When light or energy enters the Earth's atmosphere, some of it is reflected by particles and gases in the atmosphere, bouncing off in different directions. Some of the energy is also absorbed by the atmosphere, where it is converted into heat. This absorption and reflection help regulate the amount of energy that reaches the Earth's surface, contributing to the planet's overall temperature balance.
Carbon dioxide (CO2) makes up approximately 0.04% of Earth's atmosphere.
The gases in the atmosphere
Oxygen makes up roughly 20% of the atmosphere. Carbon Dioxide makes up 0.035% of the atmosphere.
Nitrogen is the gaseous nonmetal that makes up 78 percent of Earth's atmosphere.
the core, crust and atmosphere.
The green color is the result of the light absorption in methane from the planet atmosphere.
Absorption is whereby the digested food substances are entering our bloodstream. Assimilation is whereby the body makes use of these absorbed food substances that has entered our blood
because its reflection
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Reflection of the sun.
Axial reflection.
Reflection of sunlight
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Nitrogen makes up about 79% of the atmosphere.
CO2 makes up approximately 0.03% of Earth's atmosphere
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The bow in a rainbow is caused by the refraction, dispersion, and reflection of light in water droplets in the atmosphere. This process separates the sunlight into its various colors, creating the arch of colors that we see in the sky.