Energy packets interact with the clouds to cool the planet is given below.
Step-by-step explanation:
1. Solar radiation is reflected by the clouds' surfaces. ... The reflection helps to keep the heat in the atmosphere, while the passing through allows the heat to escape the Earth system.
2.Low, thick clouds primarily reflect solar radiation and cool the surface of the Earth. High, thin clouds primarily transmit incoming solar radiation; at the same time, they trap some of the outgoing infrared radiation emitted by the Earth and radiate it back downward, thereby warming the surface of the Earth.
3.Air in the atmosphere acts as a fluid. The sun's radiation strikes the ground, thus warming the rocks. As the rock's temperature rises due to conduction, heat energy is released into the atmosphere, forming a bubble of air which is warmer than the surrounding air. This bubble of air rises into the atmosphere.
4.Once in the Earth's atmosphere, clouds and the surface absorb the solar energy. The ground heats up and re-emits energy as longwave radiation in the form of infrared rays. Earth emits longwave radiation because Earth is cooler than the sun and has less energy available to give off
5.Clouds both cool and warm the earth's surface. They cool the earth by bouncing sunlight back into the atmosphere; they warm it by bouncing light down to Earth's surface. The net cloud effect is what scientists need to obtain. To do that, they measured the total amount of sunlight in a cloudy day.