Air pressure.
The temperature decreases with altitude.
it makes no difference you will still weigh the same
In the troposphere, the temperature generally decreases with increasing altitude. This decline occurs at an average rate of about 6.5 degrees Celsius per kilometer (or approximately 3.6 degrees Fahrenheit per 1,000 feet). The decrease in temperature is primarily due to the decreasing pressure and density of air at higher altitudes, which affects how heat is retained. This trend continues until the boundary with the stratosphere, where the temperature begins to increase with altitude.
The transition into the stratosphere is marked by the tropopause, which is the boundary between the troposphere and the stratosphere. This layer is characterized by a significant change in temperature gradient; while the troposphere experiences a decrease in temperature with altitude, the stratosphere exhibits a temperature increase due to the absorption of ultraviolet radiation by the ozone layer. The tropopause varies in altitude, typically reaching higher elevations at the equator and lower at the poles.
In the atmosphere, temperatures increase with altitude in the stratosphere. This layer, which lies above the troposphere, contains the ozone layer that absorbs and scatters ultraviolet solar radiation, leading to a warming effect as altitude increases. Consequently, the stratosphere experiences a temperature inversion, contrasting with the troposphere, where temperatures typically decrease with altitude.
Decrease
Decrease. The source of the river is usually in a mountainous area with a steep gradient.
1,700-foot decrease.
The temperature decreases with altitude.
Temperature decreases with altitude in the mesosphere due to the decrease in atmospheric pressure with height. This is because the mesosphere is above the stratosphere where the ozone layer absorbs incoming solar radiation, leading to a decrease in temperature as altitude increases.
it makes no difference you will still weigh the same
The temperature increases like the stratosphere
The boiling point of water decrease when the altitude increase and the atmospheric pressure decrease.
Environmental lapse rate
As altitude increases, barometric pressure decreases. This is because the air pressure decreases with increasing altitude, as there are fewer air molecules in the atmosphere exerting pressure on a given area.
In the troposphere, temperatures decrease with altitude (air pressure), in the effect known as the adiabatic lapse rate (9.8 °C per thousand feet).
The average temperature decreases by about 3.5F per 1000 feet increase in altitude.