE
FR
Русско-французский словарь нормативно-технической терминологии > климат
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53 циркуляция морской воды
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
EN
DE
FR
Русско-французский словарь нормативно-технической терминологии > циркуляция морской воды
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54 climate
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
EN
DE
FR
Англо-русский словарь нормативно-технической терминологии > climate
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55 sea circulation
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
Англо-русский словарь нормативно-технической терминологии > sea circulation
См. также в других словарях:
Polar wind — is the permanent outflow of ionization from the polar regions of the magnetosphere. [http://amsglossary.allenpress.com/glossary/browse?s=p p=43 AMS Glossary] ] Ionospheric Plasma SourceThe ‘ground state’ of the ionosphere consists of the baseline … Wikipedia
Polar mesospheric summer echoes — (PMSE) is the phenomenon of anomalous radar echoes found in the polar latitudes from May through early August between 80 90 km in altitude. The usual instrument for observing PMSE is the a VHF Mesosphere Stratosphere Troposphere (MST) radar,… … Wikipedia
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Polar city — Infobox title = Polar City name = Polar City caption = This is an artist s rendition of a Polar City planned for Longyearbyen. It represents both above and below ground components which contain city infrastructure, residential housing, limited… … Wikipedia
polar ecosystem — Introduction complex of living organisms in polar regions such as polar barrens and tundra. Polar barrens and tundra are found at high latitudes on land surfaces not covered by perpetual ice and snow. These areas lying beyond the tree line … Universalium
Polar, Wisconsin — Infobox Settlement official name = Polar, Wisconsin settlement type = Town nickname = motto = imagesize = image caption = image mapsize = 250px map caption = Location of Polar, Wisconsin mapsize1 = map caption1 = subdivision type = Country… … Wikipedia
Polar distribution — In probability theory, the polar distribution is the probability distribution of angles occurring in a set of two dimensional vectors, denoted by :p(phi).,It is usually graphically represented as a closed curve :(x,y) = (rcosphi, , rsinphi)… … Wikipedia
polar molecule — /poʊlə ˈmɒləkjul/ (say pohluh moluhkyoohl) noun a molecule which has a permanent electric dipole as a result of the distribution of electron density within it …
Mars Polar Lander — Artist depiction of Mars Polar Lander on Mars. Operator NASA / JPL Major contractors Martin Marietta … Wikipedia
Marsaglia polar method — The polar method (attributed to George Marsaglia, 1964[1]) is a pseudo random number sampling method for generating a pair of independent standard normal random variables. While it is superior to the Box–Muller transform[citation needed], the… … Wikipedia
Drag and Atmospheric Neutral Density Explorer — DANDE Operator University of Colorado at Boulder, Colorado Space Grant Consortium, CU Dept of Aerospace Engineering Sciences, AFRL, STP Mission type Demonstration of Concept, Neutral Density … Wikipedia