Global warming is the long-term increase in Earth’s average surface temperature, driven primarily by rising levels of greenhouse gases (especially CO2) from human activities. Arctic warming is occurring twice as fast as in other regions.
CO2 from burning fossil fuels is the most significant single driver of global warming, and it has accumulated in the atmosphere for centuries. Based on current trends, atmospheric CO2 concentrations will not peak this century. Only a reduction in emissions and the attainment of net-zero emissions will arrest the rise in concentrations, which doesn’t seem very likely in the current political environment. The result will be an increase in the magnitude and frequency of extreme weather events.
Global warming drives feedback that can amplify impacts (e.g., ice‑albedo feedback, permafrost carbon release). Impacts are widespread, including more frequent heatwaves, stronger storms, sea-level rise, shifting ecosystems, crop stress, and health risks.
Sea level rise is ongoing due to thermal expansion and melting ice; it will continue for centuries even if warming slows.
Limiting warming requires rapid, deep cuts in greenhouse gas emissions (because humanity has ignored it for so long).
New CO2 removal technologies, renewable energy sources, improved energy efficiency, increased use of electricity to displace fossil fuels, better land management, and scalable carbon capture are all required.
Timing matters. Near‑term emissions determine peak warming and the magnitude of many impacts, and delayed action increases the risk and cost of catastrophic events.
Countries and communities differ in their responsibilities and vulnerabilities—both mitigation and adaptation funding and planning are critical.
Many mitigation options are available now, like clean energy, improved energy efficiency, low‑carbon transport, and sustainable land use. We need to take our heads out of the sand, implement new climate-change response policies, increase the financial resources dedicated to combating climate change, and drive societal change. These will determine how many decades will witness increased warming and climate risks before a new climate balance is achieved – likely well into the next century if current trends continue.
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