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

这云形成之后约一个小时，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形态和运动机理进行了讨论。

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。

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形的冰雹云模式。模式是二维、弹性、非静力、采用地形跟随坐标、变参数冰相微物理过程参数化。

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

这形成之后约一小时，看起来会像是卷系的。

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形态和运动机理进行了讨论。

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。

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.

建立了一于复杂地形的冰雹模式。模式是二维、弹性、非静力、采地形跟随坐标、包含双变参数冰相微物理过程参数化。

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

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.

采用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。

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。

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模式。模式是二维、弹性、、采用地跟随坐标、包含双变参数冰相微物理过程参数化。

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

这云形成之后约一个小时，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.

采用速全流场显示技术和DPIV对空化水翼近壁处的空化云流动形态和运动机理讨论。

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.

（我调整图片的对比和和，然后我通过提升云的正常，建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。

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.

建立一个适用于复杂地形的冰雹云模式。模式是二维、弹性、非静力、采用地形跟随坐标、包含双变参数冰相微物理过程参数化。

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

这云形成之后约个小时，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形态和理进行讨论。

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和度，然后我通过提升云的正常高度，创建Cumulous（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。

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.

建立个适用于复杂地形的冰雹云模式。模式是二维、弹性、非静力、采用地形跟随坐标、包含双变参数冰相微物理过程参数化。

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

这形成之后约一个小时，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.

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

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.

（我图片的对比度和和度，然后我通过的正常高度，创建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。

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.

建立一个适用于复杂地形的冰雹模式。模式是二维、弹性、非静力、采用地形跟随坐标、包含双变参数冰相微物理过程参数化。

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

这形成之后约一个小时，看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对空近壁处空流动形态和运动机理进行了讨论。

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和度，然后我通过提升正常高度，创建了Cumulous（一种在平缓层上生成圆球彩构造）构造基本效果。

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形冰雹模式。模式是二维、弹性、非静力、采用地形跟随坐标、包含双变参数冰相微物理过程参数。

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

这云形成之后约一个小时，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形态和运动机理进行了讨论。

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。

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形的冰雹云模式。模式是二维、弹性、非静力、采用地形跟、包含双变参数冰相微物理过程参数化。

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DPIV对空化水翼近壁处的空化云流动运动机理进行了讨论。

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度，然后我通过提升云的正常高度，创建了Cumulous（一种的云层上生成圆球云团的云彩构造）构造的基本效果。

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、包含双变参数冰相微物理过程参数化。