Describe the water cycle process starting from an afternoon thunderstorm. There are many different variations that could happen.

The water cycle is the continuous movement of water within the  atmosphere and surface and it is described by five major steps.

The given problem is based on the concept of water cycle. The continuous movement of water within the Earth and its atmosphere, is known as water cycle. The water cycle basically involves five steps:

So when a thunderstorm occurs it helps in completing the precipitation process by enabling the release of water vapor stored up in the atmosphere to fall on the ground as rain.

After this, the water runoffs to the surface of the ground, on plants, into rocks, rivers, and lakes.  Next, the Infiltration process enables the water on the ground surface to enter the soil some of which becomes groundwater.

The cycle begins again as the evaporation and transpiration process begins, where the groundwater as a result of heat from the sun is taken back into the atmosphere, while water in plants by means of transpiration goes back into the atmosphere.  It then condenses and falls back as precipitation again.

Thus, we can conclude that the water cycle is the continuous movement of water within the atmosphere and surface and it is described by five major steps.

Learn more about the water cycle here:

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Explanation:

The water cycle basically involves five steps:

So when a thunderstorm occurs it helps in completing the precipitation process by enabling the release of water vapor stored up in the atmosphere to fall on the ground as rain.

After this, the water runoffs to the surface of the ground, on plants, into rocks, rivers, and lakes.

Next, the Infiltration process enables the water on the ground surface to enter the soil some of which becomes groundwater.

The cycle begins again as the evaporation and transpiration process begins, where the groundwater as a result of heat from the sun is taken back into the atmosphere, while water in plants by means of transpiration goes back into the atmosphere.

It then condenses and falls back as precipitation again.

they should be similar or the same

fgravity=10x10=100n case 1

fgravity=30x20=600n case 2

6 times more