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Measurement Report: Long-range transport and fate of DMS-oxidation products in the free troposphere derived from observations at the high-altitude research station Chacaltaya (5240 m a.s.l.) in the Bolivian Andes.

Authors :
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
Source :
EGUsphere; 9/23/2022, p1-42, 42p
Publication Year :
2022

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 H2SO4, MSA, DMSO, DMSO2, MSIA, MTF, CH3S(O)2OOH and CH3SOH in the gas-phase as well as measurements of the sulfate and methane- sulfonate aerosol mass fractions 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 long-range transport in the free troposphere (FT). Most of the DMS reaching the station is already converted to the rather unreactive sulfur reservoirs dimethyl sulfone (DMSO<subscript>2</subscript>) in the gas phase and methanesulfonate (MS<superscript>−</superscript>) 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, dimethyl sulfoxide, and methane sulfinic acid. Also for this event, backtrajectory calculations show, that the air masses came from above the ocean (distance >330 km) with no local sur- face 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. [ABSTRACT FROM AUTHOR]

Details

Language :
English
Database :
Complementary Index
Journal :
EGUsphere
Publication Type :
Academic Journal
Accession number :
159305593
Full Text :
https://doi.org/10.5194/egusphere-2022-887