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radiation fog相关的网络例句

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与 radiation fog 相关的网络例句 [注:此内容来源于网络,仅供参考]

To 31, 1996. Using a drop size meter and ADAS, soundings of microphysical structures of radiation fog and soundings of vertical distributions of some related meteorological elements, such as temperature, pressure, moisture, wind and so on were conducted.

利用三用滴谱仪和ADAS对辐射雾的微物理结构及温、压、湿、风等要素的垂直分布进行了探测。

About 86% of fogs occurs at night, of which nearly 69% appears from 02:00 to 08:00 based on diurnal variation of fog. Most of them belong to radiation fog.

从雾的日变化上看,近86%的雾出现在夜间,近69%的雾出现在02-08时,且多为辐射雾。

Fog produced is due to warm and moist air at night made the event of cold condensation is a common autumn and winter radiation fog.

大雾产生的原因是由于暖湿空气夜间遇冷凝结而成,是秋冬季常见的辐射雾。

The results showed that two different nature of the fog (radiation fog and advective fog) have their common features. They are both formed in the zonal circulation.The abundant water vapor and thermal conditions are supplied by the southeast wind in the middle boundary layer. However, there are obvious difference between them .

结果表明:两种性质不同的大雾有其共同的特征,都产生于纬向环流下;中层的东南暖湿气流为大雾的形成提供了充沛的水汽和热力条件。

Based on the liquid water content and optical visibility, the method for determining the parameters of gamma drop size distribution model of fog and clouds are developed, the drop size distributions for advection and radiation fog are obtained with empirical relations of the liquid water content and the visibility, the characteristics of drop size distribution for different kinds of fog are analyzed and discussed.

提出了利用云雾含水量和能见度确定gamma云雾滴尺寸分布的方法,利用雾的含水量和能见度的经验关系,得到了辐射雾和平流雾的雾滴尺寸分布模型,并对不同类型雾的尺寸分布特征进行了分析和讨论。

The advection cooling near the surface by the north-easterly wind is an important condition for the formation of radiation fog, but lead to the demise of advection fog.

但两者存在明显的差异,底层东北风平流降温是辐射雾生成的重要条件,却造成了平流雾的消亡。

Based on the relation between the attenuation ratio and the transmittance of the laser, the variation of the attenuation of 10.6μm laser traveling in advection fog or radiation fog with the visibility and the FOV of the laser receiver is given.

最后,以工作波长为10.6μm的激光为例,利用衰减率与透过率之间的关系,给出了平流雾及辐射雾中激光雾衰减随能见度、接收器视场角等的变化关系。

There are various kinds of sea fog forming in the Arctic Ocean during the summer, radiation fog, vapor fog and advection fog. One of the causes is the existence of the sea ice, which complicates the cushion and therefore the sea air exchange.

北冰洋的夏季能够形成各种类型的海雾:辐射雾、蒸汽雾和平流雾,其重要原因就是因为海冰的存在,使下垫面的性质复杂化,海气交换复杂化。

The surface southeast wind is a condition for the generation of advection fog, but it contributes to the disappearance of radiation fog. The inversion in the radiation fog is thick and strong ,but it is weaker or no inversion in the advection fog. The evolution of stratification from the occurrence to the destruction in the radiation fog is from stable to unstable, while the advection fog from unstable to stable.

底层东南风是平流雾生成的条件,却对应于辐射雾的消亡;辐射雾逆温厚而强,平流雾则为弱的逆温或无逆温;辐射雾生消演变对应于大气层结由稳定发展为不稳定,平流雾则对应于由不稳定趋于稳定。

A 2-D fog numerical model is used to simulate the formation and evolutionof advection-radiation fog of June 9, 1980 in the opening area of the Yangtze River to sea.The effects of advective wind, sea-land circulation on the fog are discussed.

本文用二维非定常数值模式模拟了1980年6月9日长江口地区海雾向上海地区平流而形成的平流雾个例,其中讨论了盛行风、海陆环流对海雾的影响,结果与实况近于一致。

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