Question

How tropopause is diffrent from the stratopause (10 - 20 )answer​

Answer 1

Answer:

As nouns the difference between tropopause and stratopause is that tropopause is the zone of transition between the troposphere and the stratosphere (approximately 13 kilometers) the tropopause normally occurs at an altitude of between 25,000 and 45,000 feet in polar and temperate zones it occurs at 55,000 feet in the tropics while stratopause is in the atmosphere, the boundary between the stratosphere and the mesosphere.

Explanation:

Answer 2

Answer:

Explanation:

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.