Dr. Johan Gilchrist
NSF EAR Postdoctoral Fellow
University of Oregon
University of Oregon
Our research featured in the May 2023 issue of Nature Geoscience explores how the terraced slopes of submarine caldera volcanoes, such as Santorini, Greece, can be used to estimate elusive eruption source conditions. We show that fountain physics causes caldera-forming eruption columns to collapse periodically as doughnut shaped sedimentation waves that impact the sea surface to generate tsunamis, surfing hot rock avalanches, and submarine pyroclastic density currents that build terraced deposits on the seafloor. Our results may help explain why large caldera-forming eruptions, like the Jan 15, 2022 eruption of Hunga Tonga Hunga-Ha'apai, can have surprisingly little impact on climate.
Listen to my overview of our work on CBC Radio's Quirks and Quarks:
https://www.cbc.ca/radio/quirks/quirks-and-quarks-april-22-2023-1.6817336
NASA GOES-West Satellite view of the January 15, 2022 climactic eruption of Hunga Tonga Hunga Ha'apai volcano. Photo credit: NOAA.
Dr. Johan Gilchrist (he/him/his)
NSF EAR Postdoctoral Fellow
Dept. Earth Sciences
University of Oregon
Volcanology 206
1255 E 13th Avenue
Eugene, OR 97403
jgilchr2 @ uoregon dot edu