What kind of light warms the stratosphere

Ethanol is increasingly used as an oxygenate additive for standard petrol, as a replacement for methyl t-butyl ether MTBE , the latter chemical being responsible for considerable groundwater and soil contamination. Ethanol can also be used to power fuel cells and to produce bio diesel. The absorbed energy warms the atmosphere and the surface of the Earth.

What is the main reason mountaintops are so cold? Mountaintops are above much of the greenhouse gas in the atmosphere. The answer is tiny organisms known as cyanobacteria, or blue-green algae. These microbes conduct photosynthesis: using sunshine, water and carbon dioxide to produce carbohydrates and, yes, oxygen. The majority of this production is from oceanic plankton — drifting plants, algae, and some bacteria that can photosynthesize.

Well with more oxygen in the atmosphere everything would catch on fire more easily. With there being even more O2 the atmosphere think of how easy everything would catch fire.

Standard Dry Air is made up of nitrogen, oxygen, argon, carbon dioxide, neon, helium, krypton, hydrogen, and xenon. It does not include water vapor because the amount of vapor changes based on humidity and temperature. A: Air is normally invisible. From space, the atmosphere, which is made of air, looks like a thin blue band because of the way the light passes through it. While water is not visible, it does bend light. This is called refraction.

You can see this when you reach into an aquarium or any body of water. Air looks invisible because it sends very little color to our eyes.

Objects appear to be the color they reflect to our eyes. The stratosphere contains ozone O3 which blocks out harmful UV radiation from the sun as the sun's light passes through the stratosphere.

Ozone depletion in the stratosphere is a big problem. It can be termed as a global problem. If you got one mars and two stratosphere, than how many panes are in a hood, so basically, kind of a big deal. This is the stratosphere. I dont believe you can get an STD from ring-warms, however, you can spread ring-warms to other people. Individuals of oxygen are formed in the stratosphere when oxygen molecules that consist of two oxygen atoms are striked by ultraviolet light.

The ozone layer protects us from UV light. It is present in the stratosphere. What warms the troposphere is the sun light that enters through the ozone layer.

It warms the air. This is called the ozone layer. Ozone absorbs UV radiation, where it would otherwise be harmful to life at the surface. This also warms the stratosphere somewhat. The ozone layer.

The ozone layer in the stratosphere. There is no set size for a light-wave. Ultraviolet waves are the smallest and get larger as the color warms up. Ozone is the chemical that absorbs UV light. Infrared light. Visible light from the Sun. Log in. Meteorology and Weather. Earth Sciences. Study now. See Answer. Best Answer. Study guides. Global Warming 20 cards. What resources do you have today that affect the economy positively. Because of this temperature stratification, there is little convection and mixing in the stratosphere, so the layers of air there are quite stable.

Commercial jet aircraft fly in the lower stratosphere to avoid the turbulence which is common in the troposphere below. The stratosphere is very dry; air there contains little water vapor. Because of this, few clouds are found in this layer; almost all clouds occur in the lower, more humid troposphere. Polar stratospheric clouds PSCs are the exception. PSCs appear in the lower stratosphere near the poles in winter.

They are found at altitudes of 15 to 25 km 9. They appear to help cause the formation of the infamous holes in the ozone layer by "encouraging" certain chemical reactions that destroy ozone. PSCs are also called nacreous clouds.

Air is roughly a thousand times thinner at the top of the stratosphere than it is at sea level. Because of this, jet aircraft and weather balloons reach their maximum operational altitudes within the stratosphere. Due to the lack of vertical convection in the stratosphere, materials that get into the stratosphere can stay there for long times.