The difference in the distance to the Sun is irrelevant - it is 150 million kilometers away. Much more significant are other effects, for example the tendency of rising air to cool.
The boundary between the stratosphere and the mesosphere is typically located around 50 kilometers (31 miles) above the Earth's surface. This region is known as the stratopause. In this region, temperatures start to decrease with increasing altitude, marking the transition from the warmer stratosphere to the cooler mesosphere.
Yes, the mesosphere is colder than the stratosphere. Temperatures in the mesosphere can drop as low as -90 degrees Celsius (-130 degrees Fahrenheit) due to its higher altitude and distance from the warming effects of the Earth's surface, while the stratosphere is warmer due to the presence of the ozone layer.
The main difference between the four layers of the atmosphere (troposphere, stratosphere, mesosphere, thermosphere) is their temperature profile. The troposphere gets colder with altitude, the stratosphere gets warmer with altitude, the mesosphere gets colder with altitude again, and the thermosphere experiences high temperatures due to absorption of solar radiation.
The stratosphere is the second major layer of Earth's atmosphere, just above the troposphere, and below the mesosphere. It is stratified in temperature, with warmer layers higher up and cooler layers farther down. This is in contrast to the troposphere near the Earth's surface, which is cooler higher up and warmer farther down. The border of the troposphere and stratosphere, the tropopause, is marked by where this inversion begins, which in terms of atmospheric thermodynamics is the equilibrium level. The stratosphere is situated between about 10 km (6 miles) and 50 km (31 miles) altitude above the surface at mid-latitudes, while at the poles it starts at about 8 km (5 miles) altitude.
The temperature typically rises in the stratosphere because of the absorption of ultraviolet solar radiation by ozone molecules. This absorption leads to the heating of the stratosphere, creating a temperature inversion where it gets warmer with altitude.
The boundary between the stratosphere and the mesosphere is typically located around 50 kilometers (31 miles) above the Earth's surface. This region is known as the stratopause. In this region, temperatures start to decrease with increasing altitude, marking the transition from the warmer stratosphere to the cooler mesosphere.
Yes, the mesosphere is colder than the stratosphere. Temperatures in the mesosphere can drop as low as -90 degrees Celsius (-130 degrees Fahrenheit) due to its higher altitude and distance from the warming effects of the Earth's surface, while the stratosphere is warmer due to the presence of the ozone layer.
The main difference between the four layers of the atmosphere (troposphere, stratosphere, mesosphere, thermosphere) is their temperature profile. The troposphere gets colder with altitude, the stratosphere gets warmer with altitude, the mesosphere gets colder with altitude again, and the thermosphere experiences high temperatures due to absorption of solar radiation.
Yes, the upper stratosphere is generally colder than the lower stratosphere. This is because the stratosphere's temperature increases with altitude due to the absorption of solar radiation by ozone in the lower stratosphere. However, the temperature starts to decrease again in the upper stratosphere due to the cooling effect of gases like ozone and molecular oxygen.
The stratosphere is the second major layer of Earth's atmosphere, just above the troposphere, and below the mesosphere. It is stratified in temperature, with warmer layers higher up and cooler layers farther down. This is in contrast to the troposphere near the Earth's surface, which is cooler higher up and warmer farther down. The border of the troposphere and stratosphere, the tropopause, is marked by where this inversion begins, which in terms of atmospheric thermodynamics is the equilibrium level. The stratosphere is situated between about 10 km (6 miles) and 50 km (31 miles) altitude above the surface at mid-latitudes, while at the poles it starts at about 8 km (5 miles) altitude.
The south is usually warmer because it is closer to the equator. The closer to the equator the more direct the suns waves are which makes it warmer. In the summer though they are about the same because the Earth is tilted which makes it warmer in the north because it has more direct rays of sunlight.
The layers Earth's Atmosphere from closest to farthest: Troposphere, Stratosphere, Mesosphere, Thermosphere, Exosphere. (It is often argued whether the Exosphere is actually part of the atmosphere or not. The amount of scientists who believe and don't is about 50-50.)As you ascend into the sky, the atmospheric temperature follows a cold-hot pattern.The temperature in the Troposphere is cooler as you go up. Above the Troposphere is the Stratosphere. The Stratosphere is significantly warmer and more dry than the Troposphere. Above the Stratosphere is the Mesosphere. The Mesosphere is the coldest layer of the Atmosphere at negative 130 degrees Fahrenheit. Above the Mesosphere is the Thermosphere. The Thermosphere is the hottest layer of the Atmosphere at approximately 2,700 degrees Fahrenheit. Above the Thermosphere is the Exosphere. The Exosphere is extremely thin and where the Atmosphere merges with outer space. It's comprised of widely dispersed particles of Hydrogen and Helium.
Warmer
The stratosphere is the second major layer of Earth's atmosphere, just above the troposphere, and below the mesosphere. It is stratified in temperature, with warmer layers higher up and cooler layers farther down. This is in contrast to the troposphere near the Earth's surface, which is cooler higher up and warmer farther down. The border of the troposphere and stratosphere, the tropopause, is marked by where this inversion begins, which in terms of atmospheric thermodynamics is the equilibrium level. The stratosphere is situated between about 10 km (6 miles) and 50 km (31 miles) altitude above the surface at moderate latitudes, while at the poles it starts at about 8 km (5 miles) altitude.--Wikipedia
In general, temperatures decline as we increase our altitude. The higher we go, the colder it is. The answer to the question about whether temperatures get warmer as we move from the lower stratosphere on up is, "No."
as you get closer it gets warmer and as you go farther away it gets colder
The places closer to the equater are warmer.