過冷水冰滴 的英文怎麼說

中文拼音 [guòlěngshuǐbīng]
過冷水冰滴 英文
droxtal
  • : 過Ⅰ動詞[口語] (超越) go beyond the limit; undue; excessiveⅡ名詞(姓氏) a surname
  • : Ⅰ形容詞1 (溫度低; 感覺溫度低) cold:冷水 coldwater; 你冷不冷? do you feel cold?; are you feeling...
  • : 名詞1 (由兩個氫原子和一個氧原子結合而成的液體) water 2 (河流) river 3 (指江、河、湖、海、洋...
  • : Ⅰ動詞(液體一點一點地向下落) drip Ⅱ名詞(一點一點地向下落的液體) drop; droplet Ⅲ量詞(用於滴下的液體的數量) drop
  • 水冰 : water ice
  1. When i become quite motionless, cold, and rigid as a corpse, then, and not before, - be careful about this, - force open my teeth with the knife, pour from eight to ten drops of the liquor containted in the phial down my throat, and i may perhaps revive.

    當我變得一動不動,,硬? ?的,象一具死屍那樣的時候,你要記住,要及時地,但千萬不要早地,用鑿子撬開我的牙,把瓶子里的藥至十到我的喉嚨里,也許我還會恢復來。 」
  2. The results show that the auto - conversion of frozen drops and graupels ( cnfh, cngh ) are the main sources of the hailstones in the strong convective storm studied in the paper, but the contribution of frozen drops is greater than that of graupels. hailstones mainly depend on the processes of collecting supercooled water ( clch, clrh ) to grow. the relatively simple mass continuous equation was used to calculate vertical velocity, and use radial projection relation of dual - doppler radar to retrieve the case ' s three - dimensional wind field

    同時模擬分析了雹形成的微物理程,結果表明,本個例模擬雹雲中,雹粒子主要由凍和霰轉化( cnfh , cngh )形成,但凍雹形成的貢獻要比霰大得多,雹含量中心的發展演變與凍量中心的發展演變相一致,雹主要是通撞凍程( clch , clrh )而進一步長大的。
  3. There is an active growth layer and super cooled water exists with ice crystals that may be an important feature layer to occur rain in stratiform cloud

    晶共存層存在,且晶活躍增長,此層的存在可能是發生降的關鍵。
  4. Using ice cold water at 5, the coffee is filtered, fermented, and dripped for 8 hours to bring out the full flavor of the beans, preserving their fragrance and revealing their mellowness

    5低溫塊與的滲透、醞釀,濾8小時粹?出咖啡豆豐富的口感與完整的香氣,展現咖啡的香醇。
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