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...

Full description

Bibliographic Details
Published in:Atmospheric Chemistry and Physics
Main Authors: 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
Format: Article in Journal/Newspaper
Language:English
Published: COPERNICUS GESELLSCHAFT MBH 2017
Subjects:
Online Access:https://oasis.postech.ac.kr/handle/2014.oak/50402
https://doi.org/10.5194/acp-17-9665-2017
id ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/50402
record_format openpolar
spelling 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
_version_ 1766315466587897856