The energy Earth receives from the Sun is often called solar energy.
The rate at which this energy arrives at Earth is about 174 petawatts ( 1 petawatt = 1,000 trillion watts) at the upper atmosphere. About 30% is reflected back to space.
The sun energy at the Earth's surface is mostly in the visible and near-infrared ranges with a small amount in the near-ultraviolet.
visible light
About 30% of solar radiation entering the Earth's atmosphere is reflected back into space by the Earth's surface and atmosphere, a phenomenon known as albedo. Of this, roughly 10% is reflected directly by the surface, while the rest is reflected by clouds and atmospheric particles. The exact percentage can vary based on factors like surface type and atmospheric conditions.
hydrogen and helium
Radio waves are one example.
Notilucent clouds
Notilucent clouds
Biologist
Oil
Through the atmosphere rather than by the atmosphere, then that would be electromagnetic energy.
Radiant and gravitational Energy.
Circle graph
a data table(NOT FOR SURE)
Atmosphere contains roughly (by volume) 78.09% nitrogen, 20.95%oxygen, 0.93% argon, 0.039% carbon dioxide, and small amounts of other gases.
The UV radiation that reaches the Earth’s surface is mostly UVA and some UVB. Almost half the daytime total of the more harmful UVB radiation is received between the hours of 10 a.m. and 4 p.m. Even on a cloudy day, you can be sunburned by UVB radiation.
There are many energy sources in the earth. Most commonly found deep inside of the earth's crust would be geothermal energy. Geothermal energy is a type of thermal energy that is cost-effective, reliable, sustainable, and most of all, environmentally friendly. It is created by pumping water from the earths core into a turbine, where some of the water is "flashed" into steam. The steam then enters a generator, which helps provide the energy to us.
visible light
A pie chart would be the best type of graph to show the percentage of gases in Earth's atmosphere. Each gas can be represented as a slice of the pie, with the size of each slice corresponding to the percentage of that gas in the atmosphere.