The atmosphere

28 Februari 2010 pukul 12:27 | Ditulis dalam Uncategorized | Tinggalkan komentar

The Earth’s atmosphere is a layer of gases surrounding the planet Earth that is held in place by the pull of Earth’s gravity.

The Earth’s atmosphere contains a mixture of gases is commonly known as air:

  • 78% nitrogen,
  • 21% oxygen,
  • 0.93% argon,
  • 0.04% carbon dioxide – although this is increasing
  • water vapour (average of 1% – but that varies).
  • trace amounts of other gases

The atmosphere protects life on Earth .

  • It is deep enough to absorb X-rays and gamma rays from outer space, preventing them from reaching ground level at all.
  • The ozone layer absorbs ultraviolet solar radiation.
  • The atmosphere acts like a blanket over the Earth, reducing temperature extremes between day and night – making it easier for life forms to survive.

The atmosphere absorbs and reflects some of the heat radiation from the Sun.

This prevents the Earth’s surface from getting too hot during the day. It retains some of that energy so that all of the energy collected from the Sun is not lost during the night (as would be the case if there was no atmosphere). Only some of it is radiated back out into space. This stops the temperature of the Earth from dropping too low during the night. It is able to do this because some of the molecules of gas in the atmosphere are ‘greenhouse gases’.

There is no definite boundary between the atmosphere and outer space. It slowly becomes thinner and fades into space. Three quarters of the atmosphere’s mass is within 11 km of the planetary surface.

  • People who travel above an altitude of 80.5 km (50 miles) are called astronauts.
  • An altitude of 120 km (75 miles) marks the boundary where atmospheric effects become noticeable during re-entry.
  • The Kármán line, at 100 km (62 miles), is also frequently regarded as the boundary between atmosphere and outer space.

atmosphere The temperature of the Earth’s atmosphere varies with altitude (how high up you are!); the mathematical relationship between temperature and altitude varies among five different atmospheric layers.

The troposphere is the layer closest to the earth, and it is the layer in which we live. It is about ten miles deep. Seventy five percent of the mass of all our atmospheric molecules is in the troposphere, and this is where we find water vapour, dust, pollen, and soot particles. Weather happens in the troposphere. This layer is turbulent, with storms and atmospheric mixing.

In the troposphere, the air cools gradually as it gets further from the earth. At the very top of this layer the air temperature is about -60 oC. Water vapour is therefore in the form of ice. This forms what we call the cold trap – a temperature region where water vapour rises no further (because it has solidified). If we had no cold trap, water molecules could rise higher and higher in the atmosphere are they would eventually break down into oxygen and hydrogen at the outermost layers – the small, light hydrogen molecules could then escape into space. Earth would lose its water if we had no cold trap!

The stratosphere lies above the troposphere. The lower part of the stratosphere is cold, but it warms up as it gets farther from the earth. It is about twenty miles deep. The stratosphere contains about 24% of the mass of all the atmospheric molecules. This layer has the ozone layer in it. The ozone layer protects life on earth from the high energy ultraviolet radiation emitted by the sun

Tinggalkan sebuah Komentar »

RSS feed for comments on this post. TrackBack URI

Tinggalkan Balasan

Isikan data di bawah atau klik salah satu ikon untuk log in:

Logo WordPress.com

You are commenting using your WordPress.com account. Logout / Ubah )

Gambar Twitter

You are commenting using your Twitter account. Logout / Ubah )

Foto Facebook

You are commenting using your Facebook account. Logout / Ubah )

Foto Google+

You are commenting using your Google+ account. Logout / Ubah )

Connecting to %s

Buat situs web atau blog gratis di WordPress.com.
Entries dan komentar feeds.

%d blogger menyukai ini: