ATMOSPHERE
The atmosphere is the layer of gases that surrounds a planet, moon, or other celestial body. On Earth, the atmosphere is crucial for supporting life and consists mainly of:
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Nitrogen (78%)
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Oxygen (21%)
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Small amounts of argon, carbon dioxide, water vapor, and other gases
Functions of Earth’s Atmosphere:
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Protects life by blocking harmful solar radiation (like UV rays)
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Regulates temperature through the greenhouse effect
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Enables weather and climate through the movement of air and moisture
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Provides oxygen for respiration and carbon dioxide for photosynthesis
Layers of Earth’s Atmosphere :
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Troposphere – where weather occurs
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Stratosphere – contains the ozone layer
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Mesosphere – where meteors burn up
Thermosphere – contains the ionosphere; auroras occur here
Exosphere – outermost layer, gradually fades into space
Troposphere:
The troposphere is the lowest layer of Earth's atmosphere, where almost all weather phenomena occur—like clouds, rain, snow, and storms.
Key Characteristics of the Troposphere:
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Extends from the Earth's surface up to about 8–15 km (5–9 miles), depending on location:
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Thicker at the equator (~15 km)
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Thinner at the poles (~8 km)
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Contains about 75–80% of the atmosphere's total mass
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Made up mostly of nitrogen (78%) and oxygen (21%), with traces of other gases
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Temperature decreases with altitude (about 6.5°C per kilometer on average)
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The top boundary is called the tropopause, which separates it from the stratosphere
Stratosphere :
The stratosphere is the second layer of Earth's atmosphere, located above the troposphere and below the mesosphere.
Key Characteristics of the Stratosphere:
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Altitude: Roughly 10 to 50 km (6 to 31 miles) above Earth's surface
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Temperature: Increases with altitude, unlike the troposphere
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This is due to the ozone layer absorbing ultraviolet (UV) radiation from the sun
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Weather: Very stable, with little mixing of air—no clouds or storms like in the troposphere
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Jet aircraft and weather balloons often fly in the lower stratosphere to avoid turbulence
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The top of the stratosphere is called the stratopause, which marks the boundary with the mesosphere
Mesosphere :
The mesosphere is the third layer of Earth’s atmosphere, located above the stratosphere and below the thermosphere.
Key Characteristics of the Mesosphere:
- Altitude: Roughly 50 to 85 km (31 to 53 miles) above Earth’s surface
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Temperature: Decreases with altitude, making it the coldest layer of the atmosphere
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Temperatures can drop to -90°C (-130°F) or lower near the top
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Top boundary: Called the mesopause, which is the coldest point in Earth's atmosphere
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Air pressure: Extremely low; only a tiny fraction of what it is at sea level
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Composition: Mostly oxygen and nitrogen, but very thin
Thermosphere:
Key Characteristics of the Thermosphere:
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Altitude: Roughly 85 to 600 km (53 to 373 miles) above Earth’s surface
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Temperature: Increases sharply with altitude
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Can reach up to 2,500°C (4,500°F) or more
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Despite high temperatures, it wouldn’t feel hot to us—because the air is so thin (few molecules to transfer heat)
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Top boundary: The thermopause, which leads into the exosphere
Contains the ionosphere (overlaps the thermosphere), a region filled with charged particles that reflect radio waves and enable long-distance communication
Exosphere:
The exosphere is the outermost layer of Earth's atmosphere, gradually transitioning into outer space.
Key Characteristics of the Exosphere:
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Altitude: Starts around 600 km (373 miles) and extends up to 10,000 km (6,200 miles) or more
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Air density: Extremely thin—molecules are so sparse they can travel hundreds of kilometers without colliding
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Composition: Mostly hydrogen and helium atoms, with traces of oxygen and carbon dioxide
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Temperature: Technically very high, but since there are so few particles, it wouldn’t feel hot
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