Question

difference between tropopause and stratopause give atleast five points each of them

Answer 1

The differences between the stratosphere and the troposphere include:

The troposphere is the lowest level of the atmosphere, so it is in contact with the Earth’s surface. In contrast, the stratosphere is located above the troposphere, so it is not in contact with the Earth’s surface.

Humans live in the troposphere, not the stratosphere. People only spend time in the stratosphere is when they are traveling through it on an airplane, or flying through it while riding in a rocket.

The air density and air pressure are much lower in the stratosphere. In fact, stratospheric air is too thin for people to be able to survive without pressurized air to breathe.

On average, the troposphere is warmer than the stratosphere.

Meteorological weather primarily occurs in the troposphere and does not occur in the stratosphere. For example, it only rains and snows in the troposphere. Also, virtually all clouds are located in the troposphere.(The only exception are polar stratospheric clouds which only occur in the winter near the Earth’s poles).

There are differences between tropospheric and stratospheric chemistry. For example, the ozone layer only occurs in the stratosphere. Also, smog and surface level pollution only occur in the troposphere. Additionally, the concentration of stratospheric water vapor, i.e., humidity, is always very low; in contrast, tropospheric humidity can vary quite a bit from the very high humidities in the tropics and extremely low humidities in the polar regions.

Answer 2

Tropopause

• The tropopause layer is that the boundary within the Earth's atmosphere between the troposphere and the stratosphere.
• The troposphere layer is that the lowest layer of Earth's atmosphere. Weather happens within the layer, and the majority clouds area unit found during this layer. following layer up is that the layer.
• The temperature decreases above within the troposphere layer, wherever less heat from the surface warms the air, the temperature drops.
• The temperature typically decreases with increasing height up to the tropopause layer
• Thus, tropopause layer  is sixteen kilometer high over Australia at year-end, and between twelve - sixteen kilometer at midyear, being lower at the upper latitudes. At latitudes higher than sixty , the layer is a smaller amount than nine -10 kilometer higher than ocean level; the bottom is a smaller amount than eight kilometer high, higher than continent and higher than geographic region and northern North American country in winter.

Stratopause

• On Earth, the stratopause is fifty to fifty five kilometres high higher than the surface. The air pressure is around 1/1000 of the pressure put off level.
• The temperature within the stratopause is -15 degrees Anders Celsius
• The layer acts as a filter for the shorter wavelength and extremely unsafe UV (UVR) from the sun, protective life on Earth from its probably harmful effects.
• The layer is stratified in temperature, with hotter layers higher and cooler layers nearer to the Earth; this increase of temperature with altitude could be a results of the absorption of the Sun's UV by the layer.
• The stratosphere layer is lush in gas, a sort of O molecule that absorbs the sun's UV and uses it to heat this layer within the atmosphere. fascinating layer Facts: The layer is one in every of 5 layers of the atmosphere.