D. L. Wellman

TL;DR: Huebert et al. as discussed by the authors showed that aqueous phase conversion of sulfur dioxide dissolved in the water associated with sea-salt particles supported the production of 2-8 nmol m −3 of non-sea-salts sulfate (nssSO 4 = ) during the Marine Acrosol and Gas Exchange (MAGE) experimcnt intensives.

TL;DR: In this article, field observations during a series of 24 atmospheric sampling flights in winter, spring, summer, and fall of 1987 provided a preliminary climatology of selected trace chemicals above the central United States.

TL;DR: Aerosol size distribution data measured during the June 1992 Marine Aerosol and Gas Exchange experiment are analyzed to investigate the characteristics of fine marine aerosol particles measured over the North Atlantic near the Azores Islands as mentioned in this paper.

TL;DR: Sulfur dioxide (SO2) was measured with a pulsed fluorescence analyzer and filter pack system from the instrumented NOAA King Air aircraft in the GCE/CASE/WATOX project in 1988 and included a series of eight flights of 4-hour duration each.

TL;DR: Dimethyl sulfide (DMS) and atmospheric aerosols were sampled simultaneously over the Atlantic Ocean in the vicinity of Bermuda using the NOAA King Air research aircraft as mentioned in this paper, and the average non-sea-salt (nss)SO 4 2− concentrations were 1.9 and 1.0 μg m −3 (as SO 4 2 − ) for the total and the fine fractions in the boundary layer (BL) and 0.27 μgm −3 in the free troposphere (FT).