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The Atmosphere
|
Main Gases: | Percent Content |
Nitrogen | 78% |
Oxygen | 20.9% |
Argon | 0.93% |
Sub-total | 99.8% |
Variable consituents: | |
Carbon dioxide | 200 to 400 parts per million |
Water vapour | 0% to 4% |
Trace gases: | |
Ozone, Neon | Helium |
Krypton, Methane | Sulphur oxides |
Nitrogen oxides | Hydrogen |
Aerosols: | |
Dust | Liquid water droplets |
Salt particles | Acidic droplets |
The weight of the total atmosphere is 5.3 x 1018 kg = 5.3 x 1015 tonnes = 5.3 million, billion tonnes.
Its thickness relative to the diameter of the Earth is like the skin on an apple to the apple.
It is layered into several "spheres"
However, it is only in the troposphere where weather as we know it is present. In the troposphere, the interaction between sunlight and the planet's surface causes unequal heating. The exchange of heat between the atmosphere and the ocean and land creates a heat engine which moves energy, air molecules and water.
Weather is the movement of air and water to exchange energy around the globe in an attempt to equalize temperature over the whole planet.
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