water vapor in atmosphere 大气中之水蒸气
vapor in night 夜间的水气
vapor in atmosphere 大气水汽
absorb vapor in liquid 液体吸收蒸气
vapor in the flue gas 烟气中水蒸气
With temperatures rising and more water vapor in the air, such storms can pull in more moisture and thus rain or snow more heavily than storms of old.
随着气温升高,空气中的水蒸气增多,这样的风暴会吸收更多的湿气,因此雨雪会比以前的风暴来得更猛烈。
The assumption of constant relative humidity is important, because water vapor in the atmosphere is another efficient absorber of radiation at infrared wavelength.
相对湿度恒定的假设是重要的,因为大气中的水蒸气是红外波长辐射的另一种有效吸收剂。
Because warm air can hold more moisture than cool air, the relative humidity will be constant only if the amount of water vapor in the atmosphere increases as the temperature rises.
因为温暖的空气比冷空气能容纳更多的湿气,所以只有当大气中的水蒸气量随着温度的升高而增加时,相对湿度才会保持不变。
And the triple point of water is 16K that temperature and pressure - there's a unique temperature and pressure where water exists in equilibrium between the liquid phase, the vapor phase, and the solid phase.
与水的三相点,我们定义它为273。,水的三相点,是一个特定的温度和压强,可以使水的液态,气态和固态三相共同达到平衡,三相点是液态。
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