0 to 4 percent
The amount of water vapor in atmospheric gases is highly variable. More water vapor is found at lower altitudes, at 30,000 feet there is virtually no water vapor. There is a maximum of 4% water vapor in the atmosphere at any time.
Liquid water, a suitable mix of atmospheric gases, proximity to the sun, the magnetosphere, Earth's size; all make life possible on Earth.
Most of earth's atmosphere is in the lowest layer, the troposphere. Thus most of the gases are within 15 km of the Earth's surface.
The definition of greenhouse gases are any gas with three or more atoms.Answer:The bond lengths between atoms in green house gases allows them to absorb heat energy more easily from sunlight. This is then shared with other atmospheric gases.
Water Vapour
The amount of water vapor in atmospheric gases is highly variable. More water vapor is found at lower altitudes, at 30,000 feet there is virtually no water vapor. There is a maximum of 4% water vapor in the atmosphere at any time.
0 to 4 percent
Carbon Dioxide makes up roughly 96.5% of Venus' atmosphere. Nitrogen makes up another 3.5%, leaving trace amounts of other gases.
Liquid water, a suitable mix of atmospheric gases, proximity to the sun, the magnetosphere, Earth's size; all make life possible on Earth.
The dominant gas on Mercury is oxygen, which makes up 42 percent of the planet's atmosphere, followed by sodium, which makes up 29 percent. Other gases include hydrogen and helium.
None. Water as a liquid makes the oceans. That water contains all the gases in the atmosphere.
0 to 4 percent
Most of earth's atmosphere is in the lowest layer, the troposphere. Thus most of the gases are within 15 km of the Earth's surface.
These gases are nitrogen, oxygen, argon, other noble gases, carbon dioxide, water vapors.
My atmosphere is the same as your atmosphere since we all live on the same planet. Oxygen makes up about 19.5% of the atmosphere.
Nobody makes gases. Gases are natural.
The definition of greenhouse gases are any gas with three or more atoms.Answer:The bond lengths between atoms in green house gases allows them to absorb heat energy more easily from sunlight. This is then shared with other atmospheric gases.