Atmosphere and Climate

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Atmospheric layers

The atmosphere is composed of layers as shown in the diagrams below:

Layers of the atmosphere
View from the International Space Station showing the different layers. A complete description can be found here.
Layers of the atmosphere, showing features of the layers


The troposphere is the layer closest to the Earth's surface and contains 80% of the atmosphere's mass. Importantly, all of the weather occurs in the troposphere.

The temperature in the troposphere decreases by 6 degrees for every km above the surface:

Temperature profile of atmosphere

We will look at the structure of the troposphere in the section on climate below.


The stratosphere is the layer above the troposphere. Here the temperature increases slightly versus height.

It contains about 19% of the mass of the atmosphere. The lower density of the stratosphere (compared to the troposphere) is important. For example, intercontinental airplanes fly here due to less resistance and therefore lower fuel usage.

Even though the weather is in the troposphere; the stratosphere does have an influence on the weather. Phenomena such as the changes in the polar vortex affects the weather (for example, see this article).

Stratospheric Aerosols

Aerosols, mainly ash from volcanoes, can be thrown into the stratosphere. Once in the stratosphere, it can remain for a long time and move a long distance, sometimes even circling the Earth many times. The main effect of these aerosols is to reflect sunlight and cause cooling.

The most famous example of the effect of aerosols is on the dinosaurs. The extinction of dinosaurs (and many other organisms such as marine reptiles and pterosaurs) is now believed to be related to the impact of the Earth by an asteroid. The impact forced a huge amount of aerosols into the stratosphere, causing a major shift in the Earth's climate. This in turn caused the mass extinction.

Eyjafjallajokull volcano, Iceland, erupting on April 17, 2010. This eruption was famous because it caused many airlines to cancel flights due to the ash
Artist's rendering of the asteroid impact which lead to the extinction of the dinosaurs
Figure showing effects of aerosols released by volcanoes

Ozone Layer

Contained in the lower part of the stratosphere is the ozone layer.

Concentration of ozone in atmosphere versus height. You can see clearly the ozone layer in the stratosphere.

Ozone cycle in the stratosphere

Formation of ozone:

O2 + hν → O + O
O + O2 → O3 (ozone)

This ozone then absorbs ultraviolet (UV) radiation:

O3 + hν(UV) → O2 + O
O + O2 → O3

Thus the ozone protects the Earth from dangerous ultraviolet radiation. If it wasn't for this layer life could not exist -- too much radiation would reach the surface.

This absorption of radiation is what causes the increase in temperature in the stratosphere.


The mesosphere is defined as where the temperature starts to decrease again with height.

The mesosphere is where most meteors burn up in the atmosphere.

The mesosphere is poorly understood (since it is too high for balloons and too low for satellites).

One interesting phenomena that occurs in the mesosphere are noctilucent clouds. They are clouds of ice crystals about 80 km above the Earth's surface. It is believed caused by ice condensing on meteoric dust.

Other interesting phenomena include blue jets and sprites.

Noctilucent clouds


In the thermosphere, the temperature starts to increase again due to solar radiation. It is the biggest layer (extending up to 700 km) and is where the International Space Station is located.


An important part of the thermosphere is the ionosphere, a region where the solar radiation is strong enough to split electrons off atoms to form ions.

A spectacular aspect of the ionosphere are the auroras

Aurora Borealis
Aurora video (timelapse)

Another important aspect of the ionosphere is that it allows radio waves to travel long distances. The waves refract off the ionosphere directing them back to Earth.

Radio wave propagation by the ionosphere

Atmospheric composition (troposphere)

Composition of the atmosphere

The numbers in the diagram consider a dry atmosphere. Water vapor accounts for 0-4%.

Climate (in the troposphere)

Icon define.gif
Average weather patterns over the long term (30+ years)

The Earth's weather and climate are determined by three main factors.

  • The tilt of the Earth's axis
  • The rotation of the Earth (known as the Coriolis effect)
  • The ocean currents

The following figures shows the axial tilt and its effects. The sun takes longer to reach the poles, therefore the light is spread out over a wider area and is less intense.

Oblique rays 04 Pengo.svg

This effect and the rotation of the Earth causes major cells in the atmospheric circulation to occur.

General circulation of the Earth's atmosphere showing the major cells that occur

Here the sun heats the air at the equator, this air rises and as it rises it cools down. Cold air can hold less moisture, so it rains. This air masses then moves away from the equator due to the Earth's rotation. This further cools it until it gets too heavy and moves back to the surface. When it falls it now warms up absorbing moisture and causes arid conditions (most deserts are around 30 degrees North and South). This then repeats.

Also important are the ocean currents:

Map showing major ocean currents of the world

Warm currents (red) can create warmer than normal climates to an area (for example, British Isles and Japan). Likewise cold currents (blue) can affect climates (for example, penguins near the Equator off South America).

All these together leads to the following climate zones:

The world's climate zones. Click on map to enlarge. For description of zones see [1]