it ranges from °c +15.0
−56.5
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.
what is the approximate height and temperature of the troposphere, stratosphere, mesosphere, and thermosphere?
The temperature is relatively constant in the tropopause, remaining around -60°C to -80°C throughout its height. This stable temperature profile forms a boundary separating the troposphere below from the stratosphere above.
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 layer immediately above the tropopause is the stratosphere. The stratosphere is characterized by its stable temperature and the presence of the ozone layer, which absorbs and scatters ultraviolet radiation from the sun.
Decrease. The tropopause marks the boundary between the troposphere and the stratosphere, where temperature generally decreases with altitude. This trend continues through the stratosphere and into the mesosphere until reaching the mesopause where temperatures are at their lowest in the upper atmosphere.
Tpp (tropopause)
No. The tropopause is the boundary between the troposphere and that stratosphere.
The troposphere's topmost boundary is the tropopause.
The tropopause is also known as the "boundary layer."
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.
The stratopause, tropopause, and mesopause are all transitional boundaries in the Earth's atmosphere between different layers. They mark the upper limits of the stratosphere, troposphere, and mesosphere, respectively. These boundaries are characterized by significant changes in temperature and atmospheric properties.