Long-range transport of giant mineral aerosol particles

Document Type

Article

Date of Original Version

1-1-1988

Abstract

Several recent studies have shown that large quantities of mineral dust from eastern Asia are transported through the atmosphere to the North Pacific each spring1-5. The paucity of information on mineral fluxes during individual dust events prompted a coordinated effort, Asian Dust Input to the Oceanic System (ADIOS), which simultaneously measured mineral fluxes in the atmosphere and upper water column during such an event. In March 1986 a major dust outbreak in China moved over the North Pacific Ocean and was detected downstream using changes in particle number, size and composition. Most striking was the presence of 'giant' (>75-μm) silica minerals found in atmospheric as well as water-column samples at the ADIOS sampling site (26° N, 155° W). Their appearance more than 10,000 km from their source cannot be explained using currently acknowledged atmospheric transport mechanisms. Furthermore, the large wind-blown minerals that dominated our samples are extremely rare in the long-term sedimentary record in the North Pacific. © 1988 Nature Publishing Group.

Publication Title, e.g., Journal

Nature

Volume

336

Issue

6199

Share

COinS