Atmosphere
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The composition of the Earth’s atmosphere changes with the altitude.
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The major constituents of the Earth’s atmosphere are:
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Nitrogen – 78.09%
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Oxygen – 20.95%
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Argon – 0.93%
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Carbon Dioxide – 0.039% (remaining other gasses)
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The pressure exerted by the weight of air at a given point is known as “Atmospheric Pressure” or “Barometric Pressure.”
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With increasing altitude, the atmospheric pressure decreases.
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On an average, a column of air (which is normally one square centimeter in cross-section), measured at the sea level, has the weight of about 1.03 kg (about 10.1 N).
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The Average Air Pressure is about 14.70 pounds per square inch, (equivalent to 1,013.25 × 103 dynes per square centimeter or 1,013.25 millibars) at the sea level.
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A visible mass of condensed vapor floating above the general level of the ground is known as Cloud.
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Based on the altitude, cloud is classified as −
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High Altitude Cloud: For example, Cirrus, Cirrocumulus, & Cirrostratus.
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Middle Altitude Cloud: For example, Altostratus and Altocumulus.
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Low Altitude Cloud: Stratus, Stratocumulus, Cumulus, and Nimbostratus (it can be also seen in the middle altitude).
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Vertical: Cumulonimbus
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