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The condensation of water vapor in clouds, influenced by marine algae, is facilitated by the emission of aerosols. Some types of marine algae release organic compounds, such as dimethylsulfide (DMS), which can form sulfate aerosols in the atmosphere. These aerosols act as cloud condensation nuclei, providing surfaces for water vapor to condense upon, thereby enhancing cloud formation and potentially influencing local climate patterns. This process underscores the interconnectedness of marine ecosystems and atmospheric dynamics.

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