📘 On Sumbawa, the summit disappeared
Stand on the rim of Tambora's caldera and the missing mountain is the first thing you notice. The depression is about six kilometres wide; before April 1815, the summit rose roughly four kilometres above sea level. Tambora had shown warning
What you’ll learn
- Tambora removes a mountainExplain what the 1815 Tambora eruption changed locally and why its caldera records its scale.Tambora's collapse, deposits, and pyroclastic flows reveal an eruption large enough to affect the atmosphere.
- Krakatoa makes a different kind of shockCompare Krakatoa's 1883 eruption with Tambora by separating volcanic size, tsunami impact, and communication.Krakatoa's collapse and tsunamis show how geography and technology shape disaster.
- A volcano reaches the stratosphereTrace how sulfur dioxide becomes sulfate aerosol and changes sunlight, circulation, and regional climate.Volcanic aerosols produce temporary, uneven cooling rather than one uniform global winter.
- 1816 turns weather into historyConnect unusual 1816 weather to food systems, historical records, and cultural responses without oversimplifying causation.The year without a summer became a human crisis through vulnerable harvests, prices, movement, and imagination.
Questions this course answers
What most directly caused Tambora's longer-lived climate effect?
Stratospheric sulfur dioxide formed sulfate aerosols that scattered sunlight and altered radiation.
Why is Krakatoa a useful comparison with Tambora?
Krakatoa's coastal setting and collapse-generated tsunamis made its human impact distinctive.
What does “year without a summer” mean?
The phrase describes severe seasonal anomalies, not a literal planet-wide winter.
Why can a global forcing produce different local weather?
Circulation, oceans, geography, and season determine how a global disturbance appears locally.
Which chain best describes Tambora's influence on 1816?
That sequence connects the volcanic event to atmospheric chemistry, climate, and human consequences.
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