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1 морской климат
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2 морской климат
1) Naval: marine climate2) Engineering: coastal climate3) Automobile industry: maritime climate4) Ecology: subtropical highland (о климате севера и северо-запада Шотландии), marine west coast climate, British climate5) Makarov: oceanic climate -
3 климат
м.1) ( особенности погоды) climateжа́ркий кли́мат — hot / torrid climate
морско́й кли́мат — maritime climate
2) ( обстановка) climate, atmosphereмеждунаро́дный кли́мат — international climate
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4 приморский климат
1) Naval: littoral climate2) Medicine: coast climate3) Engineering: maritime climate4) Automobile industry: coastal climate -
5 морской климат
marine climate, maritime climate -
6 морской климат
marine climate; maritime climate -
7 приморский климат
marine climate; maritime climateРусско-английский географический словарь > приморский климат
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8 морской
прлsea attr; marineморско́й во́здух — sea air
морско́й порт — seaport
морски́е расте́ния/живо́тные — marine plants/animals
морско́й бе́рег — seashore
морска́я ата́ка/торго́вля — seaborne attack/trade
морско́й капита́н — sea captain
морско́й офице́р — naval officer
морска́я пехо́та — marines pl
- страдать морской болезньюморско́й кли́мат — maritime climate
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9 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)
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Русско-английский словарь нормативно-технической терминологии > циркуляция морской воды
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