Abstract
To understand better the spread of ash from volcanic eruptions penetrating into the stratosphere, laboratory experiments are performed using a recently developed light attenuation technique to measure the deposit of sediments from a particle-bearing plume rising in stratified fluid. The results are used to calibrate an adaptation of a plume model that accounts for particle settling and re-entrainment.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have