The Water Droplet's Journey

On the first day, fluffy white clouds drifted in the atmosphere from the height of the earth to the height. Living in the clouds, family of water droplets, meaning and life of life. As far as I can remember, I spent a few days laying on my back and relaxing to absorb the sun's warm light. One day I put the usual place under the sun, but the light did not look so bright. In fact, as time went on, it gradually became dark, clouds were beat up hard, and Droplet felt as if he could get too heavy to move.

It is filled with a quiet and dull atmosphere. Before the pouring begins, I do not know how much water is contained in the clouds. As the waterdrop of the shower increases, a drop of rain falls on the head. Lightning and thunder covered the sky. Many people hesitate to continue their journey or to avoid the storm; umbrellas can only provide so much protection against wind speed and stinging raindrops.

When steam rises in the atmosphere, small water droplets are formed cold in the sky through a process called dew condensation. These water droplets constitute clouds. When they grow big enough they eventually become too heavy to stay in the air and fall to the ground like rain, snow and other kinds of rainfall. Most of the precipitation that falls is part of the ocean, or part of the river, lake, stream, which ultimately flows into the ocean. Some snowfall will stay on the ground as a frozen mountain glacier or as part of ice covering Greenland and Antarctica. Groundwater is often mined in wells and supplies water to farms, towns and cities.

In the cloud there is a balance between the condensation of water vapor to form water droplets and the evaporation of the droplets to form water vapor. This process can be seen in the form of changing clouds. If condensation exceeds evaporation, precipitation tends to occur. Rainfall is the reduction of water and shape and shape from the atmosphere to the surface of the earth. Examples of precipitation include rain, snow, sleeves, and hail. The air mass temperature determines how much air the air can hold. Humidity is a measure of the amount of water vapor in the air and is reported as the maximum amount of water vapor that air can carry at a particular temperature. At 100% humidity, air reaches its water vapor capacity and can no longer be transported. When the humidity becomes 100%, water vapor molecules gather and liquid water is produced. We often see this happening with rain and rain