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1 греть
1. (без доп.; излучать тепло) give* out warmthв марте солнце уже греет — in March the sun's rays are already warm, it is already warm in the sun in March
2. (вн.) warm (d.), heat (d.); (подогревать, согревать) warm up (d.), heat up (d.); (о тёплой одежде, обуви) keep* warm (d.)греть руки — warm one's hands
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2 греть
1) ( излучать тепло) give out warmthпе́чка пло́хо греет — the stove gives out very little warmth
в ма́рте со́лнце уже́ греет — in March the sun's rays are already warm, it is already warm in the sun in March
2) (сов. согре́ть) (о тёплой одежде, обуви) keep (d) warmего́ шу́ба хорошо́ греет — his fur coat keeps him warm
3) (сов. нагре́ть) (вн.; подогревать, согревать) warm up (d), heat up (d)4) (сов. согре́ть) (вн.; отогревать) warm (d), heat (d)греть ру́ки — warm one's hands
••греть ру́ки на чём-л разг. неодобр. — ≈ line one's pockets ( by dishonest or illegal means)
греть ду́шу (дт.) — give (i) comfort
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3 тепло
I с.1) ( тепловая энергия) heat; ( обогрев) heatingдать в дома́ тепло́ и свет — supply heating and light to people's homes
пе́чка не даёт никако́го тепла́ — the stove produces no heat / warmth
2) ( тёплая погода или среда) warmth16 гра́дусов тепла́ — sixteen degrees above zero
держа́ть в тепле́ (вн.) — keep (d) (in the) warm
3) ( доброта) warmth; cordialityIIсерде́чное тепло́ — sincere affection, the warmth of smb's heart
1) кратк. прил. см. тёплыйсего́дня тепло́ — it is warm today
ему́ [им] тепло́ — he is [they are] warm
вам тепло́? — are you warm enough?
на со́лнышке тепло́ — it is warm in the sun
в ко́мнате тепло́ — the room is warm, it is warm in the room
в э́том сви́тере тепло́ — this sweater ['swe-] is warm
3) предик. безл. ( в играх - о близости к искомому предмету или правильному ответу) (it's) warmIII нареч.1) ( не холодно) warmlyодева́ться тепло́ — dress warmly
2) ( сердечно) warmly, cordiallyтепло́ встре́тить кого́-л — give smb a warm / cordial / hearty welcome, welcome smb
тепло́ встре́тить сообще́ние — welcome the news
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4 тепло
1. с.1. ( тепловая энергия) heat16 градусов тепла — sixteen degrees above zero (C.), 16° C
2. (тёплое состояние чего-л.) warmth; (перен. тж.) cordiality2.держать в тепле (вн.) — keep* (in the) warm (d.)
1. прил. кратк. см. тёплый2. предик. безл.:сегодня тепло — it is warm / mild today
ему, им и т. д. тепло — he is, they are, etc., warm
3. нареч.в комнате тепло — the room is warm, it is warm in the room
warmly; (перен. тж.) cordiallyтепло встретить кого-л. — give* smb. a warm / cordial / hearty welcome, welcome smb.
тепло встретить сообщение и т. п. — welcome the news etc.
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5 тепло
I ср.1) heat ( тепловая энергия)2) warmth (теплое состояние чего-л.); cordiality перен.- сердечное тепло II 1. прил.; кратк. форма от теплый 2. предик.сегодня тепло — it is warm/mild today
3. нареч.в комнате тепло — the room is warm, it is warm in the room
warmly; cordially перен.тепло встретить кого-л. — to give smb. a warm/cordial/hearty welcome, to welcome smb.
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6 греть
несов1) warm, heatгреть ру́ки (но́ги) — warm one's hands (feet)
2) ( излучать тепло) give out warmthсо́лнце си́льно гре́ет — it's very warm in the sun
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7 нажариваться (I) > нажариться (II)
............................................................1. bask(vt.) آفتاب خوردن، با گرمای ملایم گرم کردن، حمام آفتاب گرفتن............................................................Русско-персидский словарь > нажариваться (I) > нажариться (II)
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8 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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9 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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10 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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11 нажариваться
возвр.; разг.
bask in the sun, warm oneself in the sun (for a long time)* * *нажариваться; нажариться bask in the sun -
12 пригревать
св - пригре́ть1) vti обогревать to warmсо́лнце пригрева́ет — the sun/it is getting quite warm
2) vt разг давать приют to give shelter to, to cherishпригре́ть змею́ на груди́ — to cherish a serpent/a snake in one's bosom
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13 греться
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14 греться
1) ( согревать себя) warm oneselfгре́ться на со́лнце — bask in the sun, sun oneself
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15 греться
нсвto warm/to heat oneselfгреться на со́лнце — to bask in the sun, to sun oneself
греться в луча́х сла́вы — to bask in fame
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16 Облачное небо, само по себе являющееся плохим поглотителем тепла, редко позволяет солнцу прогреть океан.
Универсальный русско-английский словарь > Облачное небо, само по себе являющееся плохим поглотителем тепла, редко позволяет солнцу прогреть океан.
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17 únu-únu
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18 солнце излучало приятное тепло
General subject: the sun was gently warmУниверсальный русско-английский словарь > солнце излучало приятное тепло
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19 нажариваться
нажариться разг. (на солнце)bask, или warm oneself, in the sun (for a long time) -
20 по-весеннему
- 1
- 2
См. также в других словарях:
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