Earth's atmosphere is primarily composed of nitrogen (about 78%) and oxygen (about 21%). The remaining 1% consists of trace gases such as argon, carbon dioxide, and other gases. Water vapor also plays a role in the atmosphere, but its concentration can vary greatly depending on location and weather conditions.
As you travel higher in Earth's atmosphere, the composition of gases changes in terms of their concentration. Oxygen, nitrogen, and argon are the most abundant gases in the lower atmosphere, while the percentage of oxygen decreases and other gases like helium and hydrogen become more prevalent in the upper atmosphere. The overall pressure also decreases with altitude, causing the air to become less dense.
The primary gases in Earth's primitive atmosphere were likely hydrogen, helium, methane, ammonia, and water vapor. Over time, these gases were likely transformed by geological and biological processes into the current composition of the atmosphere.
They slow the loss of heat
The primary source of Earth's atmosphere is outgassing from volcanic activity and the release of gases from Earth's interior. This process began billions of years ago and continues to contribute to the composition of our atmosphere.
A pie chart or a bar graph are commonly used to represent the major gases found in Earth's atmosphere. These types of graphs effectively show the distribution or composition of gases such as nitrogen, oxygen, and carbon dioxide in the atmosphere.
The Chemical Composition of the Earth's atmosphere is important because it holds the Earth together.
78% nitrogen 21% oxygen 1% other gases like argon, carbon dioxide etc.
Gases
they come from earths atmosphere and gases
As you travel higher in Earth's atmosphere, the composition of gases changes in terms of their concentration. Oxygen, nitrogen, and argon are the most abundant gases in the lower atmosphere, while the percentage of oxygen decreases and other gases like helium and hydrogen become more prevalent in the upper atmosphere. The overall pressure also decreases with altitude, causing the air to become less dense.
The primary gases in Earth's primitive atmosphere were likely hydrogen, helium, methane, ammonia, and water vapor. Over time, these gases were likely transformed by geological and biological processes into the current composition of the atmosphere.
As you go higher in the atmosphere the gases start to compose or join together which causes them to change since there is mixture of more than one gas. Sometimes they form a different element when certain gases form.
HIDROGEN
They slow the loss of heat
The primary source of Earth's atmosphere is outgassing from volcanic activity and the release of gases from Earth's interior. This process began billions of years ago and continues to contribute to the composition of our atmosphere.
A pie chart or a bar graph are commonly used to represent the major gases found in Earth's atmosphere. These types of graphs effectively show the distribution or composition of gases such as nitrogen, oxygen, and carbon dioxide in the atmosphere.
The Gas Giants have a deep gas atmosphere and earth have a not so deep atmosphere