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DOI10.5194/acp-22-10023-2022
Secondary aerosol formation in marine Arctic environments: a model measurement comparison at Ny-angstrom lesund
Xavier, Carlton; Baykara, Metin; Wollesen de Jonge, Robin; Altstaedter, Barbara; Clusius, Petri; Vakkari, Ville; Thakur, Roseline; Beck, Lisa; Becagli, Silvia; Severi, Mirko; Traversi, Rita; Krejci, Radovan; Tunved, Peter; Mazzola, Mauro; Wehner, Birgit; Sipila, Mikko; Kulmala, Markku; Boy, Michael; Roldin, Pontus
发表日期2022
ISSN1680-7316
EISSN1680-7324
起始页码10023
结束页码10043
卷号22期号:15页码:21
英文摘要In this study, we modeled the aerosol particle formation along air mass trajectories arriving at the remote Arctic research stations Gruvebadet (67ma.s.l.) and Zeppelin (474ma.s.l.), Ny-Alesund, during May 2018. The aim of this study was to improve our understanding of processes governing secondary aerosol formation in remote Arctic marine environments. We run the Lagrangian chemistry transport model ADCHEM, along air mass trajectories generated with FLEXPART v10.4. The air masses arriving at Ny-angstrom lesund spent most of their time over the open ice-free ocean. In order to capture the secondary aerosol formation from the DMS emitted by phytoplankton from the ocean surface, we implemented a recently developed comprehensive DMS and halogen multi-phase oxidation chemistry scheme, coupled with the widely used Master Chemical Mechanism (MCM). The modeled median particle number size distributions are in close agreement with the observations in the marine-influenced boundary layer near-sea-surface Gruvebadet site. However, while the model reproduces the accumulation mode particle number concentrations at Zeppelin, it overestimates the Aitken mode particle number concentrations by a factor of similar to 5 :5. We attribute this to the deficiency of the model to capture the complex orographic effects on the boundary layer dynamics at Ny-angstrom lesund. However, the model reproduces the average vertical particle number concentration profiles within the boundary layer (0-600ma.s.l.) above Gruvebadet, as measured with condensation particle counters (CPCs) on board an unmanned aircraft system (UAS). The model successfully reproduces the observed Hoppel minima, often seen in particle number size distributions at Ny-angstrom lesund. The model also supports the previous experimental findings that ion-mediated H2SO4-NH3 nucleation can explain the observed new particle formation in the marine Arctic boundary layer in the vicinity of Ny-angstrom lesund. Precursors resulting from gas- and aqueous-phase DMS chemistry contribute to the subsequent growth of the secondary aerosols. The growth of particles is primarily driven via H2SO4 condensation and formation of methane sulfonic acid (MSA) through the aqueous-phase ozonolysis of methane sulfinic acid (MSIA) in cloud and deliquescent droplets.
学科领域Environmental Sciences; Meteorology & Atmospheric Sciences
语种英语
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
WOS记录号WOS:000835747200001
来源期刊ATMOSPHERIC CHEMISTRY AND PHYSICS
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/273228
作者单位University of Helsinki; Istanbul Technical University; Lund University; Braunschweig University of Technology; North West University - South Africa; Finnish Meteorological Institute; University of Florence; Stockholm University; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Polari (ISP-CNR); Leibniz Institut fur Tropospharenforschung (TROPOS)
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Xavier, Carlton,Baykara, Metin,Wollesen de Jonge, Robin,et al. Secondary aerosol formation in marine Arctic environments: a model measurement comparison at Ny-angstrom lesund[J],2022,22(15):21.
APA Xavier, Carlton.,Baykara, Metin.,Wollesen de Jonge, Robin.,Altstaedter, Barbara.,Clusius, Petri.,...&Roldin, Pontus.(2022).Secondary aerosol formation in marine Arctic environments: a model measurement comparison at Ny-angstrom lesund.ATMOSPHERIC CHEMISTRY AND PHYSICS,22(15),21.
MLA Xavier, Carlton,et al."Secondary aerosol formation in marine Arctic environments: a model measurement comparison at Ny-angstrom lesund".ATMOSPHERIC CHEMISTRY AND PHYSICS 22.15(2022):21.
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