Atmospheric DMS in the Arctic Ocean and Its Relation to Phytoplankton Biomass
We recorded and analyzed the atmospheric dimethyl sulfide (DMS) mixing ratios at a remote Arctic location (Svalbard; 78.5 degrees N, 11.8 degrees E) during phytoplankton bloom periods in the years 2010, 2014, and 2015 and found varying regional relationships between the atmospheric DMS and the exten...
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Online Access: | https://oasis.postech.ac.kr/handle/2014.oak/96047 https://doi.org/10.1002/2017GB005805 |
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ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/96047 2023-05-15T14:49:34+02:00 Atmospheric DMS in the Arctic Ocean and Its Relation to Phytoplankton Biomass Park, Ki-Tae Lee, Kitack Kim, Tae-Wook Yoon, Young Jun Jang, Eun-Ho Jang, Sehyun Lee, Bang-Yong Hermansen, Ove Lee, Kitack Jang, Sehyun 2018-03 https://oasis.postech.ac.kr/handle/2014.oak/96047 https://doi.org/10.1002/2017GB005805 English eng AMER GEOPHYSICAL UNION GLOBAL BIOGEOCHEMICAL CYCLES Environmental Sciences Geosciences, Multidisciplinary Meteorology & Atmospheric Sciences Environmental Sciences & Ecology Geology 0886-6236 https://oasis.postech.ac.kr/handle/2014.oak/96047 doi:10.1002/2017GB005805 31292 GLOBAL BIOGEOCHEMICAL CYCLES, v.32, no.3, pp.351 - 359 000430105900002 2-s2.0-85043319191 MARGINAL ICE-ZONE DIMETHYL SULFIDE BARENTS SEA BIOGENIC SULFUR AEROSOL SUMMER BLOOMS SALT VARIABILITY EMISSIONS phytoplankton Arctic Ocean air mass exposure prymnesiophytes Article ART 2018 ftponangunivst https://doi.org/10.1002/2017GB005805 2022-10-20T20:57:54Z We recorded and analyzed the atmospheric dimethyl sulfide (DMS) mixing ratios at a remote Arctic location (Svalbard; 78.5 degrees N, 11.8 degrees E) during phytoplankton bloom periods in the years 2010, 2014, and 2015 and found varying regional relationships between the atmospheric DMS and the extent of exposure of the air mass to the phytoplankton biomass in the ocean surrounding the observation site. The DMS production capacity of the Greenland Sea was estimated to be a factor of 3 greater than that of the Barents Sea, whereas the phytoplankton biomass in the Barents Sea was more than twofold than that in the Greenland Sea. These apparently contradictory results may be induced by the occurrence of a greater abundance of DMS-producing phytoplankton in the Greenland Sea than in the Barents Sea during the phytoplankton bloom periods. 1 1 N scie scopus Article in Journal/Newspaper Arctic Arctic Ocean Barents Sea Greenland Greenland Sea Phytoplankton Svalbard Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) Arctic Arctic Ocean Barents Sea Greenland Svalbard Global Biogeochemical Cycles 32 3 351 359 |
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 |
MARGINAL ICE-ZONE DIMETHYL SULFIDE BARENTS SEA BIOGENIC SULFUR AEROSOL SUMMER BLOOMS SALT VARIABILITY EMISSIONS phytoplankton Arctic Ocean air mass exposure prymnesiophytes |
spellingShingle |
MARGINAL ICE-ZONE DIMETHYL SULFIDE BARENTS SEA BIOGENIC SULFUR AEROSOL SUMMER BLOOMS SALT VARIABILITY EMISSIONS phytoplankton Arctic Ocean air mass exposure prymnesiophytes Park, Ki-Tae Lee, Kitack Kim, Tae-Wook Yoon, Young Jun Jang, Eun-Ho Jang, Sehyun Lee, Bang-Yong Hermansen, Ove Atmospheric DMS in the Arctic Ocean and Its Relation to Phytoplankton Biomass |
topic_facet |
MARGINAL ICE-ZONE DIMETHYL SULFIDE BARENTS SEA BIOGENIC SULFUR AEROSOL SUMMER BLOOMS SALT VARIABILITY EMISSIONS phytoplankton Arctic Ocean air mass exposure prymnesiophytes |
description |
We recorded and analyzed the atmospheric dimethyl sulfide (DMS) mixing ratios at a remote Arctic location (Svalbard; 78.5 degrees N, 11.8 degrees E) during phytoplankton bloom periods in the years 2010, 2014, and 2015 and found varying regional relationships between the atmospheric DMS and the extent of exposure of the air mass to the phytoplankton biomass in the ocean surrounding the observation site. The DMS production capacity of the Greenland Sea was estimated to be a factor of 3 greater than that of the Barents Sea, whereas the phytoplankton biomass in the Barents Sea was more than twofold than that in the Greenland Sea. These apparently contradictory results may be induced by the occurrence of a greater abundance of DMS-producing phytoplankton in the Greenland Sea than in the Barents Sea during the phytoplankton bloom periods. 1 1 N scie scopus |
author2 |
Lee, Kitack Jang, Sehyun |
format |
Article in Journal/Newspaper |
author |
Park, Ki-Tae Lee, Kitack Kim, Tae-Wook Yoon, Young Jun Jang, Eun-Ho Jang, Sehyun Lee, Bang-Yong Hermansen, Ove |
author_facet |
Park, Ki-Tae Lee, Kitack Kim, Tae-Wook Yoon, Young Jun Jang, Eun-Ho Jang, Sehyun Lee, Bang-Yong Hermansen, Ove |
author_sort |
Park, Ki-Tae |
title |
Atmospheric DMS in the Arctic Ocean and Its Relation to Phytoplankton Biomass |
title_short |
Atmospheric DMS in the Arctic Ocean and Its Relation to Phytoplankton Biomass |
title_full |
Atmospheric DMS in the Arctic Ocean and Its Relation to Phytoplankton Biomass |
title_fullStr |
Atmospheric DMS in the Arctic Ocean and Its Relation to Phytoplankton Biomass |
title_full_unstemmed |
Atmospheric DMS in the Arctic Ocean and Its Relation to Phytoplankton Biomass |
title_sort |
atmospheric dms in the arctic ocean and its relation to phytoplankton biomass |
publisher |
AMER GEOPHYSICAL UNION |
publishDate |
2018 |
url |
https://oasis.postech.ac.kr/handle/2014.oak/96047 https://doi.org/10.1002/2017GB005805 |
geographic |
Arctic Arctic Ocean Barents Sea Greenland Svalbard |
geographic_facet |
Arctic Arctic Ocean Barents Sea Greenland Svalbard |
genre |
Arctic Arctic Ocean Barents Sea Greenland Greenland Sea Phytoplankton Svalbard |
genre_facet |
Arctic Arctic Ocean Barents Sea Greenland Greenland Sea Phytoplankton Svalbard |
op_relation |
GLOBAL BIOGEOCHEMICAL CYCLES Environmental Sciences Geosciences, Multidisciplinary Meteorology & Atmospheric Sciences Environmental Sciences & Ecology Geology 0886-6236 https://oasis.postech.ac.kr/handle/2014.oak/96047 doi:10.1002/2017GB005805 31292 GLOBAL BIOGEOCHEMICAL CYCLES, v.32, no.3, pp.351 - 359 000430105900002 2-s2.0-85043319191 |
op_doi |
https://doi.org/10.1002/2017GB005805 |
container_title |
Global Biogeochemical Cycles |
container_volume |
32 |
container_issue |
3 |
container_start_page |
351 |
op_container_end_page |
359 |
_version_ |
1766320650671095808 |