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  • Earth's Atmospheric Layers: A Comprehensive Guide
    The Earth's atmosphere is composed of several distinct layers, each with its own unique characteristics. Here's a breakdown:

    1. Troposphere:

    * Altitude: 0-10 km (0-6.2 miles)

    * Characteristics:

    * Contains about 80% of the atmosphere's mass.

    * Where weather occurs.

    * Temperature decreases with altitude.

    * Contains most of the atmosphere's water vapor.

    * Home to most living organisms.

    2. Stratosphere:

    * Altitude: 10-50 km (6.2-31 miles)

    * Characteristics:

    * Contains the ozone layer, which absorbs most of the Sun's harmful ultraviolet radiation.

    * Temperature increases with altitude due to the absorption of UV radiation.

    * Relatively calm and stable.

    3. Mesosphere:

    * Altitude: 50-85 km (31-53 miles)

    * Characteristics:

    * Temperature decreases with altitude.

    * The coldest layer of the atmosphere (-90°C or -130°F).

    * Most meteors burn up in this layer.

    4. Thermosphere:

    * Altitude: 85-600 km (53-373 miles)

    * Characteristics:

    * Temperature increases with altitude due to absorption of solar radiation.

    * Very thin air, but can reach very high temperatures (over 1,500°C or 2,732°F).

    * Home to the International Space Station and many satellites.

    * Auroras occur in this layer.

    5. Exosphere:

    * Altitude: 600 km (373 miles) and beyond

    * Characteristics:

    * Outermost layer, gradually merging into space.

    * Very thin and cold.

    * Contains mostly hydrogen and helium.

    * Satellites orbiting Earth in this layer are essentially in space.

    Note: There is no clear boundary between the exosphere and space. The transition is gradual.

    Beyond these five main layers, you might also hear about the ionosphere, which is a region within the thermosphere and upper mesosphere where solar radiation ionizes atoms and molecules. It plays a crucial role in radio communication.

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