Atmospheric physics is the application of physics to the study of the atmosphere.

The troposphere (lower atmosphere) is the densest layer of the atmosphere.

BC We enter the Martian atmosphere.

This is the atmosphere.

Above the level of the photosphere is the stellar atmosphere.

Air pollution atmosphere

And that is because of the atmosphere.

Carbon goes back to the atmosphere.

Imagine for a second that the Earth is a soccer ball.

Or will the biosphere stabilize?

What would the atmosphere look like?

a chemical reaction within the atmosphere.

Correct for atmospheric refraction

Correct for atmospheric refraction?

It enters the atmosphere of Mars.

Volcanoes eject aerosols into the atmosphere.

Well, you guess, that the atmosphere is, you know, gas.

But Mars' atmosphere is about 100 times thinner than Earth's so heat from the sun can easily escape.

Correct coordinates of objects for the effects of the atmosphere

The airplane is exposed to the atmosphere for the first time.

We also use a lot of the atmosphere for agriculture.

The atmosphere's much more complicated.

Most of the oxygen in the atmosphere is generated by the sea.

And outside the Earth's atmosphere, a good deal faster.

The simulated atmosphere included water, methane, ammonia and molecular hydrogen all molecules still found in the atmosphere of Jupiter.

Report of the Secretary General on air pollution atmosphere

An inch? Do we actually breathe the same air that he, Marilyn Monroe, Charles Darwin, or Genghis Khan did?

left Earth, got above the atmosphere and had seen the horizon bend back on itself, that we could understand our planet as a limited condition.

Man destroys the oceans, the fish, the atmosphere and one another.

And that atmosphere is very as dense as our own atmosphere.

We dropped a probe in the atmosphere of Titan.

Green house gases are essential for our survival.

We are now entering the atmosphere of Altair4.

Whatever they do, the atmosphere is strangely discolored.

A paleoatmosphere (or palaeoatmosphere ) is an atmosphere, particularly that of Earth, at some unspecified time in the geological past.

The index is derived from the stability (temperature difference between different levels of the atmosphere) and moisture content (dew point depression) of the lower atmosphere.

Many methods of atmospheric engineering have been proposed.

The vanishing Arctic sea ice also affects the atmosphere.

Structure, growth and development Most of the solid material in a plant is taken from the atmosphere.

It arose out of concerns for the state of the atmosphere in the 1960s.

The second, preservation of the security and safety of satellites in orbit.

Here's the stratosphere cooler.

We were trying to stop carbon from going into the atmosphere.

He succeeds getting to 100,000 feet, leaving the atmosphere, seeing a thin blue line of space.

The atmosphere is about 80 N2 and 20 O2. Scientists have worked out that Earth's atmosphere weighs about 5 x 10 21 g.