Rapid heat discharge during deep-sea eruptions generates megaplumes and disperses tephra

The footprint of column collapse regimes on pyroclastic flow temperatures and plume heights

Theoretical model for the proportion of particles reaching the umbrella

Web-Based Reanalysis Intercomparison Tools (WRIT) for Analysis and Comparison of Reanalyses and Other Datasets in: Bulletin of the American Meteorological Society Volume 95 Issue 11 (2014)

The effect of vent fluid salinity on the magnitude and sign of the D

Rapid heat discharge during deep-sea eruptions generates megaplumes and disperses tephra

Deep sea explosive eruptions may be not so different from subaerial eruptions

Generation of hydrothermal megaplumes by cooling of pillow basalts at mid- ocean ridges

T08C-07 transect showing (a) dE/dt anomalies, (b) DNTU contours and CTD

Understanding and modeling tephra transport: lessons learned from the 18 May 1980 eruption of Mount St. Helens

Rapid heat discharge during deep-sea eruptions generates megaplumes and disperses tephra

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PDF) Rapid heat discharge during deep-sea eruptions generates megaplumes and disperses tephra

PDF] Helium, heat, and the generation of hydrothermal event plumes at mid- ocean ridges

Deep sea explosive eruptions may be not so different from subaerial eruptions