关于雨的形成的英语小短文

关于雨的形成的英语小短文
关于雨的形成的英语小短文

关于雨的形成的英语小短文
It is raining now and the rain will go to the river and run to the sea.The water in the sea will becone cloud under the sun and the cloud moves to our sky.the cloud falls down and it is raining now.You see,you are in the water,in the river,in the sea and in the cloud.

It is raining now and the rain will go to the river and run to the sea. The water in the sea will becone cloud under the sun and the cloud moves to our sky. the cloud falls down and it is raining now....

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It is raining now and the rain will go to the river and run to the sea. The water in the sea will becone cloud under the sun and the cloud moves to our sky. the cloud falls down and it is raining now. You see, you are in the water, in the river, in the sea and in the cloud.
外面下雨啦，雨水变成了河流流到大海里去了，大海里的水在太阳的照耀下变成云朵了，云朵飘过来了，云朵掉下来了，就是外面在下雨了。你看呀，我们在雨里，在河流里，在大海里，在云朵里。

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It is raining now and the rain will go to the river and run to the sea. The water in the sea will becone cloud under the sun and the cloud moves to our sky. the cloud falls down and it is raining now. You see, you are in the water, in the river, in the sea and in the cloud.
^____^KO了!

在水云中，云滴都是小水滴。它们主要是靠继续凝结和互相碰撞并合而增大的。因此，在水云里，云滴要增大到雨滴的大小，首先需要云很厚，云滴浓密，含水量多，这样，它才能继续凝结增长；其次，在水云内还需要存在较强的垂直运动，这样才能增加多次碰撞并合的机会。而在比较薄的和比较稳定的水云中，云滴没有足够的凝结和并合增长的机会，只能引起多云、阴天，不大会下雨。
在各种不同的云内，其云滴大小的分布是各不相...

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在水云中，云滴都是小水滴。它们主要是靠继续凝结和互相碰撞并合而增大的。因此，在水云里，云滴要增大到雨滴的大小，首先需要云很厚，云滴浓密，含水量多，这样，它才能继续凝结增长；其次，在水云内还需要存在较强的垂直运动，这样才能增加多次碰撞并合的机会。而在比较薄的和比较稳定的水云中，云滴没有足够的凝结和并合增长的机会，只能引起多云、阴天，不大会下雨。
在各种不同的云内，其云滴大小的分布是各不相同的，造成云滴大小不均的原因就是周围空气中水汽的转移以及云滴的蒸发。使云滴增长的因素是凝结过程和碰撞并和过程，在只有凝结作用的情况下，云滴的大小是均匀的，但由于水汽的补充，使某些云滴有所增长，再加上并和作用的结果，就使较大的云滴继续增长变大成为雨滴。雨滴受地心引力的作用而下降，当有上升气流时，就会有一个向上的力加在雨滴上，使其下降的速度变慢，并且一些小雨滴还可能被带上去。只有当雨滴增大到一定的程度时，才能下降到地面，形成降雨。
In waterclouds, cloud droplets are small drops. They mainly rely on continue condensation and collisions compounded. Therefore, in the cloud droplets, aiming to increase the size of the rain, the first to need clouds and thick, thick clouds drop, so, moisture content, it will continue to increase condensation, Secondly, there still needs in waterclouds within the strong vertical movement, so as to increase the opportunities and incorporated many collisions. But in comparison with relatively stable thin cloud droplets, no waterclouds enough condensation and pushed the growth opportunities, can cause cloudy, cloudy, no rain.
In different kinds of clouds, the size distribution of cloud droplets are different, the causes of cloud droplets size is around in the air and moisture transfer of cloud droplets of evaporation. That cloud droplets growth factor is setting process and the collision and process, only to condense in the circumstances, the size of the cloud droplets are uniform, but due to some of the supplement, vapor cloud droplets increased, plus, and make greater cloud droplets continue to grow bigger be rain. Suffer the effect of gravity raindrop falls, when updraft, will have an upward force in rain, make its slow down, and a little rain may also be brought up. Only when raindrops increases to a certain extent, to fall to the ground, the formation of rainfall.

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现在的雨将走去和或海中。