What this deck covers
This deck focuses on Stratospheric Ozone Depletion, giving you a quick way to review the definitions, rules, and examples that matter most for AP Environmental Science.
Study Stratospheric 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.
0% Complete
What is the main reason for seasonal variation in ozone depletion?
Tap card or press Space to flip
Sunlight availability. UV radiation drives chemical reactions, so depletion peaks during polar spring.
How well did you know it?
Card 1 / 44
Space to flip · ← / → to move · once flipped, → Got it · ← Still learning
This deck focuses on Stratospheric 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: Sunlight availability. UV radiation drives chemical reactions, so depletion peaks during polar spring.
Answer: Polar vortex. Circular wind patterns isolate polar air, creating conditions for severe depletion.
Answer: They provide energy to release chlorine. High-energy UV photons break carbon-chlorine bonds, releasing reactive chlorine.
Answer: Chlorine. HCFCs contain some chlorine but much less than CFCs, reducing ozone impact.
Answer: Skin cancer. UV-B radiation damages DNA in skin cells, leading to malignant tumors.
Answer: Use of aerosol sprays. Aerosols historically contained CFCs as propellants, releasing them into the atmosphere.
Answer: High GWP. CFCs trap thousands of times more heat than carbon dioxide per molecule.
Answer: Chlorine monoxide (ClO). This radical forms when chlorine reacts with ozone, continuing destructive cycles.
Answer: September. Antarctic spring brings sunlight that triggers chemical reactions depleting ozone.
Answer: Increased UV exposure causes cataracts. Higher UV-B levels damage eye lenses, leading to clouding and vision problems.
Answer: Chemical reactions forming O3. Natural photochemical processes continuously create new ozone from oxygen molecules.
Answer: Volcanic eruptions. Volcanic emissions can release chlorine and bromine compounds into the stratosphere.
Answer: Mid-21st century. Recovery depends on continued compliance with international ozone protection agreements.
Answer: Protect the ozone layer. This 1985 framework established international cooperation for ozone layer protection.
Answer: Industrial chemicals. Manufacturing processes release CFCs, HCFCs, and other synthetic ozone depleters.
Answer: Dobson Unit (DU). Named after ozone researcher Gordon Dobson, measures atmospheric ozone thickness.
Answer: Chlorofluorocarbon. These synthetic compounds contain carbon, fluorine, and chlorine atoms.
Answer: UV light breaks them down, releasing chlorine. Photolysis by UV radiation breaks C-Cl bonds, freeing reactive chlorine atoms.
Answer: Volcanic eruptions. Volcanic emissions can release chlorine and bromine compounds into the stratosphere.
Answer: London Amendment. This 1990 amendment strengthened CFC phase-out timelines and added new substances.
Answer: Arctic ozone depletion. Similar to Antarctic ozone hole but typically less severe due to different conditions.
Answer: Reduces greenhouse gases. CFCs are potent greenhouse gases, so eliminating them helps climate protection.
Answer: Measures total ozone column. This unit quantifies the total amount of ozone in a vertical atmospheric column.
Answer: Release CFCs as refrigerants. Old refrigerators contain CFC coolants that escape when units are improperly disposed.
Answer: UV-B radiation. This wavelength range (280-315 nm) increases most when ozone levels drop.
Answer: Hydrofluorocarbons (HFCs). These contain no chlorine or bromine, so they don't harm the ozone layer.
Answer: Ultraviolet (UV) radiation. Ozone molecules absorb UV-B and UV-C radiation, protecting life on Earth.
Answer: Up to 100 years. CFCs have extremely long atmospheric lifetimes, causing persistent ozone depletion.
Answer: UV-B radiation. This wavelength range (280-315 nm) increases most when ozone levels drop.
Answer: Hydrochlorofluorocarbons (HCFCs). These transitional chemicals have shorter lifespans and contain less chlorine than CFCs.
Answer: Hydrochlorofluorocarbons (HCFCs). These transitional chemicals have shorter lifespans and contain less chlorine than CFCs.
Answer: Damages DNA. UV-B breaks chemical bonds in DNA, causing mutations and cellular damage.
Answer: They provide surfaces for chlorine activation. Ice crystals convert stable chlorine compounds into reactive forms that destroy ozone.
Answer: Ozone hole. This seasonal phenomenon occurs due to polar vortex conditions and chemical reactions.
Answer: Chlorofluorocarbons (CFCs). These synthetic chemicals break down in the stratosphere, releasing ozone-destroying chlorine atoms.
Answer: Stratosphere. This layer contains about 90% of Earth's ozone, located 10-50 km above Earth's surface.
Answer: Chlorine. When CFCs break down, chlorine atoms catalytically destroy thousands of ozone molecules.
Answer: Increased UV radiation. Less ozone means more harmful UV-B radiation reaches Earth's surface.
Answer: Measures total ozone column. This unit quantifies the total amount of ozone in a vertical atmospheric column.
Answer: Decreased UV radiation. As ozone layer heals, it will better absorb UV radiation reaching Earth.
Answer: Montreal Protocol. This 1987 agreement successfully phased out production of ozone-depleting chemicals worldwide.
Answer: O2+UV→2O; O+O2→O3. UV splits oxygen molecules, then atomic oxygen combines with O2 forming ozone.
Answer: It catalyzes the breakdown of O3. One chlorine atom can destroy thousands of ozone molecules through catalytic cycles.
Answer: Dobson Unit (DU). Named after ozone researcher Gordon Dobson, measures atmospheric ozone thickness.