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层云

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Noctilucent clouds are ragged extensions of a more widespread and more permanent layer which forms over the summer polar area at the mesopause.

夜光云是在夏季极地中圈顶之上形成的更广泛更持久的层的参差不齐的延伸。

Summer high temperature season, especially in highly alkaline (pH 8 ~ 9.5) and high-nitrogen low-phosphorus breeding water body, often there will be kind of the large population of blue-green algae in the water to form a layer of green, cloud porphyritic, ribbon objects , commonly known as "water-hua."

盛夏高温季节,尤其是强碱性(pH 8~9.5)和高氮低磷的养殖水体,往往会出现蓝绿藻类的大量繁殖,在水面形成一层绿色、云斑状、带状的物体,俗称&水华&。

Most lightning occurs within cumulonimbus clouds like these, but it can also be released from wide, layered formations called stratiform clouds.

大多数雷击都发生在积雨云云层像这些,但是它也可以释放出广泛的,分层次的构成所谓的层状的云。

Most lightning occurs within cumulonimbus clouds like these, but it can also be released from wide, layered formations called stratiform clouds.

最多的闪电发生在积雨云之内,但是它也能释放从广阔的,分层的构造叫做层状云。

The average rainfall rate of stratiform rain and convective rain has a considerable increase with the intensification of typhoon.

层状云降水和对流性降水的平均雨强均随台风强度加强有较大的增幅。

Results show that stratiform rain occupies more area and contributes more rainfall to the total than convective rain does at the 3 times.

结果表明:三个时次层状云降水在象素数量上及对总降水量的贡献上均比对流性降水大。

In terms of the data of stratiform could microphysical structure from airborne particle measurement system in 1997 in Liaoning province,the characteristics of cloud droplet spectrum,particle number concentration,temperature and water content of particle in the horizontal level were discussed.

根据1997年在辽宁利用机载粒子测量系统获取的探测资料,探讨了层状云中云滴谱、粒子数浓度在水平方向上的分布变化,并分析了温度、粒子含水量在水平方向上的变化特征。

Precipitation of convection will diminish, while that of stratiform clouds will maintain, so the mixture clouds can bring stronger precipitation in a large area.

对流云的降水量不断减小,而层状云的降水不断维持,带来了大面积持续时间很长的降水。

In vertical structure, the profiles of convective rain and stratiform rain are obviously different while the profiles of their own rain type among the 3 times have little difference.

在垂直结构上,对流性降水与层状云降水的廓线有明显的差别,而两类降水廓线各自在三个时次均差别不大。

The profile of stratiform rain can be divided into four sects, and there is a distinct bright band structure near the altitude of 4.5km.

层状云降水廓线大致分为四段,在4.5km高度附近表现出明显的亮带结构。

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