the stratosphere is a layer of the atmosphere that extends above the surface of the earth. It is the third layer above the earth’s crust which is the most important and the one most people are most concerned about. The stratosphere is a layer of air, mostly air that is trapped in the upper atmosphere. Below the stratosphere is a layer, the mesosphere, which is the second layer of the atmosphere.
The stratosphere is the top most layer of the atmosphere. From the ground, it is an opaque blue-green area of the sky, but from a distance of 10,000 miles or so, it appears to be an area of bright white because of the way it is structured. In reality, however, it is a layer of very thin air that extends from the atmosphere’s surface to an altitude of about 40,000 feet.
The stratosphere is very interesting in that it is the uppermost layer of the atmosphere, so it contains the most heat and the coldest air in the atmosphere. Because of this, it is constantly moving away from the Earth, and it is constantly coming back.
The stratosphere is actually very thin air because it is part of a layer of atmosphere that is constantly moving away from the Earth. It is the second layer of atmosphere you can see if you lift your eyes up above the clouds.
The stratosphere is a very thin layer in the atmosphere. It contains only a small amount of air. You can see the stratosphere by looking at the sun’s rays hitting the Earth’s surface. It is much thinner than the upper atmosphere, but it is still a very thin layer. The stratosphere is very interesting because it acts as a barrier to the atmosphere, holding back the temperature of the upper atmosphere. Thus, it has a cooling effect on the Earth.
Some scientists are concerned that the stratosphere could be a source of global warming, but the stratosphere is a good place to look for hints of where the globe is heating up. The stratosphere generally rises up to a maximum height of about 2000 miles above the Earths surface. This is because the stratosphere is not only very thin, but also very dark. On top of that, as the stratosphere gradually cools, it becomes more transparent, allowing us to see the Sun more easily.
These two factors are at work in the stratosphere, where the Earth’s surface is about 1% of the way up. The last few weeks have been a bit of a cold spell for the stratosphere, so that’s why it’s a good place to look for the world’s cooling.
It sounds like a lot of fun. We’re looking for the world that’s about 20 degrees colder than the surface of the Earth at the moment, with the Sun shining at the Earths surface. It’s a bit of a mystery, as scientists can’t explain why our atmosphere is so transparent, but we’ll find out soon enough.
What scientists can explain is how the stratosphere operates. Most of the Earths surface is covered by a layer of clouds that acts like a blanket. The atmosphere above it is also very thick, and if you look at an airplane flying over the stratosphere you can see the thin layers of clouds. This is called the “downwelling” layer, which acts as a blanket for the thinner upper layers.
The key to this is that the atmosphere above the downwelling layer is thin, and the atmosphere above the upper layers thick. The upper layers act as a layer upon layer of the atmosphere until they run into the base of the stratosphere. The layers above this is called the mesosphere, and they act as a blanket for the mesosphere above. Above the mesosphere is the thermosphere, and the lower layers of the atmosphere above this is the ionosphere.