The temperature in the atmosphere decreases as altitude increases. The reason for this is there is less warmth from the surface of the earth reaching the higher altitudes because there are fewer particles of the atmosphere to transfer the heat. The temperature begins to increase, however, around 100km in altitude because of the heat and radiation from the sun.
In the troposphere, temperature decreases with increasing altitude. This decline occurs at an average rate of about 6.5 degrees Celsius per kilometer. As air rises, it expands and cools due to lower atmospheric pressure. This temperature gradient is a key factor in weather patterns and the formation of clouds.
Because of the temperature in the troposphere that decreases as the altitude also lowers, convection only happens on it and not in the stratosphere. Also, because of the warm air from the land that is rising to the troposphere it becomes denser than the air above it that makes convection only happen in the said layer.
It increases as the temperature increases.
at altitude amount of red blood cells increases . [fatima]
In the troposphere, temperature typically decreases with increasing altitude due to the adiabatic cooling effect. In the mesosphere, temperature increases with altitude due to absorption of solar radiation by ozone molecules.
The temperature decreases
Temperature reaches its coldest at the tropopause, which is the boundary between the troposphere below and the stratosphere above. In the stratosphere, the temperature increases with height due to absorption of radiation by ozone.Temperature changes when altitude is in the stratosphere because of one things. It already rises when you climb up in the stratosphere.
The temperature typically decreases as you go up through the troposphere. This decrease in temperature with altitude is known as the lapse rate, and is usually around 6.5°C per kilometer of altitude.
In the exosphere, temperature increases with altitude. This is because the few particles in this layer can absorb large amounts of solar radiation, leading to higher temperatures the higher you go.
Altitude increases.
In the troposphere, temperature generally decreases with increasing altitude at a rate of about 6.5°C per kilometer due to the decrease in air pressure and density with height, known as the lapse rate. This trend continues until the tropopause, where the temperature stabilizes.
As altitude increases, the temperature of air generally decreases at a rate of about 5.4°F per 1000 feet. This is known as the lapse rate, and it occurs due to the decrease in air pressure with increasing altitude.
As altitude increases, atmospheric pressure decreases.
As the altitude of the sun increases, the intensity of sunlight reaching the Earth's surface increases, leading to higher temperatures. This can result in warmer weather and more direct sunlight which is why midday tends to be the warmest part of the day.
The temperature in the atmosphere decreases as altitude increases. The reason for this is there is less warmth from the surface of the earth reaching the higher altitudes because there are fewer particles of the atmosphere to transfer the heat. The temperature begins to increase, however, around 100km in altitude because of the heat and radiation from the sun.
In the troposphere, temperature generally decreases with increasing altitude at a rate of around 6.5°C per kilometer due to the adiabatic cooling effect as air pressure decreases with height. This relationship is known as the environmental lapse rate and defines the temperature profile of the troposphere.