water vapor absorption是什么意思

网络释义

用法例句

Research on the phase state of the gas-condensate system with water vapour;

含水汽凝析气体系相态特征研究

Relationship between black body temperature and water vapour,precipitation and inversion layer;

水汽、降水和逆温层与卫星红外测值的关系分析

Water vapour in Gas condensate reservoir has an effect on the phase behavior of the Gas condensate system.

凝析气藏中的水汽对凝析气体系相态变化有影响。

The calculated UV energy loss in the actual sky compared to clear sky in 1990 was 64～109 W/m\+2,this UV energy loss attenuated by ozone,“water vapor” and aerosol was 39 1～66 3,21 5～36 5 and 3 2～5 5 W/m\+2 respectively (except December), and yearly averaged values were 48 3, 26 6 and 4 0 W/m\+2 respectively.

计算了 1990年 12个月实际天气比晴天UV能量的减少值在 64～ 10 9W m2 之间 ,这一减少受臭氧、“水汽”、气溶胶等因子的衰减分别为 3 9 1～ 66 3 ,2 1 5～ 3 6 5 ,3 2～ 5 5W m2 (12月除外 ) ,12个月的平均值分别为 48 3 ,2 6 6,4 0W m2 。

Objective:This paper aim to study the influence of water vapor on the catalytic oxidation of CO on PdCl 2-CuCl 2 /activated carbon.

目的 :研究水汽对CO在Pdcl2 CuCl2 /活性炭上催化氧化的影响。

The influence of water vapor on CO photocatalytic-oxidation on the"oxidized"TiO 2 was investigated at the room temperature.

36kPa水汽时 ,光催化氧化CO的活性明显降低 。

Then a synthetic influence on radiation transmission of aerosol and vapor was considered in the radiation transmission model and equations between whole layer transmissibility and planet reflection was built.

本文综合考虑影响大气透过率的气溶胶和水汽因素,并利用中光谱分辨率MOD IS(moderateresolution im aging spectrorad iom eter)数据,在特征参数的空间及时间尺度变化均比较大时,对大气透过率进行了定量反演,并进一步建立了整层大气透过率与行星反照率的关系模型,为近地层大气能见度的遥感监测提供了方法。

The use of the conventional observation in April to October 2001～2004 investigated the character of the specific humidity and vapor flux during moderate precipitation in Akesu area.

利用2001～2004年4～10月的降水量和常规观测资料,分析了发生在阿克苏地区中量以上降水的比湿场和水汽通量场的特征;通过分析T213预报产品中的相对湿度、温度露点差和水汽通量预报场演变与阿克苏地区降水的关系,得到一些有参考价值的物理量预报场特征。

It is found that moisture and strong ascending motion produced typhoon rainstorm directly and the rainstorm has a close relation to vorticity,divergence at 850hPa.

模拟结果表明:充沛的水汽和强烈的上升运动是造成台风暴雨的直接原因,降水与850hPa涡度场、散度场有较好的对应关系。

Tropical cyclones are mainly driven by the energy from the release of latent heat which has a close relation to the moisture supply.

Bilis (0 0 10 )是一个登陆后长久维持的热带气旋 ,其维持期间与一条西南风低空急流水汽通道长时间保持联结。

In this paper number 0216 Typhoon SINLAKU vapour change after it landed is analyzed According to analysis of vapour images, microwave and some normal data, it can be seen that vapour in the lower layer will be cut off first.

本文主要对0216号台风登陆时的水汽变化,利用GMS-5水汽图、NOAA-16-AMSUB微波图以及一些常规资料进行分析阐明台风登陆后低层水汽输送首先被切断,如果后面有热带气旋的水汽流与前一登陆台风的水汽流接通,并与冷锋水汽流相汇合,在内陆将产生更大降水。