First High-Frequency Underway Observation of DMS Distribution in the Southern Ocean during Austral Autumn

We investigate the distribution of dimethyl sulfide (DMS) in the Southern Ocean’s (50° W to 170° W) surface water, including the Antarctic Peninsula and the marginal sea ice zone (MIZ) in the Ross and Amundsen Seas. This is the first high-frequency observation conducted in the austral autumn (in Apr...

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Published in:Atmosphere
Main Authors: Intae Kim, Miming Zhang, Kitae Kim, Keyhong Park
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12010122
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spelling ftmdpi:oai:mdpi.com:/2073-4433/12/1/122/ 2023-08-20T03:59:36+02:00 First High-Frequency Underway Observation of DMS Distribution in the Southern Ocean during Austral Autumn Intae Kim Miming Zhang Kitae Kim Keyhong Park agris 2021-01-16 application/pdf https://doi.org/10.3390/atmos12010122 EN eng Multidisciplinary Digital Publishing Institute Aerosols https://dx.doi.org/10.3390/atmos12010122 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 12; Issue 1; Pages: 122 dimethyl sulfide Southern Ocean austral autumn climate high-frequency underway observation Text 2021 ftmdpi https://doi.org/10.3390/atmos12010122 2023-08-01T00:52:49Z We investigate the distribution of dimethyl sulfide (DMS) in the Southern Ocean’s (50° W to 170° W) surface water, including the Antarctic Peninsula and the marginal sea ice zone (MIZ) in the Ross and Amundsen Seas. This is the first high-frequency observation conducted in the austral autumn (in April) in the Southern Ocean. The mean DMS concentration was 2.7 ± 2.5 nM (1 σ) for the entire study area. Noticeably enhanced DMS (5 to 28 nM) concentrations were observed in the MIZ around the Ross and Amundsen Seas and the coastal regions in the Antarctic Peninsula; this could be attributed to biological production of local ice algae, which appears to be supplied with nutrients from glacial or sea ice melt water. These observed DMS inventories were significantly higher (an order of magnitude) than current climatological DMS inventories. The local DMS sources being transported outward from the polynyas, where strong bloom occurs during summer, could result in larger discrepancies between observed DMS and climatological DMS in the MIZ area (in the Amundsen Sea). Overall, this study is the first to highlight the significance of the underestimation of current DMS fluxes in the austral autumn, which consequently results in significant errors in the climate models. Text Amundsen Sea Antarc* Antarctic Antarctic Peninsula ice algae Sea ice Southern Ocean MDPI Open Access Publishing Amundsen Sea Antarctic Antarctic Peninsula Austral Southern Ocean The Antarctic Atmosphere 12 1 122
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic dimethyl sulfide
Southern Ocean
austral autumn
climate
high-frequency underway observation
spellingShingle dimethyl sulfide
Southern Ocean
austral autumn
climate
high-frequency underway observation
Intae Kim
Miming Zhang
Kitae Kim
Keyhong Park
First High-Frequency Underway Observation of DMS Distribution in the Southern Ocean during Austral Autumn
topic_facet dimethyl sulfide
Southern Ocean
austral autumn
climate
high-frequency underway observation
description We investigate the distribution of dimethyl sulfide (DMS) in the Southern Ocean’s (50° W to 170° W) surface water, including the Antarctic Peninsula and the marginal sea ice zone (MIZ) in the Ross and Amundsen Seas. This is the first high-frequency observation conducted in the austral autumn (in April) in the Southern Ocean. The mean DMS concentration was 2.7 ± 2.5 nM (1 σ) for the entire study area. Noticeably enhanced DMS (5 to 28 nM) concentrations were observed in the MIZ around the Ross and Amundsen Seas and the coastal regions in the Antarctic Peninsula; this could be attributed to biological production of local ice algae, which appears to be supplied with nutrients from glacial or sea ice melt water. These observed DMS inventories were significantly higher (an order of magnitude) than current climatological DMS inventories. The local DMS sources being transported outward from the polynyas, where strong bloom occurs during summer, could result in larger discrepancies between observed DMS and climatological DMS in the MIZ area (in the Amundsen Sea). Overall, this study is the first to highlight the significance of the underestimation of current DMS fluxes in the austral autumn, which consequently results in significant errors in the climate models.
format Text
author Intae Kim
Miming Zhang
Kitae Kim
Keyhong Park
author_facet Intae Kim
Miming Zhang
Kitae Kim
Keyhong Park
author_sort Intae Kim
title First High-Frequency Underway Observation of DMS Distribution in the Southern Ocean during Austral Autumn
title_short First High-Frequency Underway Observation of DMS Distribution in the Southern Ocean during Austral Autumn
title_full First High-Frequency Underway Observation of DMS Distribution in the Southern Ocean during Austral Autumn
title_fullStr First High-Frequency Underway Observation of DMS Distribution in the Southern Ocean during Austral Autumn
title_full_unstemmed First High-Frequency Underway Observation of DMS Distribution in the Southern Ocean during Austral Autumn
title_sort first high-frequency underway observation of dms distribution in the southern ocean during austral autumn
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/atmos12010122
op_coverage agris
geographic Amundsen Sea
Antarctic
Antarctic Peninsula
Austral
Southern Ocean
The Antarctic
geographic_facet Amundsen Sea
Antarctic
Antarctic Peninsula
Austral
Southern Ocean
The Antarctic
genre Amundsen Sea
Antarc*
Antarctic
Antarctic Peninsula
ice algae
Sea ice
Southern Ocean
genre_facet Amundsen Sea
Antarc*
Antarctic
Antarctic Peninsula
ice algae
Sea ice
Southern Ocean
op_source Atmosphere; Volume 12; Issue 1; Pages: 122
op_relation Aerosols
https://dx.doi.org/10.3390/atmos12010122
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos12010122
container_title Atmosphere
container_volume 12
container_issue 1
container_start_page 122
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