You searched for: “atmosphere
atmosphere (s) (noun), atmospheres (pl)
1. The envelope of gases surrounding the Earth and other celestial bodies which is held by the force of gravity: The atmosphere of the Earth is being affected by pollution caused by the increased exploitation of natural resources.

The atmosphere consists of four distinct layers whose boundaries are not precise:

  • The "troposphere" (extending from sea level to about 5-10 miles [10 to 20 km] above the earth.
  • The "stratosphere" (up to about 30 miles [50 km]).
  • The "mesosphere" (up to about 60 miles [96 km]).
  • The "thermosphere" (up to about 300 miles or more [480 km]).

The upper region of the troposphere is often regarded as a separate region known as the "exosphere".

2. The gas bound gravitationally to a planet or the pressure of the air on the Earth at mean sea level approximately 14.7 pounds per square inch or 760 millimeters high at 0 degrees Celsius under standard gravity: Through the powerful telescope, the astronomers were able to study the atmosphere of the distant planets.

Although some details about the atmospheres of other planets and satellites are known, only the Earth's atmosphere has been well studied, the science of which is called "meteorology".

3. The outer layers of a star: The atmosphere surrounding the star appears to cause the twinkle effect which romantic couples dream about.
4. A supposed outer envelope of effective influences surrounding various bodies: The atmosphere of the capital city was one of individuals and corporations attempting to influence politicians.
5. Prevailing psychological climate; a pervading tone or mood; a characteristic mental or moral environment; a fascinating or beguiling association or effect: The atmosphere in the office appeared to be edgy as if there were major staff changes anticipated, but no one knew when that would happen.
6. Applied to the background sounds that evoke a particular mood, impression, setting, etc., in a broadcast program, etc.: The atmosphere created by the music was dark and mysterious.
7. The air in any particular place, especially as affected in its condition by heat, cold, purifying or contaminating influences, etc.: The old wood stove was not well maintained and smoked, creating a smoky atmosphere in the cabin.
8. The predominant tone or mood of a work of art, or the pervading quality, effect, or mood, especially as associated with a particular place: Henry lived in a dark old house with a depressing atmosphere.
9. A distinctively exotic or romantic quality or effect: Willy and Gertrude went to an Italian restaurant where there was lots of atmosphere.
This entry is located in the following units: atmo-, atm- + (page 2) sphero-, spher-, -sphere- (page 1)
(Modern Latin: chemical element; from Greek, helios, the sun, first observed in the sun’s atmosphere; gas)
(Greek: rain, rainstorm; showers of rain; aqueous vapor in the atmosphere; precipitation or falling down from the sky of a form of water; such as, rain, snow, hail, sleet, or mist)
Word Entries containing the term: “atmosphere
aerohygrocola (s) (noun), aerohygrocolas (pl): high atmosphere
Those creatures that naturally thrive in high atmospheric humidities.
Earth's Multilayered Atmosphere

There are Layers in Space which Serve as Barriers to Gases and Radiations and so They Protect the Earth from the Many Dangers That Exist in Space

There is a mixture of gases in the atmosphere which is around the earth that is held in place by the earth's gravity.

The invisible mixture of nitrogen, oxygen, argon, carbon dioxide, and water vapor protects our planet from harmful radiation and makes life on earth feasible.

The atmosphere's density decreases with its height or distance from the earth; however, not at a uniform or consistent rate. Above approximately 90 kilometers, or 55 miles, the air is extremely rarefied, but it extends thousands of miles above the earth.

Different layers of atmosphere are distinguished by the levels of their temperatures:

  • The troposphere extends 18 kilometers, or 11 miles, above the earth.

    It is warmed by solar rays re-radiated from earth's surface.

    This causes convection currents that bring changes in the weather.

    Temperature in the troposphere decreases with height to -60°C, -76°F, but in the stratosphere it rises close to the freezing point.

  • The stratosphere, which is just above the troposphere, extends to 50 kilometers, 30 miles.

    It contains ozone, which absorbs ultraviolet rays from the sun.

  • In the next layer above the stratosphere, is the mesosphere, which extends to 80 kilometers, 50 miles, above the earth and it is here that the temperature drops to -113°C, or -173°F.
  • The previous three layers form the lower atmosphere.
  • In the more rarefied upper atmosphere, temperature rises, reaching 227°C, 441°F, even at night where thermosphere and exosphere meet 450 kilometers, 280 miles, above the earth.
  • The upper atmosphere absorbs much of the harmful radiation and as it does this, it produces electrically charged particles called ions.
  • In this region, called the ionosphere, layers of greater ion concentration (the D, E, and F layers) exist, although they vary daily or seasonally.
  • Humans use the the ions to bounce radio waves around the earth.
  • Farther out in the ionosphere are two Van Allen Belts (Inner Van Allen belt and Outer Van Allen belt), which are zones of radiation concentration.
—Compiled from information located at
Reader's Digest Illustrated Encyclopedic Dictionary, Volume One, A-K;
The Reader's Digest Association, Inc.; Pleasantville, New York; page 117.
This entry is located in the following unit: sphero-, spher-, -sphere- (page 7)
ion atmosphere
A cloud-like configuration of ions that are loosely bound around an ion of the opposite charge.
This entry is located in the following units: ion, ion- + (page 1) sphero-, spher-, -sphere- (page 8)
neutral atmosphere
An atmospheric environment which neither oxidizes nor reduces materials that are contained within it.
This entry is located in the following units: neutro-, neuter-, neutr-, neut- + (page 1) sphero-, spher-, -sphere- (page 10)
soil atmosphere, soil air (s)  (noun), soil atmospheres (pl)
In geology, The air occupying the pore or open spaces in soil: Soil atmosphere can be a gas located in the pores or cavities in the soil or, in other words, in the zone of aeration.
This entry is located in the following units: soil- + (page 1) sphero-, spher-, -sphere- (page 11)
Word Entries at Get Words: “atmosphere
atmosphere
1. The thin layer of gasses surrounding the earth that is the medium for weather and climate.
2. An envelope of gas surrounding a planet, star, or other celestial body, where the gravitational field is strong enough to restrain the gases.
This entry is located in the following unit: Geography Terms + (page 1)
atmosphere, standard atmosphere, atm
In physics, a unit of pressure equal to 760 torr, 1013.25 millibars, or 1.01325 x 105 newtons per square meter (the terms used here are located in this unit).

The actual pressure exerted by he atmosphere fluctuates around this value, which is assumed to be standard at sea level and zero degrees centigrade/32 degrees Fahrenheit, and is used when dealing with very high pressures.

This entry is located in the following unit: Measurements and Mathematics Terms (page 2)
(topics about the study of the complex motions and interactions of the atmosphere, including the observation of phenomena; such as, temperature, density, winds, clouds, and precipitation)
Word Entries at Get Words containing the term: “atmosphere
earth's atmosphere
A mixture of gases surrounding the earth and such atmosphere is prevented from escaping because of the pull of gravity.

On earth, atmospheric pressure decreases with altitude and in its lowest layer, earth's atmosphere consists of nitrogen (78%) and oxygen (21%), both in molecular form (two atoms bonded together) and 1% argon.

Small quantities of other gases are important to the chemistry and physics of the earth's atmosphere, including water and carbon dioxide.

The earth's atmosphere is divided into four regions of atmosphere classified by temperature and the thermal structure of the earth's atmosphere is the result of the complex interaction of the following:

  • Electromagnetic radiation from the sun.
  • Radiation reflected from the earth's surface.
  • Molecules and atoms in the atmosphere.