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ToggleBlack Carbon (BC) is a fine particulate aerosol formed by incomplete combustion of fossil fuels, biofuels, and biomass—essentially the soot in the air. It is a component of PM₂.₅ and a potent climate-forcing agent, often second only to CO₂ in warming potential.
It is a short-lived climate pollutant—the average atmospheric lifetime of black carbon particles is 4-12 days.
It has a warming impact up to 1,500 times stronger than CO2 per unit of mass.
Black carbon is emitted during the incomplete combustion of fossil fuels, wood, biomass, and waste. This process not only produces black carbon particles but also releases carbon dioxide (CO₂), carbon monoxide (CO), volatile organic compounds (VOCs), and organic carbon — collectively referred to as soot.
Major Black Carbon Emitting Sectors
Note: Household energy accounts for nearly half of global black carbon emissions globally.
Reducing black carbon (BC) emissions is crucial for both climate mitigation and public health. Unlike CO₂, black carbon stays in the atmosphere for only a few days to weeks, so cutting emissions can deliver quick climate and air quality benefits.
Black carbon is a major short-lived climate pollutant that significantly contributes to global warming, glacial melting, disrupted rainfall patterns, and severe health impacts. Unlike carbon dioxide, it persists in the atmosphere for a short time, meaning that cutting black carbon emissions can yield immediate climate and health benefits. Tackling black carbon through clean energy adoption, improved waste management, sustainable agriculture, and vehicle emission control can serve as a dual solution—fighting both climate change and air pollution.
Q1. What is black carbon?
A: Black carbon is a component of fine particulate matter (PM2.5), produced by the incomplete combustion of fossil fuels, biomass, and waste. It is also commonly referred to as “soot.”
Q 2. How does black carbon affect the climate?
A: In the atmosphere, black carbon absorbs sunlight and heats the air. When it settles on ice or snow, it reduces reflectivity (albedo), causing faster melting, especially in the Himalayas and Arctic.
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