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40 vocabulary flashcards summarizing key concepts, terms, gases, epochs, impacts, and responses discussed in the climate-change lecture.
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Climate Change
Long-term alteration in the state of Earth’s climate system that persists for decades or longer.
Global Warming
Current trend of rising average global temperatures due to increased greenhouse gases.
Greenhouse Gas (GHG)
Atmospheric gas (e.g., CO₂, CH₄, N₂O) that traps heat and contributes to the greenhouse effect.
Greenhouse Effect
Warming of Earth as GHGs absorb and re-emit infrared radiation, acting like an insulating blanket.
Atmosphere
Layer of gases surrounding Earth; one of the climate subsystems affected by GHGs.
Hydrosphere
All liquid water on Earth, including oceans, lakes, rivers; absorbs heat and CO₂.
Cryosphere
Frozen water part of Earth (ice sheets, glaciers, sea ice, snow).
Lithosphere
Earth’s rigid outer crust and upper mantle; interacts with climate over geologic time.
Biosphere
Zone of all living organisms on Earth, influenced by and influencing climate.
Anthropogenic Climate Change
Climate change caused or accelerated by human activities, especially post-industrialization.
Industrial Revolution
19th-century shift to mass manufacturing and fossil-fuel energy that triggered rapid GHG rise.
IPCC
Intergovernmental Panel on Climate Change; UN body assessing climate science and impacts.
Carbon Dioxide (CO₂)
Major GHG (≈76 % of emissions) from fossil fuel use, industry, and deforestation.
Methane (CH₄)
Potent GHG (≈16 % of emissions) released from agriculture, waste, and fossil extraction.
Nitrous Oxide (N₂O)
GHG (≈6 % of emissions) emitted mainly by fertilizer use and industrial processes.
Fluorinated Gases
Synthetic, high-global-warming-potential gases from refrigeration and other industries.
Holocene
Current geological epoch (~11,700 yrs) with relatively stable climate supporting humans.
Pliocene
Epoch ~3 million years ago; CO₂ concentrations similar to today, temps 2–3 °C higher, sea level ~25 m higher.
Paris Agreement
2015 global treaty aiming to limit warming well below 2 °C, pursuing 1.5 °C above pre-industrial levels.
1.5–2 °C Temperature Limit
Target range scientists deem critical to avoid worst climate impacts.
Sea Level Rise
Increase in average ocean level from thermal expansion and melting ice sheets/glaciers.
Ocean Acidification
Decrease in seawater pH as oceans absorb excess atmospheric CO₂, harming calcifying species.
Ocean Warming
Increase in ocean heat content; drives coral bleaching, stronger storms, and sea-level rise.
Extreme Weather Events
More intense/frequent heatwaves, hurricanes, floods, and droughts linked to climate change.
Carbon Emission Sources by Sector
Energy (20 %), industry (12 %), agriculture/land use (10 %), transport (8 %), buildings (3 %), waste, etc.
Carbon Emission Sources by Geography
Disproportionate GHG output from high-emitting nations; others emit less but often face greater impacts.
Deforestation
Removal of forests, reducing CO₂ uptake and adding ~11 % to global CO₂ emissions.
Food-Water-Energy Nexus
Interconnected challenge of sustainably supplying food, water, and energy under climate pressure.
Cascading Impacts
Series of linked effects where primary climate changes trigger secondary social, ecological, or economic consequences.
Climate Change Mitigation
Efforts to reduce or prevent GHG emissions (e.g., renewable energy, efficiency).
Climate Change Adaptation
Adjustments in systems or behaviors to lessen harm from present or expected climate effects.
Engineering Design Uncertainty
Challenge of designing infrastructure amid shifting hazard frequency and magnitude due to climate change.
Indigenous Knowledge
Traditional observations and stories offering insights into environmental change and hazard history.
Climate Change Learning Outcomes
Ability to define climate change, describe its causes, and explain its impacts—key study focus.
Ice-Free Arctic
Projection that with 2 °C warming, Arctic Ocean could be ice-free in summer once per decade.
Ice Age
Extended period of widespread glaciation; evidence shows natural but slow climatic shifts over millions of years.
Ocean Heat Absorption
Process where oceans take up over 90 % of excess heat, moderating air temps but altering marine systems.
Coral Bleaching
Loss of symbiotic algae from coral due to heat or acidification stress, leading to reef decline.
Shell Dissolving
Chemical erosion of shells of oysters, clams, etc., as lower pH reduces carbonate availability.
Mass Extinction Events
Historical episodes where >75 % of species vanished; two occurred before the Holocene, highlighting climate’s impact on life.