L4: Atmospheric Composition and Radiative Balance

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29 Terms

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Troposphere

Lowest atmospheric layer, temperature decreases with altitude.

<p>Lowest atmospheric layer, temperature decreases with altitude.</p>
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Stratosphere

Layer above troposphere, temperature increases with altitude.

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Residence Time

Average duration an atom spends in a reservoir.

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Coefficient of Variation

Standard deviation divided by mean.

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Nitrogen Gas (N2)

Major atmospheric component, inert with long residence time.

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Water Vapor

Varies 0-4% in atmosphere, short residence time.

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Carbon Dioxide (CO2)

Residence time of 3-5 years, influenced by natural processes.

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Ozone (O3)

Blocks UV radiation, produced and destroyed in cycles.

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Volatile Organic Carbon (VOC)

Gaseous organic compounds affecting air quality.

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Electromagnetic Radiation

Radiation emitted by objects based on temperature.

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Greenhouse Effect

Traps IR radiation, warming Earth's surface.

<p>Traps IR radiation, warming Earth's surface.</p>
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Radiative Balance

Equilibrium of incoming solar and outgoing IR radiation.

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UV Radiation

High-energy light damaging to living organisms.

<p>High-energy light damaging to living organisms.</p>
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Infrared Radiation (IR)

Longer wavelengths emitted by Earth, absorbed by gases.

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Ozone Depletion

Reduction of stratospheric ozone due to human activities.

<p>Reduction of stratospheric ozone due to human activities.</p>
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Ozone Formation

O2 splits into radicals, forms O3 in stratosphere.

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Atmospheric Composition

Mixture of gases defining atmospheric properties.

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Solar Radiation

Energy from the sun, crucial for Earth's climate.

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Aerosols

Tiny particles in the atmosphere, can be natural or human-made.

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Primary Aerosols

Directly emitted particles like soot and dust.

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Secondary Aerosols

Formed from chemical reactions in the atmosphere.

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Albedo

Reflectivity of Earth's surface affecting energy balance.

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Chemical Processes

Reactions in the atmosphere influenced by solar radiation.

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Long-lived Constituents

Atmospheric components with residence times over 7,000 years.

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Short-lived Constituents

Atmospheric components with residence times under 10 years.

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Dynamic Equilibrium

State where inputs and outputs balance over time.

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Heat Release

Energy emitted as heat during atmospheric reactions.

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Atmospheric Reservoir

Storage of gases within the atmosphere.

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Photochemistry

Chemical reactions initiated by light, affecting air quality.