| Full text | |
| Author(s): Show less - |
Scholz, Wiebke
;
Shen, Jiali
;
Aliaga, Diego
;
Wu, Cheng
;
Carbone, Samara
;
Moreno, Isabel
;
Zha, Qiaozhi
;
Huang, Wei
;
Heikkinen, Liine
;
Jaffrezo, Jean Luc
;
Uzu, Gaelle
;
Partoll, Eva
;
Leiminger, Markus
;
Velarde, Fernando
;
Laj, Paolo
;
Ginot, Patrick
;
Artaxo, Paolo
;
Wiedensohler, Alfred
;
Kulmala, Markku
;
Mohr, Claudia
;
Andrade, Marcos
;
Sinclair, Victoria
;
Bianchi, Federico
;
Hansel, Armin
Total Authors: 24
|
| Document type: | Journal article |
| Source: | Atmospheric Chemistry and Physics; v. 23, n. 2, p. 26-pg., 2023-01-19. |
| Abstract | |
Dimethyl sulfide (DMS) is the primary natural contributor to the atmospheric sulfur burden. Observations concerning the fate of DMS oxidation products after long-range transport in the remote free troposphere are, however, sparse. Here we present quantitative chemical ionization mass spectrometric measurements of DMS and its oxidation products sulfuric acid (H2SO4), methanesulfonic acid (MSA), dimethylsulfoxide (DMSO), dimethylsulfone (DMSO2), methanesulfinic acid (MSIA), methyl thioformate (MTF), methanesulfenic acid (MSEA, CH3SOH), and a compound of the likely structure CH3S(O)(2)OOH in the gas phase, as well as measurements of the sulfate and methanesulfonate aerosol mass fractions. The measurements were performed at the Global Atmosphere Watch (GAW) station Chacaltaya in the Bolivian Andes located at 5240 m above sea level (a.s.l.). DMS and DMS oxidation products are brought to the Andean high-altitude station by Pacific air masses during the dry season after convective lifting over the remote Pacific ocean to 6000-8000 m a.s.l. and subsequent longrange transport in the free troposphere (FT). Most of the DMS reaching the station is already converted to the rather unreactive sulfur reservoirs DMSO2 in the gas phase and methanesulfonate (MS-) in the particle phase, which carried nearly equal amounts of sulfur to the station. The particulate sulfate at Chacaltaya is however dominated by regional volcanic emissions during the time of the measurement and not significantly affected by the marine air masses. In one of the FT events, even some DMS was observed next to reactive intermediates such as methyl thioformate, dimethylsulfoxide, and methanesulfinic acid. Also for this event, back trajectory calculations show that the air masses came from above the ocean (distance > 330 km) with no local surface contacts. This study demonstrates the potential impact of marine DMS emissions on the availability of sulfur containing vapors in the remote free troposphere far away from the ocean. (AU) | |
| FAPESP's process: | 17/17047-0 - Aerosol and clouds life cycles in Amazonia: biogenic emissions, biomass burning and impacts on ecosystem |
| Grantee: | Paulo Eduardo Artaxo Netto |
| Support Opportunities: | Research Program on Global Climate Change - Thematic Grants |