Climatology
Ocean acidification refers to the process by which the ocean becomes more acidic due to increased absorption of carbon dioxide (CO2) from the atmosphere. As CO2 levels rise, a significant portion is absorbed by seawater, leading to chemical reactions that decrease the pH of the ocean. This change in acidity can disrupt marine ecosystems, affecting organisms that rely on calcium carbonate for their shells and skeletons, and has broader implications for climate variability and extreme weather events.
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