The Karl effect, named after Swedish chemist Svante Arrhenius, is a phenomenon in which increased levels of carbon dioxide (CO2) in the atmosphere lead to a warming of the Earth's surface. This is due to the fact that CO2 is a greenhouse gas, meaning it traps heat in the atmosphere and prevents it from escaping back into space.
The Karl effect is part of the broader concept of global warming, which refers to the overall increase in global temperatures over time. Human activities, such as the burning of fossil fuels and deforestation, have significantly increased the levels of CO2 in the atmosphere, contributing to the Karl effect and global warming.
The consequences of the Karl effect and global warming are significant and wide-ranging, including rising sea levels, more frequent and severe weather events, and ecosystem disruptions. Addressing the Karl effect and mitigating its impact is a critical challenge facing the world today.
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