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AP Environmental Science Unit 9 Review: Global Change

Review AP Environmental Science Unit 9 to understand how human activities drive global-scale environmental change, from ozone depletion and the greenhouse effect to ocean acidification, invasive species, and biodiversity loss. This unit carries 15-20% of the exam and connects directly to concepts from nearly every earlier unit.

Use this page to review all 10 topics in Unit 9, check key terms, and find topic guides and practice questions available through Fiveable.

What is AP Environmental Science unit 9?

Unit 9 asks you to trace human-caused changes from the atmosphere all the way through ocean chemistry and living communities. The topics build on each other: greenhouse gas increases warm the planet, warming changes ocean temperature and chemistry, and those changes combine with direct human pressures to threaten species and biodiversity.

Unit 9 covers global environmental change caused primarily by human activities. Key themes include stratospheric ozone depletion by CFCs, the enhanced greenhouse effect and its climate consequences, ocean warming and acidification from rising CO2, and biodiversity threats from invasive species, habitat loss, and overexploitation.

Atmosphere: ozone and greenhouse gases

CFCs destroy stratospheric ozone through catalytic chlorine reactions, increasing UV-B at Earth's surface. Separately, CO2, methane, nitrous oxide, and CFCs trap outgoing infrared radiation and enhance the greenhouse effect. GWP ranks CFCs highest, followed by nitrous oxide, then methane, with CO2 as the baseline of 1.

Oceans: warming and acidification

Rising greenhouse gases cause oceans to absorb excess heat, stressing marine species through habitat loss, metabolic disruption, and coral bleaching when zooxanthellae are expelled. Simultaneously, oceans absorb CO2, forming carbonic acid, lowering pH, and reducing calcium carbonate availability, which harms shell-building organisms and corals.

Biodiversity: invasive species, endangered species, and HIPPCO

Invasive species are often generalist, r-selected organisms that outcompete natives. Species become endangered through overhunting, habitat loss, limited diet, or invasive competition. HIPPCO summarizes the six main human-driven biodiversity threats: habitat destruction, invasive species, population growth, pollution, climate change, and overexploitation.

Human activity reshapes Earth's systems at a global scale

Every topic in Unit 9 traces back to a human action, whether burning fossil fuels, releasing CFCs, fragmenting habitat, or introducing non-native species. The exam expects you to explain the mechanism behind each change, not just name it. For example, knowing that CO2 dissolves to form carbonic acid (CO2 + H2O forms H2CO3, which releases H+ ions) is more useful than simply stating that oceans become acidic.

AP Environmental Science unit 9 topics

9.1

Stratospheric Ozone Depletion

The ozone layer absorbs UV-B radiation. CFCs release chlorine radicals that catalytically destroy ozone. The Antarctic ozone hole forms each spring. Reduced ozone increases UV-B, raising skin cancer and cataract risk.

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9.2

Reducing Ozone Depletion

CFCs are replaced by HFCs, which do not deplete ozone because they lack chlorine. However, many HFCs are potent greenhouse gases. The Montreal Protocol phased out CFC production internationally.

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9.3

The Greenhouse Effect

CO2, methane, water vapor, nitrous oxide, and CFCs are the principal greenhouse gases. The natural greenhouse effect maintains surface temperatures for life. GWP ranks CFCs highest, then nitrous oxide, then methane, with CO2 as the baseline.

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9.4

Increases in the Greenhouse Gases

Rising greenhouse gas concentrations enhance the greenhouse effect, causing sea-level rise from ice melt and thermal expansion, and shifting disease vector ranges toward the poles.

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9.5

Global Climate Change

Climate change alters sea level, ocean circulation, atmospheric circulation (Hadley cells, jet stream), soil, and polar ecosystems. The ice-albedo positive feedback loop causes polar regions to warm faster than the rest of Earth.

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9.6

Ocean Warming

Greenhouse gases cause oceans to absorb excess heat. Warmer water causes coral bleaching by expelling zooxanthellae, disrupts marine species metabolism and reproduction, and shifts species ranges poleward.

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9.7

Ocean Acidification

Oceans absorb CO2, forming carbonic acid and lowering pH. Lower pH reduces calcium carbonate availability, harming corals, oysters, and other shell-building organisms. Fossil fuel combustion and deforestation are the main anthropogenic causes.

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9.8

Invasive Species

Invasive species thrive outside their native habitat and threaten native species. They are often generalist, r-selected species. Control strategies include prevention, physical removal, chemical treatment, and biological control.

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9.9

Endangered Species

Species become endangered through overhunting, limited diet, invasive competitors, or specific habitat needs. Selective pressures reduce fitness. Strategies include the Endangered Species Act, CITES, captive breeding, and habitat protection.

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9.10

Human Impacts on Biodiversity

HIPPCO summarizes the six main biodiversity threats. Habitat fragmentation isolates populations and reduces gene flow. Some species are domesticated for economic use, reducing genetic diversity. Mitigation includes protected areas, corridors, and legislation.

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Major Environmental Disasters

Review major AP Environmental Science disasters from Chernobyl to coral bleaching, with causes, effects, and prevention strategies you can use on FRQs.

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practice snapshot

Hardest AP Environmental unit 9 topics

This snapshot uses Fiveable practice activity to show where students tend to miss questions and which review moves are worth prioritizing first.

72%average MCQ accuracy

Across 17k multiple-choice practice attempts for this unit.

17kMCQ attempts

Practice activity included in this snapshot.

63%average FRQ score

Across 31 scored free-response attempts for this unit.

Hardest topics in unit 9

MCQ miss rate
9.3

Review The Greenhouse Effect with attention to how the concept appears in AP-style source and evidence questions.

35%2,715 tries
9.5

Review Global Climate Change with attention to how the concept appears in AP-style source and evidence questions.

32%1,878 tries
9.2

Review Reducing Ozone Depletion with attention to how the concept appears in AP-style source and evidence questions.

31%1,894 tries
9.1

Review Stratospheric Ozone Depletion with attention to how the concept appears in AP-style source and evidence questions.

27%2,411 tries

Unit 9 review notes

9.1

Stratospheric Ozone Depletion

The stratospheric ozone layer absorbs UV-B radiation, protecting life on Earth. CFCs released at the surface eventually reach the stratosphere, where UV light breaks them apart and releases chlorine radicals. Those radicals catalytically destroy ozone molecules. The Antarctic ozone hole forms each spring when polar stratospheric clouds provide surfaces for these reactions after winter darkness ends. Natural factors such as melting ice crystals also contribute to seasonal ozone loss.

  • CFCs: Synthetic compounds containing carbon, chlorine, and fluorine; used in refrigerants and aerosols; primary anthropogenic cause of ozone depletion.
  • Chlorine radical catalytic cycle: Cl atoms released from CFCs react with ozone (O3) to form ClO and O2, then react again to regenerate Cl, destroying many ozone molecules per chlorine atom.
  • Antarctic ozone hole: Seasonal thinning of stratospheric ozone over Antarctica each spring, intensified by polar stratospheric clouds and the polar vortex.
  • UV-B increase: Reduced ozone allows more UV-B to reach Earth's surface, increasing rates of skin cancer and cataracts in humans and harming other organisms.
Can you explain why the ozone hole appears over Antarctica in spring rather than year-round or at the equator?
FactorTypeMechanism
CFCsAnthropogenicRelease Cl radicals that catalytically destroy O3
Polar stratospheric cloudsNatural/amplifiedProvide surfaces for ozone-destroying reactions in Antarctic spring
Melting ice crystalsNaturalRelease trapped reactive compounds at start of Antarctic spring
9.2

Reducing Ozone Depletion

Ozone depletion is reduced by replacing CFCs with chemicals that break down before reaching the stratosphere. Hydrofluorocarbons (HFCs) are the main CFC substitute because they contain no chlorine and do not deplete ozone. However, many HFCs are potent greenhouse gases, creating a trade-off between ozone protection and climate impact. The Montreal Protocol is the international agreement that phased out CFC production.

  • HFCs: CFC substitutes that contain no chlorine and do not deplete ozone, but some have high global warming potential.
  • Montreal Protocol: International agreement that phased out production of ozone-depleting substances including CFCs; considered highly effective.
  • Trade-off: HFCs protect the ozone layer but some are strong greenhouse gases, so switching from CFCs to HFCs reduces one problem while potentially worsening another.
Why are HFCs considered an imperfect solution to ozone depletion?
CompoundDepletes Ozone?Strong Greenhouse Gas?
CFCsYesYes
HFCsNoYes (many)
HFOs (newer alternatives)NoLow GWP
9.3

The Greenhouse Effect and Rising Greenhouse Gases

The natural greenhouse effect keeps Earth warm enough for life by allowing solar radiation in while greenhouse gases absorb outgoing infrared radiation. The principal greenhouse gases are CO2, methane, water vapor, nitrous oxide, and CFCs. Human activities have increased concentrations of these gases, enhancing the greenhouse effect and driving global warming. Water vapor has a short residence time and does not directly drive climate change the way long-lived gases do. GWP ranks the potency of each gas relative to CO2 (GWP = 1). Consequences of rising greenhouse gases include sea-level rise from melting ice and thermal expansion, and disease vectors such as mosquitoes spreading toward the poles.

  • Global warming potential (GWP): A measure of how much heat a greenhouse gas traps relative to CO2 over 100 years; CFCs have the highest GWP, followed by nitrous oxide, then methane.
  • Residence time: How long a gas stays in the atmosphere; water vapor has a short residence time and does not accumulate, while CO2 and methane persist for decades to centuries.
  • Sea-level rise: Caused by two mechanisms: melting ice sheets and glaciers adding water, and thermal expansion of warming ocean water.
  • Disease vector range shifts: Warmer temperatures allow mosquitoes and other disease vectors to survive at higher latitudes and elevations, spreading diseases like malaria and dengue.
Why does water vapor not drive long-term climate change even though it is a greenhouse gas?
Greenhouse GasGWP RankKey Human Source
CO2Baseline (1)Fossil fuel combustion, deforestation
Methane (CH4)High (about 25x CO2)Livestock, landfills, natural gas leaks
Nitrous oxide (N2O)Very high (about 265x CO2)Fertilizers, agriculture
CFCsHighestRefrigerants, aerosols (now phased out)
Water vaporGreenhouse gas but short residence timeEvaporation (natural, not a driver)
9.5

Global Climate Change and Ecosystem Impacts

Climate change reshapes ecosystems through multiple interconnected pathways. Polar regions warm fastest because of the ice-albedo positive feedback loop: melting ice exposes darker ocean or land, which absorbs more solar energy, causing further warming. Atmospheric circulation changes include Hadley cell expansion and jet stream shifts. Ocean circulation, including the thermohaline conveyor belt, can slow as freshwater from melting ice reduces salinity-driven density differences. Marine ecosystems face both gains (new shallow habitats on flooded continental shelves) and losses (deeper communities pushed below the photic zone). Soil erosion and permafrost thaw releasing methane are additional land-based consequences.

  • Ice-albedo feedback: Melting ice reduces surface reflectivity, causing more solar absorption and further warming, a positive feedback loop that accelerates polar warming.
  • Ocean conveyor belt: Global thermohaline circulation that distributes heat; slows when freshwater input from melting ice reduces the density differences that drive it.
  • Hadley cells: Atmospheric circulation cells in the tropics; their expansion with warming shifts precipitation patterns and can expand deserts.
  • Jet stream: Upper-atmosphere wind current that influences weather; temperature changes from climate change can cause it to shift or become more erratic.
  • Permafrost: Permanently frozen ground in polar and high-altitude regions; thawing releases stored methane and CO2, creating another positive feedback.
Explain why the Arctic warms faster than the tropics using the albedo feedback mechanism.
System AffectedChangeConsequence
Polar iceMeltingSea-level rise, reduced albedo, positive feedback
Ocean circulationSlowing conveyor beltRegional climate shifts, especially in North Atlantic
AtmosphereHadley cell expansion, jet stream shiftsAltered precipitation, more extreme weather
Marine ecosystemsSea-level riseNew shelf habitats gained, deep communities lose photic zone access
9.6

Ocean Warming and Ocean Acidification

Oceans absorb most of the excess heat from the enhanced greenhouse effect, raising sea surface temperatures. Warmer water causes coral bleaching when corals expel their symbiotic zooxanthellae algae; some corals recover if temperatures drop, but prolonged bleaching leads to coral death. Warmer water also disrupts marine species metabolism and reproduction and shifts species ranges poleward. Separately, oceans absorb atmospheric CO2, which reacts with water to form carbonic acid: CO2 + H2O forms H2CO3, which dissociates to release H+ ions, lowering pH. Lower pH reduces carbonate ion availability, making it harder for corals, oysters, and other calcifying organisms to build calcium carbonate shells and skeletons.

  • Coral bleaching: Corals expel zooxanthellae under thermal stress, turning white; prolonged bleaching causes coral death because zooxanthellae provide most of the coral's energy through photosynthesis.
  • Zooxanthellae: Photosynthetic algae living symbiotically inside coral tissue; their loss during bleaching deprives corals of nutrients.
  • Ocean acidification: Decrease in ocean pH caused by absorption of atmospheric CO2, which forms carbonic acid and releases hydrogen ions.
  • Calcium carbonate: The mineral used by corals, oysters, and other organisms to build shells and skeletons; less available as ocean pH drops.
  • Carbonic acid reaction: CO2 + H2O forms H2CO3, which releases H+ ions, lowering pH and reducing carbonate ion concentration in seawater.
Distinguish between ocean warming and ocean acidification: what causes each, and how do their effects on coral differ?
ProcessPrimary CauseEffect on Coral
Ocean warmingGreenhouse gas-driven heat absorptionBleaching from zooxanthellae expulsion
Ocean acidificationCO2 absorption forming carbonic acidReduced calcium carbonate, weaker skeletons
9.8

Invasive Species

Invasive species are organisms living outside their native habitat that threaten native species. They are often generalist, r-selected species that reproduce quickly, tolerate a wide range of conditions, and outcompete native specialists for resources. Examples include zebra mussels filtering out phytoplankton in the Great Lakes, kudzu overgrowing native vegetation in the southeastern US, and the brown tree snake eliminating native birds on Guam. Control strategies include prevention (inspections, ballast water treatment), physical removal, chemical treatment, and biological control using natural predators or pathogens.

  • Generalist species: Species that can use a wide range of resources and tolerate varied conditions, giving them a competitive advantage in new environments.
  • r-selected species: Species with high reproductive rates and short generation times; these traits help invasive species establish quickly in new habitats.
  • Biological control: Using a natural predator, parasite, or pathogen to reduce invasive species populations; must be carefully evaluated to avoid introducing another invasive.
  • Competitive exclusion: When an invasive species outcompetes a native species for the same resources, potentially driving the native species to local extinction.
Why are r-selected generalist species more likely to become successful invaders than K-selected specialists?
9.9

Endangered Species and Human Impacts on Biodiversity

Species become endangered when threats exceed their ability to adapt or relocate. Specialist species with limited diets, specific habitat needs, or low reproductive rates are most vulnerable. Selective pressures including overhunting, invasive competitors, and habitat loss reduce fitness and population size. HIPPCO summarizes the six main human-driven biodiversity threats: habitat destruction, invasive species, population growth, pollution, climate change, and overexploitation. Habitat fragmentation breaks large habitats into isolated patches, reducing gene flow and increasing edge effects. Strategies to protect species include the Endangered Species Act, CITES, captive breeding programs, habitat corridors, and protected areas.

  • HIPPCO: Acronym for the six main causes of biodiversity loss: Habitat destruction, Invasive species, Population growth, Pollution, Climate change, Overexploitation.
  • Habitat fragmentation: Breaking large continuous habitats into smaller isolated patches through roads, agriculture, or development; reduces population connectivity and increases extinction risk.
  • Selective pressure: Any environmental factor that changes the survival or reproductive success of organisms; overhunting, disease, and competition are examples.
  • Captive breeding program: Breeding endangered species in controlled settings to increase population size, often followed by reintroduction to the wild.
  • Habitat corridors: Connected strips of habitat linking fragmented patches, allowing movement, gene flow, and recolonization between populations.
List the six HIPPCO factors and give one specific example of each that you could use in a free-response answer.
StrategyHow It HelpsExample
Endangered Species ActLegal protection for listed species and their habitatsBald eagle recovery in the US
CITESRegulates international trade in endangered speciesBans ivory trade to protect elephants
Captive breedingIncreases population size outside the wildCalifornia condor reintroduction
Habitat corridorsConnects fragmented patches for gene flowWildlife overpasses across highways
Protected areasPreserves habitat from developmentNational parks and wildlife refuges

Practice AP Environmental Science unit 9 questions

Try stimulus-based AP practice questions and written prompts after you review the notes.

Example stimulus-based MCQs

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Stimulus-based practice question

Wildlife biologists hypothesized that constructing vegetated overpasses across major highways would increase gene flow and restore genetic diversity in isolated populations of an endangered mammalian carnivore within ten years. They measured genetic diversity (mean heterozygosity) in a fragmented population for five years before an overpass was built, and for ten years after construction. The graph displays the genetic monitoring results.

Question

Which interpretation of the genetic data relative to the hypothesis is most accurate?

The data refute the hypothesis because genetic diversity failed to increase during the ten years following overpass construction.

The data support the hypothesis because the overpass successfully prevented any further decline in the population's heterozygosity.

The data are inconclusive because fifteen years is an insufficient timeframe to measure any changes in mammalian genetic diversity.

The data strongly support the hypothesis since the genetic diversity stabilized immediately after the wildlife overpass was built.

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Stimulus-based practice question

Land managers hypothesized that a pre-emergent herbicide would reduce invasive cheatgrass density by at least 80% and reduce native bunchgrass density by at least 30%. They compared treated plots with untreated control plots after one growing season. The figure shows plant density in stems/m² for both species.

Question

Which interpretation of the figure best evaluates the herbicide hypothesis?

The data partially support the hypothesis; cheatgrass declined 85%, but bunchgrass declined only 5%.

The data fully support the hypothesis because both cheatgrass and native bunchgrass densities decreased.

The data refute the hypothesis because cheatgrass did not decline by the predicted 80%.

The data are inconclusive because native bunchgrass density increased after herbicide application.

Example FRQs

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FRQ

Atmospheric carbon dioxide and ocean acidification impacts

2. Atmospheric carbon dioxide (CO2CO_2) concentrations have increased from 280 parts per million (ppm) in preindustrial times to over 420 ppm today. This increase in CO2CO_2 and other greenhouse gases has led to rising global temperatures and significant changes in ocean chemistry. These changes are affecting marine ecosystems and the species that depend on them.

Figure 1. Atmospheric CO2 Concentration (ppm) and Ocean Surface pH from 1800 to 2020 (dual y-axes, two lines).

Figure 1
A.

Based on the data in Figure 1, identify the relationship between atmospheric CO2CO_2 concentration and ocean pH from 1800 to 2020.

B.

Identify the greenhouse gas, other than carbon dioxide, that has the highest global warming potential (GWP) over a 100-year timeframe.

Figure 2. Characteristics of Two Marine Regions (Region A: coral reef ecosystem; Region B: polar ocean ecosystem).

Figure 2
C.

Based on Figure 2, identify which region (A or B) would be most directly affected by increases in ocean temperature due to thermal expansion of water.

D.

Explain how increased atmospheric CO2CO_2 leads to the change in ocean pH shown in Figure 1.

E.

Describe one specific negative effect of decreased ocean pH on the reef-building corals in Region A.

F.

Propose one realistic solution that could reduce the rate of coral reef decline in Region A.

G.

Describe how the loss of sea ice in Region B threatens ice-dependent seal populations.

H.

Justify the solution you proposed in part F by explaining one additional environmental benefit, other than reducing coral decline.

I.

Describe one way that invasive species introductions, facilitated by warming ocean temperatures, can threaten native biodiversity in marine ecosystems.

J.

Describe one strategy, other than the solution proposed in part F, that could be used to protect endangered marine species from the impacts of climate change.

FRQ

Ocean acidification impacts on coral reef ecosystems

1. Coral reefs are among the most biodiverse ecosystems on Earth, providing habitat for approximately 25% of all marine species. Atmospheric carbon dioxide (CO2CO_2) dissolves in ocean water, forming carbonic acid (H2CO3H_2CO_3), which lowers the pH of seawater in a process called ocean acidification.

A.

Describe one ecosystem service provided by coral reef ecosystems.

B.

Explain how increasing atmospheric CO2CO_2 concentrations lead to ocean acidification.

Figure 1. Coral Calcification Rate and Seawater pH

Figure 1
C.

Based on the data in Figure 1, identify the coral calcification rate at a seawater pH of 8.0.

D.

Based on the data in Figure 1, describe the relationship between seawater pH and coral calcification rate.

Figure 2. Fish Species Richness and Seawater pH at Coral Reef Sites

Figure 2
E.

Scientists hypothesized that fish species richness would decrease if ocean pH dropped below 8.0. Describe how the data in Figure 2 support this hypothesis.

F.

Marine invertebrate biodiversity is essential for maintaining healthy ocean ecosystems. A group of students investigated the effect of ocean acidification on marine invertebrate species richness. They obtained two seawater aquarium tanks and adjusted the pH of one tank to 7.9 (low pH treatment) and maintained the other tank at 8.2 (control pH). The students collected marine invertebrate samples from a local tide pool and randomly assigned equal numbers of each species to both tanks. After 30 days, they identified and counted the number of different invertebrate species surviving in each tank.

i.

Identify the independent variable in the students' investigation.

ii.

Identify the dependent variable in the students' investigation.

Site

Species A

Species B

Species C

Species D

Species E

Species F

Low pH site (7.9)

X

X

Control pH site (8.2)

X

X

X

X

X

G.

The data from the student investigation of marine invertebrate diversity are shown in the following table. An 'X' in the table indicates that the species was present at that site after 30 days.

i.

Explain why the invertebrate community at the control pH site would be more resilient to environmental disturbances than the invertebrate community at the low pH site.

ii.

Explain how the results of the investigation could be affected if the students had used different initial numbers of each species in the two tanks.

H.

Describe one effect that increasing ocean temperatures can have on coral reef ecosystems. Ocean warming is another consequence of increased greenhouse gas emissions.

FRQ

Industrial aquaculture, ocean acidification, marine ecosystem pressures

3. Coastal nations increasingly rely on industrial-scale aquaculture facilities to meet global seafood demand. These operations contribute to atmospheric CO₂ emissions through energy use and to local water quality changes. Marine ecosystems face additional pressures from warming oceans, acidification, and invasive species introduction through ballast water discharge from international shipping vessels.

A.

Identify one greenhouse gas, other than carbon dioxide, that contributes to climate change.

B.

Describe how coral bleaching occurs as a specific consequence of increased ocean temperatures.

C.

Explain how increased atmospheric CO₂ concentrations lead to ocean acidification and negatively impact shell-forming marine organisms.

D.

Calculate the percent reduction in diesel fuel consumption between 2023 and 2024. Show your work. An industrial aquaculture facility operates diesel generators to power water circulation pumps and aeration systems. In 2023, the facility consumed 4.8 × 10⁵ liters of diesel fuel. After installing solar panels and energy-efficient pumps in 2024, diesel consumption decreased to 2.7 × 10⁵ liters.

E.

Calculate the number of metric tons of carbon credits the facility must purchase to offset all CO₂ emissions from diesel combustion in 2024. Show your work. Combustion of diesel fuel releases 2.68 kg of CO₂ per liter of fuel burned. After the 2024 upgrades described in part D, the aquaculture facility reduced its annual diesel consumption to 2.7 × 10⁵ liters. The facility operator wants to offset all remaining CO₂ emissions by purchasing carbon credits. Carbon credits are sold in units of metric tons (1 metric ton = 1,000 kg).

F.

Propose a realistic solution that port authorities could implement to prevent future introduction of aquatic invasive species through ballast water discharge. International cargo ships discharge ballast water into coastal harbors, introducing non-native marine species that can become invasive. A Mediterranean mussel species was detected in a harbor adjacent to several aquaculture facilities and threatens to outcompete native filter-feeding bivalves.

G.

Calculate the total mass of carbon, in kilograms, that will be sequestered over the entire 15-year duration of the project. Show your work. A coastal protection initiative aims to restore kelp forest ecosystems that absorb dissolved CO₂ from seawater. Scientists estimate that healthy kelp forests sequester 1.2 kg of carbon per square meter per year. The restoration project will establish 3.5 × 10⁶ square meters of kelp forest. The project will operate for 15 years before requiring significant maintenance.

Key terms

TermDefinition
Chlorofluorocarbons (CFCs)Synthetic compounds containing carbon, chlorine, and fluorine; primary anthropogenic cause of stratospheric ozone depletion and also potent greenhouse gases; phased out under the Montreal Protocol.
Ozone LayerRegion of the stratosphere with high ozone (O3) concentration that absorbs UV-B radiation, protecting life on Earth from increased skin cancer and cataract risk.
Montreal ProtocolInternational agreement that phased out production of ozone-depleting substances, primarily CFCs; widely regarded as a successful global environmental policy.
Hydrofluorocarbons (HFCs)CFC substitutes that do not deplete the ozone layer because they contain no chlorine, but many have high global warming potential, creating a climate trade-off.
Global warming potential (GWP)A measure of how much heat a greenhouse gas traps relative to CO2 (GWP = 1) over 100 years; CFCs rank highest, followed by nitrous oxide, then methane.
residence timeHow long a gas remains in the atmosphere; water vapor has a short residence time and does not accumulate, while CO2 and methane persist for decades to centuries and drive long-term warming.
ice and snow albedo feedbackA positive feedback loop in which melting ice exposes darker surfaces that absorb more solar energy, causing further warming and more melting; explains why polar regions warm faster than the tropics.
ocean conveyor beltGlobal thermohaline circulation that distributes heat through the world's oceans; can slow when freshwater from melting ice reduces the salinity-driven density differences that drive it.
Coral BleachingThermal stress causes corals to expel their symbiotic zooxanthellae algae, turning white; prolonged bleaching leads to coral death because zooxanthellae provide most of the coral's energy.
ZooxanthellaePhotosynthetic algae living symbiotically inside coral tissue; their expulsion during bleaching deprives corals of nutrients and is caused by elevated sea surface temperatures.
Calcium CarbonateThe mineral used by corals, oysters, and other calcifying organisms to build shells and skeletons; less available as ocean pH drops due to acidification.
Generalist speciesSpecies that tolerate a wide range of environmental conditions and use varied food sources; this flexibility helps invasive species establish and outcompete native specialists.
habitat corridorsConnected strips of habitat linking fragmented patches, allowing organisms to move between areas, maintaining gene flow and reducing local extinction risk.
Sea-Level RiseLong-term increase in average ocean height caused by two mechanisms: melting ice sheets and glaciers adding water volume, and thermal expansion of warming seawater.

Common unit 9 mistakes

Confusing ozone depletion with the greenhouse effect

These are two separate problems. CFCs deplete stratospheric ozone by releasing chlorine radicals, increasing UV-B at the surface. The greenhouse effect is about infrared radiation being trapped by greenhouse gases. CFCs contribute to both, but the mechanisms are completely different.

Saying water vapor is a major driver of climate change

Water vapor is a greenhouse gas, but it has a very short residence time in the atmosphere and does not accumulate the way CO2 or methane do. It amplifies warming as a feedback but is not the primary driver of anthropogenic climate change.

Mixing up the two causes of sea-level rise

Sea-level rise has two distinct mechanisms: melting ice sheets and glaciers add water volume, and thermal expansion occurs because warmer water takes up more space. Both must be mentioned for full credit on a free-response question.

Treating coral bleaching and ocean acidification as the same threat to coral

Bleaching is caused by thermal stress that expels zooxanthellae. Acidification reduces calcium carbonate availability, weakening coral skeletons. Both harm coral but through different mechanisms, and the exam may ask you to distinguish them.

Forgetting that HFCs are a trade-off, not a perfect solution

HFCs do not deplete ozone, which is why they replaced CFCs. But many HFCs have very high global warming potential, so switching to HFCs solves one environmental problem while potentially worsening another.

How this unit shows up on the AP exam

Cause-and-effect chains across Earth's systems

AP Environmental Science free-response questions frequently ask you to trace a human activity through multiple environmental consequences. In Unit 9, practice building chains such as: fossil fuel combustion increases CO2, which enhances the greenhouse effect, which warms oceans, which causes coral bleaching and disrupts marine food webs. Being able to write these chains with specific mechanisms (not just general statements) is the core skill tested.

Propose and evaluate solutions with trade-offs

The exam often asks you to propose a realistic solution to an environmental problem and explain why it works or identify a limitation. Unit 9 has several built-in trade-offs to practice with: HFCs solve ozone depletion but worsen climate change; biological control of invasive species can introduce new ecological risks; captive breeding helps endangered species but does not address the habitat loss driving endangerment.

Interpret data on global change indicators

Stimulus-based questions may present graphs of atmospheric CO2 concentration, ocean pH trends, temperature anomalies, or species population data. You should be able to identify the trend, connect it to a mechanism from Unit 9, and predict a consequence. Knowing the carbonic acid reaction and the GWP rankings gives you the quantitative and chemical vocabulary to answer these questions precisely.

Final unit 9 review checklist

  • Final Unit 9 review checklistUse this list to confirm you can handle every major idea in Unit 9 before the exam.
  • Explain the ozone depletion mechanismDescribe how CFCs release chlorine radicals in the stratosphere, why the Antarctic ozone hole forms in spring, and what health effects follow from increased UV-B exposure.
  • Compare greenhouse gases using GWP and residence timeRank CO2, methane, nitrous oxide, CFCs, and water vapor by GWP. Explain why water vapor does not drive long-term climate change despite being a greenhouse gas.
  • Trace climate change consequences through Earth's systemsConnect rising greenhouse gases to sea-level rise (two mechanisms), ice-albedo feedback, changes in Hadley cells and the jet stream, ocean conveyor belt slowdown, and permafrost methane release.
  • Distinguish ocean warming from ocean acidificationKnow the cause, chemical mechanism, and biological effects of each. Write the carbonic acid reaction and explain how lower pH reduces calcium carbonate for shell-building organisms.
  • Apply HIPPCO to biodiversity lossName all six HIPPCO factors, give a specific example of each, and explain how habitat fragmentation differs from outright habitat destruction in its effects on species.
  • Evaluate solutions for each global change problemFor each threat (ozone depletion, climate change, invasive species, endangered species), identify at least one specific mitigation strategy and explain its mechanism or trade-off.

How to study unit 9

Step 1: Ozone depletion and its reduction (9.1-9.2)Read the topic guides for 9.1 and 9.2. Draw the chlorine radical catalytic cycle from memory. Then practice explaining the HFC trade-off in one or two sentences. Check your understanding of the Montreal Protocol as a policy response.
Step 2: Greenhouse gases and climate consequences (9.3-9.5)Review the five principal greenhouse gases and their GWP rankings. Build a cause-and-effect chain from rising CO2 to sea-level rise, ice-albedo feedback, and circulation changes. Use the topic guides for 9.3, 9.4, and 9.5 to check your chain against the essential knowledge statements.
Step 3: Ocean warming and acidification (9.6-9.7)Write out the carbonic acid reaction without looking at notes. Then compare the mechanisms and effects of ocean warming versus acidification on coral. Use the topic guides for 9.6 and 9.7 to confirm you have the zooxanthellae and calcium carbonate details correct.
Step 4: Invasive and endangered species (9.8-9.9)List three real invasive species examples and explain why each succeeded using r-selection and generalist traits. Then list the factors that make a species vulnerable to extinction and match each to a specific protection strategy. Review the topic guides for 9.8 and 9.9.
Step 5: HIPPCO and full-unit synthesis (9.10)Write out HIPPCO from memory and give one concrete example per factor. Then practice connecting topics across the unit: for example, explain how climate change (9.3-9.5) contributes to habitat loss (9.10) and how that interacts with invasive species pressure (9.8). Use available practice questions to test your ability to apply these connections in writing.

More ways to review

Topic study guides

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Watch past review streams filtered to Unit 9 when you want a video walkthrough.

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Frequently Asked Questions

What topics are covered in APES Unit 9?

APES Unit 9: Global Change covers 10 topics: Stratospheric Ozone Depletion, Reducing Ozone Depletion, The Greenhouse Effect, Increases in Greenhouse Gases, Global Climate Change, Ocean Warming, Ocean Acidification, Invasive Species, Endangered Species, and Human Impacts on Biodiversity. Together they connect human activity to large-scale environmental consequences. See the full topic breakdown at /ap-enviro/unit-9.

How much of the APES exam is Unit 9?

APES Unit 9 makes up 15-20% of the AP exam, making it one of the heavier-weighted units. It covers global climate change, the greenhouse effect, ozone depletion, ocean warming, ocean acidification, invasive species, and human impacts on biodiversity. Expect several multiple-choice questions and possible FRQ components drawn from these topics.

What's on the APES Unit 9 progress check (MCQ and FRQ)?

The APES Unit 9 progress check includes both MCQ and FRQ parts that pull from all 10 topics in the unit. The MCQ section tests concepts like the greenhouse effect, stratospheric ozone depletion, ocean acidification, and invasive species. The FRQ part typically asks you to explain causes and consequences of global climate change or human impacts on biodiversity, and may ask you to propose solutions. For matched practice questions that mirror the progress check format, visit /ap-enviro/unit-9.

How do I practice APES Unit 9 FRQs?

APES Unit 9 FRQs most often focus on global climate change, the greenhouse effect, biodiversity loss, and ocean acidification. These questions typically ask you to identify causes, describe environmental consequences, and propose realistic solutions or policies. To practice, write out full responses to past prompts, check that you use precise vocabulary like 'greenhouse gases' and 'stratospheric ozone', and time yourself at about 22 minutes per FRQ. Find Unit 9 FRQ practice at /ap-enviro/unit-9.

Where can I find APES Unit 9 practice questions?

The best place to find APES Unit 9 practice questions, including multiple-choice and practice test sets, is /ap-enviro/unit-9. That page has MCQ practice covering the greenhouse effect, ozone depletion, ocean warming, invasive species, and biodiversity. Working through unit-specific MCQs before a full practice test helps you spot which of the 10 topics still need attention.

How should I study APES Unit 9?

Start APES Unit 9 by building a cause-and-effect map that links human activities to outcomes like global climate change, biodiversity loss, and ocean acidification. Then study each of the 10 topics in order, since topics like The Greenhouse Effect (9.3) and Increases in Greenhouse Gases (9.4) directly set up Global Climate Change (9.5). Use diagrams for the greenhouse effect and ozone depletion cycles, make a comparison chart for invasive vs. endangered species, and practice explaining solutions out loud since FRQs reward clear, specific reasoning. Finish each study session with a short MCQ set to check retention. All topic guides and practice are at /ap-enviro/unit-9.

Ready to review Unit 9?Start with the notes, check the topic cards, and use the practice or resource links when they are available for this course.