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No, the changes are far more gradual and are seasonal rather than day to day
As altitude increases, temperature generally decreases in the troposphere, leading to a reduction in atmospheric pressure and density. The composition of the atmosphere also changes slightly with altitude, as the concentration of lighter gases like oxygen decreases more rapidly than heavier gases. In higher layers, such as the stratosphere, temperature can increase again due to the absorption of solar radiation by ozone. Overall, these variations are essential for understanding weather patterns and atmospheric behavior.
The temperature in the stratosphere hardly changes with altitude, making it a stable atmospheric layer. This is due to the absorption of ultraviolet radiation by the ozone layer.
The temperature at which a liquid changes into a gas is called the boiling point.
Changes in physical properties: cooling is temperature decrease caused by heat exchange
false
It reappears when the atmospheric temperature changes
The boundaries between atmospheric layers are determined by changes in temperature and composition. For example, the boundary between the troposphere and stratosphere is defined by the tropopause, where temperature begins to increase with altitude. The boundaries between layers are also influenced by the mixing of gases and other atmospheric properties.
No, the changes are far more gradual and are seasonal rather than day to day
The temperature at which water changes into vapor is known as the boiling point, which is 100 degrees Celsius at standard atmospheric pressure.
It depends what type of matter it is, as well as, atmospheric pressure.
the temperature
As altitude increases, temperature generally decreases in the troposphere, leading to a reduction in atmospheric pressure and density. The composition of the atmosphere also changes slightly with altitude, as the concentration of lighter gases like oxygen decreases more rapidly than heavier gases. In higher layers, such as the stratosphere, temperature can increase again due to the absorption of solar radiation by ozone. Overall, these variations are essential for understanding weather patterns and atmospheric behavior.
The temperature at which the vapor pressure of the liquid equals the atmospheric pressure is called THE BOILING POINT.
Henryk Arctowski has written: 'On solar-constant and atmospheric temperature changes' -- subject(s): Solar radiation, Atmospheric temperature 'The bathymetrical conditions of the Antarctic regions'
Freezing point is a physical property. It is the temperature at which a substance changes from a liquid to a solid state under standard atmospheric pressure. Physical changes involve a change in state without altering the chemical composition of a substance.
Boiling point