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The eruption plume rose as high as 10.8 km a.s.l.l
The amount correlates weakly with eruption plume height.
Fig. 9 a Growing eruption plume photographed immediately after the beginning of eruption.
The eruption plume altitude reached approximately 2 km (above the crater), according to visual measurements.
The eruption plume reached an estimated 10,000 m above sea level (Meteorological Research Institute 2016).
Scientists have calculated that an eruption plume stretched nearly 40 miles above sea level and electric storms ripped through the sky.
After the passage of the typhoon in the late night of July 1, no eruption plume was visible (Fig. 10d).
This water is considered to have been derived from the precipitation of water vapor contained in the eruption plume.
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Enhancement of spatial resolution and observation frequencies are very useful for analysis and monitoring of eruption plumes.
However, in the late evening, cameras occasionally captured vigorous eruption plumes rising from several sources (Fig. 13b).
These simulations rely on key input parameters such as the maximum height of eruption plumes and the mass eruption rate at the vent, which remain loosely constrained.
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