Kilauea Volcanic Ash Induced a Massive Phytoplankton Bloom in the Nutrient-Poor North Pacific Subtropical Gyre

Abstract

Kilauea volcano is one of the most active volcanoes in the world with nearly continuous seismic activity from 1983 to 2018. In May 2018, the Kilauea volcano erupted and released volcanic ash into the atmosphere. Carried by easterly winds, the volcanic ash plume dispersed westward and by June 2018, the plume was observed over the central part (150 degrees E to 160 degrees W) of the nutrient-poor North Pacific Subtropical Gyre (NPSG). Coincident with precipitation during the same period, anomalously high dust deposition comprised mostly of wet dust was observed over the same region. Consequently, patches of high chlorophyll a (chl a) waters were observed approximately 5 degrees north of the high dust deposition area from the middle of June to early August 2018 via satellite images. The phytoplankton bloom peaked in July encompassing >1.5 million km(2), about 5 or 50 times the size of Malaysia or Taiwan, respectively. In addition to the large dust deposition, shoaling of the mixed layer in the range of 25-50 m is believed to have concentrated the bloom within the optical depth detected by satellite. Net primary production and export production estimated from satellite observations show that the July 2018 bloom generated an additional 1.91 Tg C of net carbon production, and 0.34 Tg C was exported from the euphotic zone.