There is no definite boundary between the atmosphere and the outer space. It slowly begins thinner and fades in space.
The average height of Greek individuals is slightly above the global average height.
the environment which has the availability of oxygen it is called aerobic atmosphere and if the availability of oxygen is not there in atmosphere then it is anaerobic type We live in a aerobic atmosphere which has the oxygen available
the atmosphere is important because without the atmosphere the oxygen would escape from our atmosphere into space and without the atmosphere we would all dye because there would be nothing to protect us from the suns heat
His Height is 5' 8.5
Dorthy Height actually did have an affair.
it means the air height.
describe how the height of the tides changes from monday to thursday
To find the percentage of atmosphere above a certain height in kilometers, you can use the barometric formula to calculate the pressure at that height. Then, you can simply divide the pressure at the given height by the pressure at sea level (1013.25 mb) and multiply by 100 to get the percentage of atmosphere above that height.
The scale height of Earth's atmosphere is about 8.5 kilometers. This height plays a crucial role in determining the distribution of gases in the atmosphere, which in turn affects the planet's climate and weather patterns. The scale height influences the temperature, pressure, and density of the atmosphere at different altitudes, leading to variations in weather conditions and climate patterns across the globe.
The Earth's atmosphere declines with altitude.
Density decreases with height in the atmosphere because as you go higher, there is less air above pushing down on the air below, causing it to spread out and become less dense.
The answer depends on whether you want the mass of the atmosphere, the depth (height) or the volume above 8.5 km.
The lowest clouds in the atmosphere are typically found at a height of about 6,500 to 13,000 feet above the ground.
It decreases
The temperature of the atmosphere reduces with height. Mountains are high, thus cooler.
As height increases, the density of the atmosphere decreases. This is because there is less air above pushing down, leading to lower pressure and fewer air molecules per unit volume at higher altitudes.
Scale height is a crucial factor in understanding the composition and properties of an atmosphere. It represents the distance over which the atmospheric pressure decreases by a factor of e (approximately 2.718), and is influenced by the temperature and mass of the atmosphere. A larger scale height indicates a more gradual decrease in pressure with altitude, which can affect the distribution of gases and their interactions within the atmosphere. This information is essential for studying atmospheric dynamics, climate, and the potential habitability of a planet.