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This deck focuses on Reducing Ozone Depletion, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Study Reducing Ozone Depletion in AP Environmental Science with focused flashcards that help you recognize the idea, recall the key rule, and apply it in practice-style prompts.
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What is the primary role of the ozone layer in Earth's atmosphere?
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Absorbing UV radiation. Ozone filters harmful UV-B and UV-C radiation from reaching Earth's surface.
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This deck focuses on Reducing Ozone Depletion, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Work through these flashcards in short sessions. Try to answer each prompt before flipping the card, then revisit any cards you miss until the explanation feels automatic.
Answer: Absorbing UV radiation. Ozone filters harmful UV-B and UV-C radiation from reaching Earth's surface.
Answer: Hydrochlorofluorocarbons (HCFCs). HCFCs have lower ozone depletion potential than CFCs but still cause damage.
Answer: 100%. The protocol aims for complete elimination of CFC production and consumption.
Answer: United Nations Environment Programme (UNEP). UNEP coordinates global efforts and monitors compliance with ozone treaties.
Answer: Volcanic eruptions. Volcanoes release sulfur compounds that can deplete ozone temporarily.
Answer: Refrigeration and air conditioning. CFCs were widely used as coolants before their ozone-depleting effects were known.
Answer: Phasing out CFC production. The protocol mandates complete phase-out of CFC production by developed nations.
Answer: Satellite observations. Satellites measure total ozone column thickness to track layer recovery.
Answer: Hydrofluorocarbons (HFCs). HFCs don't deplete ozone but have high global warming potential.
Answer: Halons. Halons contain bromine atoms that are particularly destructive to ozone.
Answer: Hydrofluorocarbons (HFCs). HFCs don't deplete ozone but have high global warming potential.
Answer: Oxygen molecules and UV light. UV light splits O2 molecules; oxygen atoms combine with O2 forming O3.
Answer: Firefighting. Fire suppression systems historically used halons before safer alternatives.
Answer: Non-halogenated solvents. These solvents lack halogen atoms that cause ozone destruction.
Answer: Decreased crop yields. Excess UV-B radiation damages plant cells and reduces photosynthesis efficiency.
Answer: Polar stratospheric clouds. These clouds provide surfaces where chlorine compounds become ozone-destroying.
Answer: Aerosol propellants. CFCs were commonly used to propel contents from spray cans and bottles.
Answer: Chlorofluorocarbons (CFCs). CFCs release chlorine atoms that destroy ozone molecules in the stratosphere.
Answer: The Montreal Protocol. Signed in 1987, this protocol phases out ozone-depleting substances globally.
Answer: Using energy-efficient appliances. Efficient appliances reduce demand for refrigerants containing ozone-depleting chemicals.
Answer: Ozone Depleting Potential (ODP). ODP compares substances to CFC-11's ozone destruction capability (ODP = 1.0).
Answer: UV-B. Ozone molecules absorb UV-B wavelengths (280-315 nm) most effectively.
Answer: Polar stratospheric clouds. These clouds provide surfaces where chlorine compounds become ozone-destroying.
Answer: Refrigeration and air conditioning. CFCs were widely used as coolants before their ozone-depleting effects were known.
Answer: UV-B. Ozone molecules absorb UV-B wavelengths (280-315 nm) most effectively.
Answer: Chlorine. Chlorine atoms act as catalysts, destroying many ozone molecules per atom.
Answer: Ammonia-based refrigeration. Natural refrigerants like ammonia don't contain ozone-depleting halogens.
Answer: Protecting the ozone layer. Signed in 1985, this convention established framework for ozone protection.
Answer: Decrease in atmospheric chlorine. Reduced chlorine levels indicate the protocol's effectiveness in ozone protection.
Answer: Methyl bromide. Used in fumigation and foam production, methyl bromide releases bromine atoms.
Answer: HFCs contribute to global warming. HFC replacements for CFCs are potent greenhouse gases warming the climate.
Answer: Phasing out CFC production. The protocol mandates complete phase-out of CFC production by developed nations.
Answer: Protecting the ozone layer. Signed in 1985, this convention established framework for ozone protection.
Answer: Cellulose insulation. Natural insulation materials eliminate need for foam-blowing chemicals.
Answer: Hydrochlorofluorocarbons (HCFCs). HCFCs have lower ozone depletion potential than CFCs but still cause damage.
Answer: Reduced phytoplankton growth. Increased UV-B damages marine phytoplankton, disrupting ocean food webs.
Answer: Firefighting. Fire suppression systems historically used halons before safer alternatives.
Answer: UV-B. UV-B causes skin cancer, cataracts, and immune system suppression in humans.
Answer: Increased skin cancer risk. More UV-B radiation penetrates when ozone layer is depleted, causing DNA damage.
Answer: Decrease in atmospheric chlorine. Reduced chlorine levels indicate the protocol's effectiveness in ozone protection.
Answer: Ammonia-based refrigeration. Natural refrigerants like ammonia don't contain ozone-depleting halogens.
Answer: Chlorine. Chlorine atoms act as catalysts, destroying many ozone molecules per atom.
Answer: Halons. Halons contain bromine which is highly effective at destroying ozone.
Answer: The Kigali Amendment. This 2016 amendment targets HFCs to prevent climate change acceleration.
Answer: Satellite observations. Satellites measure total ozone column thickness to track layer recovery.
Answer: Agriculture. Soil fumigation with methyl bromide releases bromine into the atmosphere.
Answer: United Nations Environment Programme (UNEP). UNEP coordinates global efforts and monitors compliance with ozone treaties.
Answer: Chlorofluorocarbons (CFCs). CFCs release chlorine atoms that destroy ozone molecules in the stratosphere.
Answer: Halons. Halons contain bromine atoms that are particularly destructive to ozone.
Answer: Ozone Depleting Potential (ODP). ODP compares substances to CFC-11's ozone destruction capability (ODP = 1.0).
Answer: The stratosphere. The ozone layer is located 15-35 km above Earth's surface in the stratosphere.
Answer: Using energy-efficient appliances. Efficient appliances reduce demand for refrigerants containing ozone-depleting chemicals.
Answer: Agriculture. Soil fumigation with methyl bromide releases bromine into the atmosphere.
Answer: Oxygen molecules and UV light. UV light splits O2 molecules; oxygen atoms combine with O2 forming O3.
Answer: CFCs releasing chlorine atoms. Chlorine atoms from CFCs catalytically destroy thousands of ozone molecules.
Answer: Non-halogenated solvents. These solvents lack halogen atoms that cause ozone destruction.
Answer: Methyl bromide. Used in fumigation and foam production, methyl bromide releases bromine atoms.
Answer: 50 to 100 years. CFCs persist for decades, continuing to destroy ozone long after release.
Answer: Reduced phytoplankton growth. Increased UV-B damages marine phytoplankton, disrupting ocean food webs.
Answer: Absorbing UV radiation. Ozone filters harmful UV-B and UV-C radiation from reaching Earth's surface.
Answer: HFCs contribute to global warming. HFC replacements for CFCs are potent greenhouse gases warming the climate.
Answer: The stratosphere. The ozone layer is located 15-35 km above Earth's surface in the stratosphere.
Answer: Cellulose insulation. Natural insulation materials eliminate need for foam-blowing chemicals.