An increase in temperature, for example, can boost the moisture content of the atmosphere, which then causes further warming because water vapor is a greenhouse gas.
例如，温度的升高会增加大气中的水分含量，这又会导致进一步的变暖，因为水蒸气是一种温室气体。
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。
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。
Water vapor in the lower atmosphere can vary in amount from a mere trace in arid regions to about 4% by volume in moist areas.
大气低层的水汽量在干燥地区（量）甚微，而在潮湿地区按体积占4%左右。
This map shows the distribution of water vapor in Earth's atmosphere during August 2010.
这张地图展示了2010年八月期间地球大气层中的水蒸气分布情况。
Water vapor, carbon dioxide and other gases in the atmosphere trap heat from the sun, warming Earth.
水蒸气、二氧化碳和大气中的一些其它气体将来自太阳的热量收集起来，温暖了地球。
The heaviest rainstorms have already become 67 percent heavier since 1958 in the Northeast, as warmer weather evaporates more water vapor into the atmosphere to feed storm clouds.
——由于炎热的天气导致大量的水蒸发到大气中，形成暴雨云，从1958年至今，东北部大暴雨的强度已经增加了67%。
Together, evaporation, transpiration, and sublimation, plus volcanic emissions, account for almost all the water vapor in the atmosphere.
大气层中水蒸气几乎都来源于蒸发作用、蒸腾作用、升华作用再加上火山释放的水蒸气。
Eventually, the water stored as vapor in the atmosphere will condense to liquid again.
最后，大气中储存的水蒸气将再次凝缩为液体。
The local weighted average temperature has very important function in remote sensing atmosphere precipitable water vapor by using ground-based GPS.
在利用地基GPS进行大气水汽遥感时，加权平均温度对水汽遥感结果起着举足轻重的作用。
Due to the strong spatial inhomogeneity and temporal variability of atmosphere, especially water vapor , accurate modeling of path delay in GPS signals is necessary for high -accuracy position.
由于大气分布不均和不断的变化，尤其是大气中的水汽影响，使建立无线电信号路径延迟的精确模型在GPS高精度定位中非常必要。
The distribution of total cooling rate in the lower atmosphere is mainly determined the distribution of water vapor cooling rate.
大气低层总冷却率的分布主要取决于水汽冷却率的分布。
Many gases naturally occur in the atmosphere, such as water vapor, carbon dioxide, methane, and nitrous oxide.
许多气体自然出现在大气层中，例如，水蒸气，二氧化碳，甲烷和一氧化二氮。
This structure is produced by chemical vapor deposition (CVD) of carbon nanotubes in the presence of a metal catalyst in a reaction atmosphere with an oxidizing agent, preferably water, added thereto.
将该结构体是在金属催化剂的存在下，在反应气氛中添加氧化剂、优选水，使碳纳米管进行化学气相成长(CVD)进行制造的。
The fundamental and method of the ground-based microwave radiometer remote sensing retrieval of integrated water vapor(V) and cloud liquid water(L) in the atmosphere are introduced herein.
介绍了地基微波辐射计遥感反演大气柱中的水汽总量和云液态水总量的辐射传输原理和反演方法。
Water vapor in earth's atmosphere plays a crucial role for climate, dynamics of weather system, atmosphere environment, hydrology and space geodesy.
地球大气中的水汽在全球气候系统、天气动力系统、大气环境科学、水文学以及空间大地测量等方面占有非常重要的地位。
Sunphotometer is designed to measure the direct solar irradiance for retrieving the amount of the vapor of water, ozone and nitrogen oxide etc. in the atmosphere.
太阳辐射计通过测量不同波段的直接太阳辐射反演地球大气中水汽、臭氧及氮氧化物等气体的含量。
The height and the excess phase variations of the occultation caused by water vapor and the temperature variety in the atmosphere boundary layer are studied in details.
详细研究了大气边界层水汽和温度变化对掩星观测高度、相位时延的影响；
The height and the excess phase variations of the occultation caused by water vapor and the temperature variety in the atmosphere boundary layer are studied in details.
详细研究了大气边界层水汽和温度变化对掩星观测高度、相位时延的影响；
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