This data set is based on a prior density model, combined with satellite gravity anomaly data, and uses the variable density interface iterative inversion algorithm in spherical coordinates to estimat
Holdt_et_al_2022_SupportingInformation: Residual depth/topographic measurements published in the article "Densely sampled global dynamic topographic observations and their significance" Citation: Hol
Compute of the mass flow rate (at stationary condition) feeding the co-ignimbrite as the ratio between the initial mass flow rate and the total deposition rate.
