A topic in the Open Knowledge Graph — a free, open map of 15,495 topics and the order to learn them in.
Societies respond to climate change in two ways. Mitigation reduces the cause, by cutting greenhouse gas emissions or removing carbon dioxide from the air. Adaptation reduces the harm, by changing how people live and build so they can cope with the changes that happen. Because global warming rises nearly in proportion to the total CO₂ ever emitted, warming from CO₂ stops only when net CO₂ emissions reach zero. The 2015 Paris Agreement aims to hold warming well below 2°C above pre-industrial levels and to pursue efforts to limit it to 1.5°C.
Start with the idea of a carbon budget: show a graph of warming against cumulative CO₂ emissions and ask what has to happen for the line to stop rising. Then sort a list of real actions, such as solar farms, sea walls, methane leak repair, reforestation, heat warning systems, and drought-resistant crops, into mitigation, adaptation, or both. Finish by comparing the time scales: methane cuts slow warming within decades, while CO₂ already emitted keeps the climate warm for centuries.
You know the physical case for human-caused warming. This topic asks what can be done about it. Responses fall into two groups.
Mitigation tackles the cause. The largest source of emissions is burning coal, oil, and gas for electricity, heat, transport, and industry. Mitigation options include using less energy through efficiency, generating electricity from low-carbon sources such as wind, solar, hydro, and nuclear, and switching vehicles and heating to that clean electricity. Other options target non-CO₂ gases, such as fixing methane leaks from oil and gas systems and reducing methane from landfills and livestock. Protecting forests keeps carbon stored on land.
A key result from climate science shapes all of these choices. Warming rises almost in a straight line with the total amount of CO₂ emitted over time. That means a temperature limit is also a limit on total emissions, called a carbon budget. It also means CO₂-driven warming stops only when net emissions reach zero. The IPCC special report on 1.5°C found that limiting warming to 1.5°C with little or no overshoot requires global net CO₂ emissions to fall by about 45 percent from 2010 levels by 2030 and to reach net zero around 2050.
"Net" zero allows some emissions to continue if an equal amount is removed. Carbon dioxide removal includes planting forests, adding carbon to soils, and technologies such as direct air capture with underground storage. These methods are limited in scale and cost, so they mostly balance emissions that are hard to eliminate.
Adaptation deals with the effects. Some warming is already locked in, so communities plan for higher sea levels, stronger heat waves, heavier downpours, and droughts. Examples include sea walls and restored wetlands, heat-warning systems and cooling centers, drought-tolerant crops, and building codes for stronger storms. Adaptation has limits. Some low-lying places and ecosystems such as coral reefs cannot be fully protected if warming continues.
The two strategies support each other. The more mitigation succeeds, the less adaptation is needed. Policy frameworks such as the 2015 Paris Agreement coordinate national targets, while the earlier Montreal Protocol on ozone shows that a global treaty can cut a harmful emission sharply.
No topics depend on this one yet.