- 更多网络例句与水汽含量相关的网络例句 [注：此内容来源于网络，仅供参考]
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The large orography of the Plateau hinders the moisture transport from Bay of Bengal, leading to the decreasing of atmospheric humidity from the southeastern to northwestern Plateau.
高原地区比湿值显著的日变化现象，表现为傍晚时比湿值比清晨显著升高，大气水汽含量增加，尤其是在高原的南部地区。
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Firstly, we used the Raman scattering method which can calibrate in real time to measure the O2 (a1 Δ) yield of SOG for the first time in China. The measurement relative error is less than 8%. Based on the data from the experiments, we report the results that the diluent category and ratios influence the O2 (a1 Δ) yield. The relationship of P-τ values and the O2 (a1 Δ) yield of this SOG were given. The effects of distance and bypass of gas transportation on the O2 (a1 Δ) yield are investigated. Secondly, the chlorine utilization was measured by using Raman spectroscopy simultaneously when the O2 (a1 Δ) yield was measured. This method originated with us. The result about the chlorine utilization is coincident with other theoretic and experimental conclusions. The relationship given in this paper between gas stay time in SOG and chlorine utilization offers reference to improve the reaction efficiency and chemical efficiency of COIL. Finally, the partial water vapor pressure at the exit of SOG was measured by absorption spectroscopy. The water vapor fraction and partial pressure have trends changed with the generator total pressure, the diluentratios, and the BHP temperature. These experimental results are very important to improve experimental conditions of SOG, reduce the water vapor fraction, and enhance the output power of COIL.
由侧得的数据得到了加入稀释气体、稀释气体种类以及稀释比例对单重态氧产率的影响，给出了该发生器P一：值与仇产率的关系，还考察了传输距离对仇产率的影响；在国际上首创利用喇曼散射光谱法在侧量产率的同时进行了氯气利用率的检侧，侧试结果与其他理论及实验结果十分相近；给出了气体在发生器中的滞留时间与氯气利用率之间的关系，该结果为提高氧碘化学激光器的反应效率和化学效率提供了参考依据；另外采用了吸收光谱法对发生器出口处的水汽含量进行了测量、得到了水汽分压和百分含量随着发生器压力、稀释气体比例以及BHP温度等的变化情况，该实验结果对于改进发生器工作条件、减少水汽含量、提高氧碘化学激光器的出光功率具有十分重要的指导意义。
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The calculating results of precipitable water by using our empirical expressions agree well with the actual ones.
仅利用地面水汽压计算出的整层大气可降水量和有效水汽含量，同实际情况符合得很好，平均相对误差普遍小于15％。
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Remote Sensing, MODIS, Atmospheric Precipitable Water Vapor, Meteorological Data, Regression Analysis
仿真实验中进行了回归分析，并研究了水汽含量与气象数据之间的相关影响关系。
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The radiosonde data and the surface data are not enough to gain thedistribution of the water vapor in time.
如果在时间分辨率上能够提高，就可以更好的了解空中水汽含量的情况。
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Results show that there is little difference between water vapor content detected by ground-based GPS and that calculated from radiosonde data, and that the water vapor content fits well with the precipitation.
结果表明：GPS反演的水汽含量与探空计算得到的水汽数据具有较好的一致性，同时水汽含量值与地面降水吻合较好。
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Comparisons between GPS/PWV and radiosonde observations show that GPS/PWV retrieved by above method can have the accuracy of millimeter level.
利用地基GPS技术层析水汽三维分布的前提是获取精确的GPS信号斜路径方向的水汽含量。
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It can be gained to the distribution of the water vapor in China.
文中给出了便捷的计算公式，可以快速得到水汽含量的结果。
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The water-vapour transmissivity is measured by aspectral radiometer and the water vapour content is obtained by our calculationprogram of infrared-radiation atmospheric transmissivity.
水汽透过率用辐射计测量，水汽含量由我们自行编制的红外辐射大气透过率计算程序计算。
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The vapor content in the air had a complex influence on aerosol size distribution. The increasing of vapor content in some degree will mainly the effective radius of aerosol particle. But the overlarge vapor content may lead to remove of coarse particles in aerosol.
大气中的水汽含量对气溶胶粒子谱分布的影响较为复杂，当水汽含量在一定范围内增加时，将会增加气溶胶粒子的有效半径，但当水汽含量过大，却又易造成大粒子气溶胶的移出。
- 更多网络解释与水汽含量相关的网络解释 [注：此内容来源于网络，仅供参考]
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absolute humidity：绝对湿度
HW1-22 绝对湿度:(absolute humidity) 绝对湿度是指单位体积空气中所含水汽的质量,单位为g/m3. 空气中水汽含量越大,绝对湿度越大,利用绝对湿度直接表示空气中水汽的含量. HW1-23 相对湿度:(relative humidity) 相对湿度是指空气中实际水汽压与同温度下饱和水汽压之比,
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moisture content：含湿量;水汽含量
moire frenge grating,莫尔条纹光栅 | moisture content,含湿量;水汽含量 | moisture sensor,湿敏元件
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Vapor deposition：汽相沉积
饱和蒸气压:Vapor pressure | 汽相沉积:Vapor deposition | 水汽含量:Water Vapor Content
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dew point：点
HW1-25 露点:(dew point) 在空气中水汽含量不变,且气压一定时,因气温下降,使空气达到饱和时的温度称为露点温度,简称为"露点",单位为℃. 空气中水汽含量愈多,则露点愈高,否则反之. 如果气温高于露点,则说明空气水分尚未饱和,
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dew：露 ","露
贴近地面空气中的水汽冷却后形成露 露(dew)以液滴形式凝结在地面覆盖物体上的凝结现象. 夜间气温下降,越近地面冷却越快,形成与白天相反的下冷上热的温度分布,当地面温度冷却到使贴地面空气中的水汽含量达到饱和时,
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frost：霜冻
并随即变为绕轴心向上的涡流,龙卷中的风总是气旋性...霜冻(Frost) 温度低于0℃的地面和物体表面上有水汽凝结成白色结晶的是白霜,水汽含量少没结霜称黑霜对农作物都有冻害,称霜冻.
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relative humidity：湿度
HW1-22 绝对湿度: (absolute humidity) 绝对湿度是指单位体积空气中所含水汽的质量, 单位为 g/m3.空气中水汽含量越大,绝对湿度越大,利用绝对湿度直接表示空气中水汽的 含量.HW1-23 相对湿度:(relative humidity) 相对湿度是指空气中实际水汽压与同温 度下饱和水汽压之比,
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saturation deficit：饱和差
HW1-24 饱和差:(saturation deficit) 饱和差是指在某一温度下饱和水汽压与当时空气中实际水汽压之差. 饱和差愈大,表示空气愈干燥,否则反之. HW1-25 露点:(dew point) 在空气中水汽含量不变,且气压一定时,因气温下降,使空气达到饱和时的温度称为露点温度,
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water vapor pressure：水汽压
水汽压 水汽压(water vapor pressure) 空气中水汽的分压强. 大气中水汽的含量虽然不多,却是大气中极其活跃的成分. 气象上对水汽含量有很多种测量方法,日常生活中人们最关心
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water vapor：水汽
1)大气吸收与辐射射 红外大气衰减计算主要考虑二氧化碳 CO2 和水汽(water vapor)H2O 的影响. 参见第 4 章"4.4.2.1 大气吸收特性" .特别是水汽,因为变化很大,因此在红外 遥感中, 准确的结果需要对水汽含量和垂直分布进行准确的测量.