Nitrogen 78%
The most abundant element in the troposphere is nitrogen, making up about 78% of the atmospheric composition. Oxygen is the second most abundant element in the troposphere, making up about 21% of the atmosphere.
Nitrogen 78%
The two most abundant elements in the troposphere are nitrogen and oxygen. Nitrogen makes up about 78% of the atmosphere, while oxygen makes up about 21%.
The troposphere is the most abundant layer in Earth's atmosphere. It is where most weather phenomena occur and contains about 75% of the atmosphere's mass.
Troposphere: nitrogen Lithosphere and hydrosphere: oxygen
This layer of the atmosphere is troposphere.
Oxygen content is highest in the troposphere, which is the lowest layer of Earth's atmosphere. Approximately 20% of the troposphere's gas composition is oxygen, making it the layer where oxygen is most abundant.
The gases that make up the troposphere are: Nitrogen 78% Oxygen 21% Argon 1% Carbon Dioxide 0.03% Other gases less than 1%
The most abundant gases in the troposphere are nitrogen (approximately 78%), oxygen (around 21%), and argon (about 0.93%). Additionally, trace amounts of carbon dioxide, water vapor, and other gases can also be found, with water vapor varying significantly based on temperature and humidity. Together, these gases play crucial roles in weather, climate, and the overall composition of the Earth's atmosphere.
The most abundant gas in the lower atmosphere, or troposphere, is nitrogen, which makes up about 78% of the air we breathe. Oxygen follows as the second most abundant gas, comprising about 21%. Other gases, such as argon, carbon dioxide, and trace gases, make up the remaining percentage. This composition is crucial for supporting life and various atmospheric processes.
The troposphere gases, from most abundant to least abundant, are nitrogen (N2), oxygen (O2), water vapor (H2O), argon (Ar), and carbon dioxide (CO2). Nitrogen makes up about 78% of the atmosphere, oxygen about 21%, and the others in trace amounts.
The sun is the most useful cause for the heating of the troposphere