Observational evidence for the formation of DMS-derived aerosols during Arctic phytoplankton blooms
The connection between marine biogenic dimethyl sulfide (DMS) and the formation of aerosol particles in the Arctic atmosphere was evaluated by analyzing atmospheric DMS mixing ratio, aerosol particle size distribution and aerosol chemical composition data that were concurrently collected at Ny-Alesu...
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COPERNICUS GESELLSCHAFT MBH
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Online Access: | https://oasis.postech.ac.kr/handle/2014.oak/50402 https://doi.org/10.5194/acp-17-9665-2017 |
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ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/50402 2023-05-15T14:43:53+02:00 Observational evidence for the formation of DMS-derived aerosols during Arctic phytoplankton blooms Park, Ki-Tae Jang, Sehyun Lee, Kitack Yoon, Young Jun Kim, Min-Seob Park, Kihong Cho, Hee-Joo Kang, Jung-Ho Udisti, Roberto Lee, Bang-Yong Shin, Kyung-Hoon Jang, Sehyun Lee, Kitack 2017-08 https://oasis.postech.ac.kr/handle/2014.oak/50402 https://doi.org/10.5194/acp-17-9665-2017 English eng COPERNICUS GESELLSCHAFT MBH ATMOSPHERIC CHEMISTRY AND PHYSICS Meteorology & Atmospheric Sciences 1680-7316 https://oasis.postech.ac.kr/handle/2014.oak/50402 doi:10.5194/acp-17-9665-2017 28356 ATMOSPHERIC CHEMISTRY AND PHYSICS, v.17, no.15, pp.9665 - 9675 000407464800003 2-s2.0-85027378433 ATMOSPHERIC DIMETHYL SULFIDE CLOUD CONDENSATION NUCLEI NEW-PARTICLE FORMATION SULFURIC-ACID ISOTOPIC COMPOSITION ATLANTIC-OCEAN SVALBARD ISLANDS NY-ALESUND SULFATE NUCLEATION Article ART 2017 ftponangunivst https://doi.org/10.5194/acp-17-9665-2017 2022-10-20T20:30:27Z The connection between marine biogenic dimethyl sulfide (DMS) and the formation of aerosol particles in the Arctic atmosphere was evaluated by analyzing atmospheric DMS mixing ratio, aerosol particle size distribution and aerosol chemical composition data that were concurrently collected at Ny-Alesund, Svalbard (78.5 degrees N, 11.8 degrees E), during April and May 2015. Measurements of aerosol sulfur (S) compounds showed distinct patterns during periods of Arctic haze (April) and phytoplankton blooms (May). Specifically, during the phytoplankton bloom period the contribution of DMS-derived SO42- to the total aerosol SO42- increased by 7-fold compared with that during the proceeding Arctic haze period, and accounted for up to 70% of fine SO42- particles (<2.5 mu m in diameter). The results also showed that the formation of submicron SO42- aerosols was significantly associated with an increase in the atmospheric DMS mixing ratio. More importantly, two independent estimates of the formation of DMS-derived SO42- aerosols, calculated using the stable S-isotope ratio and the non-sea-salt SO42-/methanesulfonic acid ratio, respectively, were in close agreement, providing compelling evidence that the contribution of biogenic DMS to the formation of aerosol particles was substantial during the Arctic phytoplankton bloom period. 1 1 4 scie scopus Article in Journal/Newspaper Arctic Phytoplankton Svalbard Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) Arctic Svalbard Atmospheric Chemistry and Physics 17 15 9665 9675 |
institution |
Open Polar |
collection |
Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) |
op_collection_id |
ftponangunivst |
language |
English |
topic |
ATMOSPHERIC DIMETHYL SULFIDE CLOUD CONDENSATION NUCLEI NEW-PARTICLE FORMATION SULFURIC-ACID ISOTOPIC COMPOSITION ATLANTIC-OCEAN SVALBARD ISLANDS NY-ALESUND SULFATE NUCLEATION |
spellingShingle |
ATMOSPHERIC DIMETHYL SULFIDE CLOUD CONDENSATION NUCLEI NEW-PARTICLE FORMATION SULFURIC-ACID ISOTOPIC COMPOSITION ATLANTIC-OCEAN SVALBARD ISLANDS NY-ALESUND SULFATE NUCLEATION Park, Ki-Tae Jang, Sehyun Lee, Kitack Yoon, Young Jun Kim, Min-Seob Park, Kihong Cho, Hee-Joo Kang, Jung-Ho Udisti, Roberto Lee, Bang-Yong Shin, Kyung-Hoon Observational evidence for the formation of DMS-derived aerosols during Arctic phytoplankton blooms |
topic_facet |
ATMOSPHERIC DIMETHYL SULFIDE CLOUD CONDENSATION NUCLEI NEW-PARTICLE FORMATION SULFURIC-ACID ISOTOPIC COMPOSITION ATLANTIC-OCEAN SVALBARD ISLANDS NY-ALESUND SULFATE NUCLEATION |
description |
The connection between marine biogenic dimethyl sulfide (DMS) and the formation of aerosol particles in the Arctic atmosphere was evaluated by analyzing atmospheric DMS mixing ratio, aerosol particle size distribution and aerosol chemical composition data that were concurrently collected at Ny-Alesund, Svalbard (78.5 degrees N, 11.8 degrees E), during April and May 2015. Measurements of aerosol sulfur (S) compounds showed distinct patterns during periods of Arctic haze (April) and phytoplankton blooms (May). Specifically, during the phytoplankton bloom period the contribution of DMS-derived SO42- to the total aerosol SO42- increased by 7-fold compared with that during the proceeding Arctic haze period, and accounted for up to 70% of fine SO42- particles (<2.5 mu m in diameter). The results also showed that the formation of submicron SO42- aerosols was significantly associated with an increase in the atmospheric DMS mixing ratio. More importantly, two independent estimates of the formation of DMS-derived SO42- aerosols, calculated using the stable S-isotope ratio and the non-sea-salt SO42-/methanesulfonic acid ratio, respectively, were in close agreement, providing compelling evidence that the contribution of biogenic DMS to the formation of aerosol particles was substantial during the Arctic phytoplankton bloom period. 1 1 4 scie scopus |
author2 |
Jang, Sehyun Lee, Kitack |
format |
Article in Journal/Newspaper |
author |
Park, Ki-Tae Jang, Sehyun Lee, Kitack Yoon, Young Jun Kim, Min-Seob Park, Kihong Cho, Hee-Joo Kang, Jung-Ho Udisti, Roberto Lee, Bang-Yong Shin, Kyung-Hoon |
author_facet |
Park, Ki-Tae Jang, Sehyun Lee, Kitack Yoon, Young Jun Kim, Min-Seob Park, Kihong Cho, Hee-Joo Kang, Jung-Ho Udisti, Roberto Lee, Bang-Yong Shin, Kyung-Hoon |
author_sort |
Park, Ki-Tae |
title |
Observational evidence for the formation of DMS-derived aerosols during Arctic phytoplankton blooms |
title_short |
Observational evidence for the formation of DMS-derived aerosols during Arctic phytoplankton blooms |
title_full |
Observational evidence for the formation of DMS-derived aerosols during Arctic phytoplankton blooms |
title_fullStr |
Observational evidence for the formation of DMS-derived aerosols during Arctic phytoplankton blooms |
title_full_unstemmed |
Observational evidence for the formation of DMS-derived aerosols during Arctic phytoplankton blooms |
title_sort |
observational evidence for the formation of dms-derived aerosols during arctic phytoplankton blooms |
publisher |
COPERNICUS GESELLSCHAFT MBH |
publishDate |
2017 |
url |
https://oasis.postech.ac.kr/handle/2014.oak/50402 https://doi.org/10.5194/acp-17-9665-2017 |
geographic |
Arctic Svalbard |
geographic_facet |
Arctic Svalbard |
genre |
Arctic Phytoplankton Svalbard |
genre_facet |
Arctic Phytoplankton Svalbard |
op_relation |
ATMOSPHERIC CHEMISTRY AND PHYSICS Meteorology & Atmospheric Sciences 1680-7316 https://oasis.postech.ac.kr/handle/2014.oak/50402 doi:10.5194/acp-17-9665-2017 28356 ATMOSPHERIC CHEMISTRY AND PHYSICS, v.17, no.15, pp.9665 - 9675 000407464800003 2-s2.0-85027378433 |
op_doi |
https://doi.org/10.5194/acp-17-9665-2017 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
17 |
container_issue |
15 |
container_start_page |
9665 |
op_container_end_page |
9675 |
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1766315466587897856 |