Temperature decreases with increasing altitude, Also air concentration decreases with altitude.
How does liquid pressure vary with depth
How does liquid pressure vary with depth
Air pressure decreases with increasing altitude. This means that as you go higher in the atmosphere, the air pressure becomes lower.
The four main layers of the atmosphere are the troposphere, stratosphere, mesosphere, and thermosphere. They vary in temperature, composition, and altitude. The troposphere is where weather occurs and temperature decreases with altitude. The stratosphere has the ozone layer and temperature increases with altitude. The mesosphere is where meteors burn up and temperature decreases with altitude. The thermosphere is where the auroras occur and temperature increases with altitude due to absorption of solar radiation.
In the atmosphere, pressure generally decreases with higher altitude due to the decrease in air density. Temperature changes can vary depending on altitude and location, but in general, the temperature decreases with increasing altitude in the troposphere, remains relatively constant in the stratosphere, and then increases in the mesosphere and thermosphere.
The temp in the atmosphere approaches -90C at an altitude of 80 kilometers.
No, the Earth's atmosphere varies in thickness depending on factors such as altitude and location. The atmosphere is thickest at the surface and gradually becomes thinner as you move higher up into the atmosphere. Additionally, the atmosphere can also vary in density and composition at different locations on Earth.
Yes, air pressure decreases with altitude because the atmosphere becomes less dense. In contrast, temperature changes can vary with altitude; typically, temperature decreases with altitude, but there are atmospheric layers where temperature may increase, known as inversions.
the temperature in the atmosphere approaches -90 degrees Celsius at an altitude of about answer is 80 kilometers
The greater the altitude, the lower the air pressure.
The apparent molecular weight of a mixture of ideal gases depends on the concentrations of such gases in the Atmosphere. Below 100km altitude the gases in the atmosphere are very well mixed so that the concentration of all the gases does not vary (approximately) with altitude. Therefore the apparent molecular weight would not vary very much at an elevation and at sea level.
The atmosphere becomes less dense with altitude. Atmosphere, thin though it is, has weight, and it is the weight of the air above which compresses the air below it, to greater density.