Warming / Climate Change & Ozone Loss

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Last updated 8:42 PM on 4/12/26
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82 Terms

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Is climate change new?

No. Climate has changed many times over Earth’s 4.7-billion-year history due to natural processes.

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Natural cause of past climate change: volcanic eruptions

Volcanoes release ash and gases that block sunlight and cool the Earth short-term.

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Natural cause of past climate change: solar cycles

Changes in solar output affect how much energy Earth receives.

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Natural cause of past climate change: continental drift

Moving continents change ocean currents and atmospheric circulation.

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Natural cause of past climate change: meteor impacts

Impacts release dust that blocks sunlight and alters climate.

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What are ice cores used for?

Ice cores trap ancient air bubbles that reveal past atmospheric gas composition.

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What do ice core gases tell scientists?

Past CO₂, methane, and temperature levels.

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What is dendrochronology?

The study of tree rings to determine past climate conditions.

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What do tree ring widths indicate?

Growing conditions such as temperature and rainfall.

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How far back do direct temperature records go?

To about the 1860s.

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When did satellite temperature data begin?

Around the 1960s.

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When did direct CO₂ measurements begin?

1958 (Mauna Loa data).

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What is the IPCC?

Intergovernmental Panel on Climate Change.

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Who created the IPCC and when?

The UN’s World Meteorological Organization in 1988.

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What does the IPCC do?

Reviews climate data, forms scientific consensus, makes predictions and recommendations.

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What is the greenhouse effect?

Gases absorb and re-radiate heat, trapping warmth in the troposphere.

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Is the greenhouse effect bad?

No—it is natural and necessary for life.

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What is enhanced greenhouse effect?

Increased greenhouse gases from human activities causing extra warming.

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What does “anthropogenic” mean?

Caused by humans.

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Other names for enhanced greenhouse warming

Global warming, climate change, AGW, ACC.

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Greenhouse gas: Carbon dioxide (CO₂)

Source: burning fossil fuels, deforestation, land clearing.

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Warming power of CO₂

Baseline = 1.

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Greenhouse gas: Methane (CH₄)

Sources: natural gas leaks, cow burps, rice paddies, landfills.

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Warming power of methane

25× stronger than CO₂.

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Greenhouse gas: Nitrous oxide (N₂O)

Source: bacterial breakdown of fertilizers, whipped cream propellants.

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Warming power of nitrous oxide

300× stronger than CO₂.

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Greenhouse gas: CFCs

Sources: refrigerants, aerosols, packing materials.

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Warming power of CFCs

1000× stronger than CO₂.

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Average global temperature increase

1.1°C (1.9°F).

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Cryosphere evidence of warming

Melting sea ice, ice caps, glaciers, and permafrost.

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What causes sea level rise?

Thermal expansion of water + melting ice.

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What are environmental refugees?

People displaced due to climate-related environmental changes.

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Role of oceans in climate

Absorb and release heat.

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Another ocean role

Distribute heat via currents.

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Third ocean role

Absorb and release CO₂.

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Why are clouds a climate “mystery”?

Different cloud types warm or cool the Earth.

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Altostratus clouds effect

Cool the Earth.

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Cirrus clouds effect

Warm the Earth.

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Role of global wind circulation cells

Distribute heat and moisture worldwide.

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What happens if wind circulation is disrupted?

Major global climate impacts.

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Soil impacts of climate change

Changes in temperature and rainfall increase erosion and reduce productivity.

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Methane release from melting ice

Increases warming via positive feedback loop.

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Methane release from swamps/marshes

Reduces biodiversity and increases warming.

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Ice-albedo feedback

Less ice  lower albedo  more heat absorbed  more warming  even less ice.

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Disease movement due to warming

Tropical diseases move into temperate regions.

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Marine species impact

Habitat loss from sea level rise and photic zone changes.

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What is coral bleaching?

Coral lose symbiotic algae, turn white, and may die.

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Big policy question about climate change

Do economic costs outweigh environmental benefits?

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Prevention strategy for climate change

Stop producing greenhouse gases.

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Why is cleanup difficult?

Greenhouse gases persist (like toothpaste back in the tube).

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What is carbon sequestration?

Capturing and storing carbon to reduce atmospheric CO₂.

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Simple sequestration method

Planting trees.

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What is CCS?

Carbon Capture and Storage.

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How does CCS work?

Capture CO₂ and inject it deep underground.

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Kyoto Protocol (1997)

International agreement to reduce greenhouse gas emissions.

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Paris Accord (2016)

Global agreement to limit climate change by reducing emissions.

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Transportation changes to reduce CO₂

Walk, bike, drive fuel-efficient vehicles.

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Thermostat changes

Adjust to reduce energy use.

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Home efficiency actions

Insulate and seal house.

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Lighting choice

Use energy-efficient lighting.

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Diet change

Reduce meat consumption.

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Laundry habit

Wash clothes in cold or warm water.

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Carbon offset action

Plant trees.

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Where is the ozone layer located?

Stratosphere.

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What is ozone chemically?

O₃.

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Role of the ozone layer

Filters harmful UV radiation.

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Why is ozone essential for life?

Prevents DNA damage and skin cancer.

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Why were CFCs popular?

Cheap, nonflammable, noncorrosive, non-toxic, effective.

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Why are CFCs bad?

Destroy ozone and are powerful greenhouse gases.

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Key atom responsible for ozone destruction

Chlorine (Cl).

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Why is chlorine dangerous to ozone?

It is regenerated and destroys many ozone molecules.

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When does the polar vortex form?

Antarctic winter (June–August).

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What happens inside the polar vortex?

Ice crystals collect CFCs.

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What triggers ozone destruction in spring?

Sunlight returns in October.

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What happens when the vortex breaks up?

Ozone-depleted air spreads over the Southern Hemisphere.

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Human health effect

Increased skin cancer.

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Effect on phytoplankton

Killed by UV, reducing oxygen production.

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Effect on crops

Lower crop yields.

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Air pollution effect

Increased photochemical smog.

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How can ozone depletion be prevented?

Eliminate ODCs and use substitutes (e.g., HCFCs).

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Montreal Protocol (1987)

International treaty reducing ozone-depleting chemicals.

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Copenhagen Protocol (1992)

Strengthened restrictions on CFCs and ODCs.