The atmosphere's chemical makeup is a complex blend of gases, each playing a unique role. Nitrogen and oxygen dominate, but trace gases like carbon dioxide and methane are crucial for Earth's climate. Understanding these components is key to grasping atmospheric processes.
From greenhouse gases trapping heat to ozone shielding us from UV rays, atmospheric gases shape our world. Sources and sinks of these gases, along with their mixing ratios, help scientists track changes and predict future climate scenarios.
Chemical Composition of the Atmosphere
Composition of Earth's atmosphere
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Nitrogen (N 2 N_2 N 2 )
Most abundant gas in the atmosphere makes up about 78% of the atmosphere by volume
Largely inert and does not participate in many chemical reactions
Oxygen (O 2 O_2 O 2 )
Second most abundant gas in the atmosphere comprises about 21% of the atmosphere by volume
Essential for life on Earth as it is used in respiration by many organisms
Argon (Ar)
Third most abundant gas in the atmosphere makes up about 0.93% of the atmosphere by volume
Inert gas that does not react with other substances under normal conditions
Carbon dioxide (C O 2 CO_2 C O 2 )
Trace gas in the atmosphere comprises about 0.04% of the atmosphere by volume
Important greenhouse gas that absorbs and emits infrared radiation contributing to the Earth's energy balance
Role of atmospheric trace gases
Greenhouse gases
Absorb and emit infrared radiation trapping heat in the atmosphere (greenhouse effect)
Examples: water vapor (H 2 O H_2O H 2 O ), carbon dioxide (C O 2 CO_2 C O 2 ), methane (C H 4 CH_4 C H 4 ), nitrous oxide (N 2 O N_2O N 2 O )
Increasing concentrations due to human activities lead to global warming and climate change
Ozone (O 3 O_3 O 3 )
Absorbs ultraviolet (UV) radiation in the stratosphere protecting life on Earth from harmful UV rays
Can be a pollutant in the troposphere contributing to smog and respiratory issues (ground-level ozone)
Formed by photochemical reactions involving nitrogen oxides (NOx) and volatile organic compounds (VOCs)
Aerosols
Solid or liquid particles suspended in the atmosphere can have cooling or warming effects on climate
Scatter and absorb solar radiation influencing the Earth's energy balance (aerosol direct effect)
Act as cloud condensation nuclei affecting cloud properties and precipitation (aerosol indirect effect)
Examples: dust, sea salt, volcanic ash, sulfates, black carbon
Sources and sinks of gases
Carbon dioxide (C O 2 CO_2 C O 2 )
Sources: fossil fuel combustion (coal, oil, natural gas), deforestation, cement production, respiration
Sinks: photosynthesis by plants and phytoplankton, ocean absorption, weathering of rocks
Increasing atmospheric concentrations primarily due to human activities (anthropogenic emissions)
Methane (C H 4 CH_4 C H 4 )
Sources: wetlands, agriculture (rice cultivation, livestock), fossil fuel extraction (natural gas, coal), landfills
Sinks: chemical reactions in the atmosphere (oxidation by hydroxyl radicals)
Has a stronger greenhouse effect per molecule compared to C O 2 CO_2 C O 2 but shorter atmospheric lifetime
Nitrous oxide (N 2 O N_2O N 2 O )
Sources: microbial processes in soils and oceans, agricultural activities (fertilizer use), industrial processes
Sinks: photodissociation in the stratosphere where it is broken down by ultraviolet radiation
Long-lived greenhouse gas with a global warming potential 298 times that of C O 2 CO_2 C O 2 over a 100-year period
Ozone (O 3 O_3 O 3 )
Sources: photochemical reactions involving NOx and VOCs in the troposphere, stratospheric production from oxygen photolysis
Sinks: chemical reactions with other substances (NOx, HOx), deposition to surfaces
Beneficial in the stratosphere but harmful to human health and vegetation in the troposphere
Atmospheric mixing ratios
Mixing ratio
Ratio of the number of moles of a particular gas to the total number of moles of air in a given volume
Expressed as mole fraction, parts per million by volume (ppmv), or parts per billion by volume (ppbv)
Allows for consistent comparison of gas concentrations across different locations and times
Dry air mixing ratio
Excludes water vapor from the calculation as water vapor content can vary significantly
Used to compare the composition of air masses with different moisture content
Helpful in understanding the behavior of gases in the atmosphere
Conversion between units
ppmv = (mole fraction) × 1 0 6 10^6 1 0 6
ppbv = (mole fraction) × 1 0 9 10^9 1 0 9
Useful for expressing the concentrations of trace gases with very low abundances
Importance in atmospheric science
Used in atmospheric models and climate simulations to represent the composition of the atmosphere
Helps monitor changes in atmospheric composition due to natural and anthropogenic factors
Provides a standardized way to report and analyze atmospheric measurements from different instruments and platforms