your mother
Tpp (tropopause)
The tropopause is also known as the "boundary layer."
The upper limit of the troposphere is called the tropopause.
No, the temperature near the tropopause is typically colder than the temperature near the Earth's surface. This is because the tropopause marks the boundary between the troposphere and the stratosphere, where temperature generally decreases with altitude due to the way gases in the atmosphere absorb and emit radiation.
Stratosphere. (From a kid from mr salems class!!!)
The temperature in the tropopause remains relatively constant due to the balance between the warming effect of solar radiation in the stratosphere and the cooling effect of altitude. As one ascends in the troposphere, temperature decreases, but once reaching the tropopause, the transition to the stratosphere occurs where ozone absorbs ultraviolet radiation, leading to a warming effect that offsets any further cooling. This creates a stable layer where temperatures level off, resulting in a constant temperature profile at that altitude.
Tpp (tropopause)
No. The tropopause is the boundary between the troposphere and that stratosphere.
Yes, the temperature stops decreasing at the top of the troposphere, known as the tropopause. The tropopause marks the boundary between the troposphere and the stratosphere, and beyond this point, temperature remains relatively constant or may even increase with altitude.
The tropopause is also known as the "boundary layer."
The troposphere's topmost boundary is the tropopause.
The upper limit of the troposphere is called the tropopause.
The tropopause is the boundary layer in the Earth's atmosphere from the troposphere below and the stratosphere above.
The stratosphere.
Tropopause
No, the temperature near the tropopause is typically colder than the temperature near the Earth's surface. This is because the tropopause marks the boundary between the troposphere and the stratosphere, where temperature generally decreases with altitude due to the way gases in the atmosphere absorb and emit radiation.
There are two main layers of the atmosphere beneath the tropopause: the stratosphere and the troposphere. The stratosphere lies just below the tropopause and extends down to about 31 miles (50 kilometers) above Earth's surface, while the troposphere is the layer closest to Earth's surface and extends up to the tropopause.