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Biogeochemical controls on climatically active gases and atmospheric sulfate aerosols in the western Pacific.

Authors :
Xu F
Zhang HH
Yan SB
Sun MX
Wu JW
Yang GP
Source :
Environmental research [Environ Res] 2023 Mar 01; Vol. 220, pp. 115211. Date of Electronic Publication: 2023 Jan 02.
Publication Year :
2023

Abstract

The Pacific Ocean plays an important role in regulating the budget of climatically active gases and the burden of sulfate aerosols. Here, a field investigation was conducted to clarify the key processes and factors controlling climatically active gases, including dimethyl sulfide (DMS), carbonyl sulfide (OCS), carbon disulfide (CS <subscript>2</subscript> ), and carbon dioxide (CO <subscript>2</subscript> ), in both surface seawater and the lower atmosphere of the western Pacific. In addition, the relative contributions of different sources to atmospheric sulfate aerosols were quantitatively estimated, and their causes were explored. The maximum concentrations of DMS, OCS and CS <subscript>2</subscript> and the minimum partial pressure of CO <subscript>2</subscript> (pCO <subscript>2</subscript> ) were observed in the Kuroshio-Oyashio Extension. Kuroshio-induced mesoscale eddies brought abundant nutrients and organic matter from the subsurface layer of Oyashio into the euphotic layer, thus enhancing primary productivity and accelerating the photoreaction of organic matter. These processes led to higher concentrations of DMS, OCS and CS <subscript>2</subscript> and lower pCO <subscript>2</subscript> . However, the oligotrophic subsurface layer in the subtropical gyre and the strong barrier layer in the equatorial waters suppressed the upward fluxes of nutrients and organic matter, resulting in lower surface concentrations of DMS, OCS, and CS <subscript>2</subscript> in these areas. Being far from the continents, atmospheric concentrations of DMS, OCS and CS <subscript>2</subscript> and pCO <subscript>2</subscript> in the western Pacific generally were observed to depend on the local sea-to-air exchange and may be regulated by atmospheric oxidation and mixing of air masses. In general, oceanic DMS emissions played an important role in the formation of sulfate aerosols in the western Pacific (accounting for ∼19.5% of total sulfate aerosols), especially in the Kuroshio-Oyashio Extension (∼32.3%). These processes in seawater may also determine the variations and emissions of other climatically active gases from biogenic and photochemical sources.<br />Competing Interests: Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.<br /> (Copyright © 2023 Elsevier Inc. All rights reserved.)

Details

Language :
English
ISSN :
1096-0953
Volume :
220
Database :
MEDLINE
Journal :
Environmental research
Publication Type :
Academic Journal
Accession number :
36603657
Full Text :
https://doi.org/10.1016/j.envres.2023.115211