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Visual Review
AP Environmental Science Unit 9 Visual Review
A 10-slide visual walkthrough of every Topic 9.1-9.10 concept — ozone depletion, the greenhouse effect, ocean warming and acidification, invasive and endangered species, and human impacts on biodiversity — built right into the page.
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TOPIC 9.1
Stratospheric Ozone Depletion
stratospheric ozone (O₃) layer
CFC
UV breaks
off Cl atom
Cl
O₃
Cl destroys O₃,
is regenerated —
repeats 1000s of times
Why the ozone layer matters
Stratospheric ozone absorbs most incoming UV
radiation, shielding life below from radiation
damage — skin cancer, cataracts, and crop
damage all increase as this layer thins.
One chlorine atom, thousands of hits
CFCs (once common in refrigerants and
aerosols) release chlorine when broken down
by UV light. Each chlorine atom acts as a
catalyst, destroying thousands of O3 molecules.
This ozone layer protects us from UV; ground-level ozone (7.2) is a harmful pollutant — don't mix up the two.
The Review Hub · AP Environmental Science Unit 9
TOPIC 9.2
Reducing Ozone Depletion
ozone-depleting emissions
1987 (Montreal Protocol) → today
treaty signed
The Montreal Protocol (1987)
A global treaty that phased out CFCs and
other ozone-depleting chemicals, replacing
them with safer alternatives in refrigeration
and aerosols.
The exam's favorite success story
Nearly every country ratified it, and the
ozone layer is now measurably recovering —
proof that global cooperation CAN reverse an
atmospheric crisis when the cause is narrow.
Compare this to climate change (9.3-9.5): a single, well-defined cause made ozone recovery far easier to negotiate.
The Review Hub · AP Environmental Science Unit 9
TOPIC 9.3
The Greenhouse Effect
sunlight (visible) in
Earth's surface
infrared (heat) out
greenhouse gas layer (traps IR)
A natural, necessary process
Sunlight passes through the atmosphere and
warms Earth's surface, which re-radiates that
energy as infrared (heat). Without ANY
greenhouse effect, Earth would be far too cold for life.
The problem is the ENHANCED effect
Greenhouse gases (CO2, methane, water vapor)
absorb and re-emit that outgoing infrared
radiation back toward the surface. MORE of
these gases traps more heat — warming the planet.
The mechanism is about infrared, not visible light — sunlight passes through greenhouse gases easily; outgoing heat doesn't.
The Review Hub · AP Environmental Science Unit 9
TOPIC 9.4
Increases in Greenhouse Gases
Fossil fuel combustion
The single largest source of
CO2 — power plants, cars,
industry (Unit 6).
Agriculture
Livestock (methane from
digestion) and fertilizer
(nitrous oxide, N2O).
Deforestation
Removes a carbon SINK and
releases stored carbon —
a double hit (recall 1.4).
Two gases, two different strengths
CO2 is by far the most ABUNDANT greenhouse gas, so it drives the most total warming. Methane (CH4) is far
less abundant but traps roughly 25-80x more heat per molecule (depending on timeframe) — so livestock and
landfill methane punch well above their weight despite the smaller quantity released.
Ounce for ounce methane is far more potent than CO2, but it also breaks down faster — both facts matter for policy.
The Review Hub · AP Environmental Science Unit 9
TOPIC 9.5
Global Climate Change
Sea level rise
Thermal expansion +
melting ice sheets
threaten coastal cities.
Extreme weather
More intense storms,
droughts, and heat
waves.
Shifting ranges
Species migrate poleward
or to higher elevation as
their climate niche moves.
Climate vs. weather
A single cold day doesn't disprove warming — climate describes long-term AVERAGE
conditions over decades, while weather is what happens day to day. Climate change also
increases VARIABILITY, which is why extreme weather of all kinds becomes more common,
not just heat.
Topics 9.6 and 9.7 zoom into two specific consequences of this warming that deserve their own deep dive — the ocean.
The Review Hub · AP Environmental Science Unit 9
TOPIC 9.6
Ocean Warming
healthy
coral
algae symbionts give color
warming
bleached
coral
The ocean absorbs most excess heat
Over 90% of the extra heat trapped by
enhanced greenhouse gases goes into the
ocean, not the atmosphere — buffering air
temperatures but steadily warming the sea.
Coral bleaching
Heat stress causes coral to expel the
symbiotic algae living in their tissue — the
same algae that give coral its color AND
much of its food, via photosynthesis.
Bleached coral isn't dead yet, but it's starving — if warm water persists, the reef collapses.
The Review Hub · AP Environmental Science Unit 9
TOPIC 9.7
Ocean Acidification
CO₂
+ H₂O
carbonic acid
pH ↓
shell
(CaCO₃)
acid dissolves shell
A separate mechanism from warming
The ocean absorbs roughly a quarter of
human CO2 emissions directly. Dissolved CO2
reacts with water to form carbonic acid,
lowering ocean pH — this is CHEMISTRY, not heat.
Shell- and skeleton-builders at risk
Lower pH makes it harder for organisms to
build calcium carbonate shells and skeletons
— threatening corals, oysters, and the tiny
plankton that anchor the entire marine food web.
Same CO2, two ocean crises: warming (physics — heat absorption) and acidification (chemistry — CO2 dissolving) act independently.
The Review Hub · AP Environmental Science Unit 9
TOPIC 9.8
Invasive Species
native
established niche,
natural predators
introduced
invasive
no natural predators,
outcompetes natives
Why they take over
Introduced species (accidentally or
deliberately) often arrive without the
predators, parasites, or diseases that kept
their population in check back home.
Real-world examples
Zebra mussels clog waterways and outcompete
native mussels; Burmese pythons have
decimated small mammal populations in the
Everglades — both reshape entire food webs.
Prevention (inspecting cargo, ballast water rules) is far cheaper than eradication once a species is established.
The Review Hub · AP Environmental Science Unit 9
TOPIC 9.9
Endangered Species
population size
time →
threatened
critically endangered
Main drivers
Habitat loss (Unit 5/8) is the single biggest
cause worldwide. Overharvesting (overfishing,
poaching) and invasive species (9.8) add
further pressure to already shrinking populations.
Small populations compound the risk
Once numbers fall low enough, reduced
genetic diversity (2.1) and difficulty finding
mates can accelerate decline even if the
original threat is later removed.
The IUCN Red List formalizes these risk categories — from Least Concern through Endangered to Extinct.
The Review Hub · AP Environmental Science Unit 9
TOPIC 9.10
Human Impacts on Biodiversity
BIODIVERSITY
LOSS
habitat loss
pollution
climate change
invasive species
Threats compound, not isolate
Rarely does one mechanism act alone. A
species facing habitat fragmentation is also
less able to shift its range as climate change
moves its viable habitat — the threats interact.
The course's central throughline
This is APES in one diagram: land use (Unit
5), pollution (Units 7-8), and global change
(9.1-9.9) all converge here — on the
biodiversity introduced all the way back in Unit 2.
This final topic is the whole course's synthesis question — every unit you've studied feeds into this one outcome.
The Review Hub · AP Environmental Science Unit 9
▤ Show all slides
How to use the visual review
Spend 30 seconds per slide before clicking next. Look at the diagram, then ask yourself: "Could I draw this from memory and explain it?"
Use the fullscreen button () on desktop for the best experience. Use arrow keys to navigate. Tap "Show all slides" to jump around.
This covers every one of Unit 9's 10 CED topics, from stratospheric ozone depletion through human impacts on biodiversity.