These clouds show what Cirrus floccus clouds might look like an hour or so after they form.

这云成之后约个小时，看起来会像卷云系的絮状云。

The cloudy cavitating around a hydronautics foil has been experimentally studied by means of high-speed fluid visualization and DPIV.

采用高速全流场显示技术和DPIV对空化水翼近壁处的空化云流动态和运动机理进行讨论。

A hail cloud model that is two dimensional elastic non-hydrostatic, uses a terrain-following coordinate system and includes double parameters for ice phase microphysics, has been developed.

建个适用于复杂地的冰雹云模。模维、弹性、非静力、采用地跟随坐标、包含双变参数冰相微物理过程参数化。

I adjusted the contrast and saturation of the picture.Then I have created the basic effect of Cumulous formations raising up from the normal height of the clouds.

（我调整图片的对比度和饱和度，然后我通过提升云的正常高度，创建Cumulous（种在平缓的云层上生成圆球云团的云彩构造）构造的基本效果。

These clouds show what Cirrus floccus clouds might look like an hour or so after they form.

这云成之后约一个小时，看起来会像是卷云系的絮状云。

The cloudy cavitating around a hydronautics foil has been experimentally studied by means of high-speed fluid visualization and DPIV.

采用高速全流场显示技术和DPIV对空化水处的空化云流动态和运动机理进行了讨论。

A hail cloud model that is two dimensional elastic non-hydrostatic, uses a terrain-following coordinate system and includes double parameters for ice phase microphysics, has been developed.

建立了一个适用于复杂地的雹云模式。模式是二维、弹性、非静力、采用地跟随坐标、包含双变参数物理过程参数化。

I adjusted the contrast and saturation of the picture.Then I have created the basic effect of Cumulous formations raising up from the normal height of the clouds.

（我调整了图片的对比度和饱和度，然后我通过提升云的正常高度，创建了Cumulous（一种在平缓的云层上生成圆球云团的云彩构造）构造的基本效果。

These clouds show what Cirrus floccus clouds might look like an hour or so after they form.

这云成之后约一个小时，看起来会像是卷云系的絮状云。

The cloudy cavitating around a hydronautics foil has been experimentally studied by means of high-speed fluid visualization and DPIV.

采用高速全流场显示技术和DPIV对空化水翼近壁处的空化云流动态和运动机理进行了讨。

A hail cloud model that is two dimensional elastic non-hydrostatic, uses a terrain-following coordinate system and includes double parameters for ice phase microphysics, has been developed.

了一个适用于复杂地的冰雹云模式。模式是、性、非静力、采用地跟随坐标、包含双变参数冰相微物理过程参数化。

I adjusted the contrast and saturation of the picture.Then I have created the basic effect of Cumulous formations raising up from the normal height of the clouds.

（我调整了图片的对比度和饱和度，然后我通过提升云的正常高度，创了Cumulous（一种在平缓的云层上生成圆球云团的云彩构造）构造的基本效果。

These clouds show what Cirrus floccus clouds might look like an hour or so after they form.

这成之后约一个小时，看起来会像是卷系的絮状。

The cloudy cavitating around a hydronautics foil has been experimentally studied by means of high-speed fluid visualization and DPIV.

采高速全流场显示技术和DPIV对空化水翼近壁处的空化流动态和运动机理进行了讨论。

A hail cloud model that is two dimensional elastic non-hydrostatic, uses a terrain-following coordinate system and includes double parameters for ice phase microphysics, has been developed.

建立了一个适杂地的冰式。式是二维、弹性、非静力、采地跟随坐标、包含双变参数冰相微物理过程参数化。

I adjusted the contrast and saturation of the picture.Then I have created the basic effect of Cumulous formations raising up from the normal height of the clouds.

（我调整了图片的对比度和饱和度，然后我通过提升的正常高度，创建了Cumulous（一种在平缓的层上生成圆球团的彩构造）构造的基本效果。

These clouds show what Cirrus floccus clouds might look like an hour or so after they form.

这云成之后约一个小时，看起来会像是卷云系的絮状云。

The cloudy cavitating around a hydronautics foil has been experimentally studied by means of high-speed fluid visualization and DPIV.

采用高速全流场显示技术和DPIV对空化水翼近壁处的空化云流动态和运动机理进行了。

A hail cloud model that is two dimensional elastic non-hydrostatic, uses a terrain-following coordinate system and includes double parameters for ice phase microphysics, has been developed.

立了一个适用于复杂地的冰雹云模式。模式是二、、非静力、采用地跟随坐标、包含双变参数冰相微物理过程参数化。

I adjusted the contrast and saturation of the picture.Then I have created the basic effect of Cumulous formations raising up from the normal height of the clouds.

（我调整了图片的对比度和饱和度，然后我通过提升云的正常高度，创了Cumulous（一种在平缓的云层上生成圆球云团的云彩构造）构造的基本效果。

These clouds show what Cirrus floccus clouds might look like an hour or so after they form.

这云成之后约一个小时，看起来会像是卷云系的絮状云。

The cloudy cavitating around a hydronautics foil has been experimentally studied by means of high-speed fluid visualization and DPIV.

采用高速全流场显示技术和DPIV对空化水翼近壁处的空化云流动态和运动机理进行了讨。

A hail cloud model that is two dimensional elastic non-hydrostatic, uses a terrain-following coordinate system and includes double parameters for ice phase microphysics, has been developed.

了一个适用于复杂地的冰雹云模式。模式是、性、非静力、采用地跟随坐标、包含双变参数冰相微物理过程参数化。

I adjusted the contrast and saturation of the picture.Then I have created the basic effect of Cumulous formations raising up from the normal height of the clouds.

（我调整了图片的对比度和饱和度，然后我通过提升云的正常高度，创了Cumulous（一种在平缓的云层上生成圆球云团的云彩构造）构造的基本效果。

These clouds show what Cirrus floccus clouds might look like an hour or so after they form.

这云成之后约一个小时，看起来会像是卷云系的絮状云。

The cloudy cavitating around a hydronautics foil has been experimentally studied by means of high-speed fluid visualization and DPIV.

高速全流场显示技术和DPIV对空化水翼近壁处的空化云流态和运进行了讨论。

A hail cloud model that is two dimensional elastic non-hydrostatic, uses a terrain-following coordinate system and includes double parameters for ice phase microphysics, has been developed.

建立了一个适于复杂的冰雹云模式。模式是二维、弹性、非静力、跟随坐标、包含双变参数冰相微物过程参数化。

I adjusted the contrast and saturation of the picture.Then I have created the basic effect of Cumulous formations raising up from the normal height of the clouds.

（我调整了图片的对比度和饱和度，然后我通过提升云的正常高度，创建了Cumulous（一种在平缓的云层上生成圆球云团的云彩构造）构造的基本效果。

These clouds show what Cirrus floccus clouds might look like an hour or so after they form.

这云成之后约一个小时，看起来会像是卷云系的絮状云。

The cloudy cavitating around a hydronautics foil has been experimentally studied by means of high-speed fluid visualization and DPIV.

采用高速全流场显示技DPIV空化水翼近壁处的空化云流动态运动机理进行了讨论。

A hail cloud model that is two dimensional elastic non-hydrostatic, uses a terrain-following coordinate system and includes double parameters for ice phase microphysics, has been developed.

建立了一个适用于复杂地的冰雹云模式。模式是二维、弹性、非静力、采用地跟随坐标、包含双变冰相微物理过化。

I adjusted the contrast and saturation of the picture.Then I have created the basic effect of Cumulous formations raising up from the normal height of the clouds.

（我调整了图片的比度饱度，然后我通过提升云的正常高度，创建了Cumulous（一种在平缓的云层上生成圆球云团的云彩构造）构造的基本效果。

These clouds show what Cirrus floccus clouds might look like an hour or so after they form.

这成之后约一个，起来会像是卷系絮状。

The cloudy cavitating around a hydronautics foil has been experimentally studied by means of high-speed fluid visualization and DPIV.

采用高速全流场显示技术和DPIV对空化水翼近壁处空化流动态和运动机理进行了讨论。

A hail cloud model that is two dimensional elastic non-hydrostatic, uses a terrain-following coordinate system and includes double parameters for ice phase microphysics, has been developed.

建立了一个适用于复杂地冰雹模式。模式是二维、弹性、非静力、采用地跟随坐标、包含双变参数冰相微物理过程参数化。

I adjusted the contrast and saturation of the picture.Then I have created the basic effect of Cumulous formations raising up from the normal height of the clouds.

（我调整了图片对比度和饱和度，然后我通过提升常高度，创建了Cumulous（一种在平缓层上生成圆球团彩构造）构造基本效果。