Biogenic Aerosol in the Arctic from Eight Years of MSA Data from Ny Ålesund (Svalbard Islands) and Thule (Greenland)

In remote marine areas, biogenic productivity and atmospheric particulate are coupled through dimethylsulfide (DMS) emission by phytoplankton. Once in the atmosphere, the gaseous DMS is oxidized to produce H2SO4 and methanesulfonic acid (MSA); both species can affect the formation of cloud condensat...

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Published in:Atmosphere
Main Authors: Silvia Becagli, Alessandra Amore, Laura Caiazzo, Tatiana Di Iorio, Alcide di Sarra, Luigi Lazzara, Christian Marchese, Daniela Meloni, Giovanna Mori, Giovanni Muscari, Caterina Nuccio, Giandomenico Pace, Mirko Severi, Rita Traversi
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2019
Subjects:
MSA
NAO
Online Access:https://doi.org/10.3390/atmos10070349
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spelling ftmdpi:oai:mdpi.com:/2073-4433/10/7/349/ 2023-08-20T04:04:06+02:00 Biogenic Aerosol in the Arctic from Eight Years of MSA Data from Ny Ålesund (Svalbard Islands) and Thule (Greenland) Silvia Becagli Alessandra Amore Laura Caiazzo Tatiana Di Iorio Alcide di Sarra Luigi Lazzara Christian Marchese Daniela Meloni Giovanna Mori Giovanni Muscari Caterina Nuccio Giandomenico Pace Mirko Severi Rita Traversi agris 2019-06-26 application/pdf https://doi.org/10.3390/atmos10070349 EN eng Multidisciplinary Digital Publishing Institute Biosphere/Hydrosphere/Land–Atmosphere Interactions https://dx.doi.org/10.3390/atmos10070349 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 10; Issue 7; Pages: 349 biogenic aerosol Arctic MSA sea ice extent marginal ice zone NAO Text 2019 ftmdpi https://doi.org/10.3390/atmos10070349 2023-07-31T22:23:12Z In remote marine areas, biogenic productivity and atmospheric particulate are coupled through dimethylsulfide (DMS) emission by phytoplankton. Once in the atmosphere, the gaseous DMS is oxidized to produce H2SO4 and methanesulfonic acid (MSA); both species can affect the formation of cloud condensation nuclei. This study analyses eight years of biogenic aerosol evolution and variability at two Arctic sites: Thule (76.5° N, 68.8° W) and Ny Ålesund (78.9° N, 11.9° E). Sea ice plays a key role in determining the MSA concentration in polar regions. At the beginning of the melting season, in April, up to June, the biogenic aerosol concentration appears inversely correlated with sea ice extent and area, and positively correlated with the extent of the ice-free area in the marginal ice zone (IF-MIZ). The upper ocean stratification induced by sea ice melting might have a role in these correlations, since the springtime formation of this surface layer regulates the accumulation of phytoplankton and nutrients, allowing the DMS to escape from the sea to the atmosphere. The multiyear analysis reveals a progressive decrease in MSA concentration in May at Thule and an increase in July August at Ny Ålesund. Therefore, while the MSA seasonal evolution is mainly related with the sea ice retreat in April, May, and June, the IF-MIZ extent appears as the main factor affecting the longer-term behavior of MSA. Text Arctic Greenland Ny Ålesund Ny-Ålesund Phytoplankton Sea ice Svalbard Thule MDPI Open Access Publishing Arctic Greenland Ny-Ålesund Svalbard Atmosphere 10 7 349
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic biogenic aerosol
Arctic
MSA
sea ice extent
marginal ice zone
NAO
spellingShingle biogenic aerosol
Arctic
MSA
sea ice extent
marginal ice zone
NAO
Silvia Becagli
Alessandra Amore
Laura Caiazzo
Tatiana Di Iorio
Alcide di Sarra
Luigi Lazzara
Christian Marchese
Daniela Meloni
Giovanna Mori
Giovanni Muscari
Caterina Nuccio
Giandomenico Pace
Mirko Severi
Rita Traversi
Biogenic Aerosol in the Arctic from Eight Years of MSA Data from Ny Ålesund (Svalbard Islands) and Thule (Greenland)
topic_facet biogenic aerosol
Arctic
MSA
sea ice extent
marginal ice zone
NAO
description In remote marine areas, biogenic productivity and atmospheric particulate are coupled through dimethylsulfide (DMS) emission by phytoplankton. Once in the atmosphere, the gaseous DMS is oxidized to produce H2SO4 and methanesulfonic acid (MSA); both species can affect the formation of cloud condensation nuclei. This study analyses eight years of biogenic aerosol evolution and variability at two Arctic sites: Thule (76.5° N, 68.8° W) and Ny Ålesund (78.9° N, 11.9° E). Sea ice plays a key role in determining the MSA concentration in polar regions. At the beginning of the melting season, in April, up to June, the biogenic aerosol concentration appears inversely correlated with sea ice extent and area, and positively correlated with the extent of the ice-free area in the marginal ice zone (IF-MIZ). The upper ocean stratification induced by sea ice melting might have a role in these correlations, since the springtime formation of this surface layer regulates the accumulation of phytoplankton and nutrients, allowing the DMS to escape from the sea to the atmosphere. The multiyear analysis reveals a progressive decrease in MSA concentration in May at Thule and an increase in July August at Ny Ålesund. Therefore, while the MSA seasonal evolution is mainly related with the sea ice retreat in April, May, and June, the IF-MIZ extent appears as the main factor affecting the longer-term behavior of MSA.
format Text
author Silvia Becagli
Alessandra Amore
Laura Caiazzo
Tatiana Di Iorio
Alcide di Sarra
Luigi Lazzara
Christian Marchese
Daniela Meloni
Giovanna Mori
Giovanni Muscari
Caterina Nuccio
Giandomenico Pace
Mirko Severi
Rita Traversi
author_facet Silvia Becagli
Alessandra Amore
Laura Caiazzo
Tatiana Di Iorio
Alcide di Sarra
Luigi Lazzara
Christian Marchese
Daniela Meloni
Giovanna Mori
Giovanni Muscari
Caterina Nuccio
Giandomenico Pace
Mirko Severi
Rita Traversi
author_sort Silvia Becagli
title Biogenic Aerosol in the Arctic from Eight Years of MSA Data from Ny Ålesund (Svalbard Islands) and Thule (Greenland)
title_short Biogenic Aerosol in the Arctic from Eight Years of MSA Data from Ny Ålesund (Svalbard Islands) and Thule (Greenland)
title_full Biogenic Aerosol in the Arctic from Eight Years of MSA Data from Ny Ålesund (Svalbard Islands) and Thule (Greenland)
title_fullStr Biogenic Aerosol in the Arctic from Eight Years of MSA Data from Ny Ålesund (Svalbard Islands) and Thule (Greenland)
title_full_unstemmed Biogenic Aerosol in the Arctic from Eight Years of MSA Data from Ny Ålesund (Svalbard Islands) and Thule (Greenland)
title_sort biogenic aerosol in the arctic from eight years of msa data from ny ålesund (svalbard islands) and thule (greenland)
publisher Multidisciplinary Digital Publishing Institute
publishDate 2019
url https://doi.org/10.3390/atmos10070349
op_coverage agris
geographic Arctic
Greenland
Ny-Ålesund
Svalbard
geographic_facet Arctic
Greenland
Ny-Ålesund
Svalbard
genre Arctic
Greenland
Ny Ålesund
Ny-Ålesund
Phytoplankton
Sea ice
Svalbard
Thule
genre_facet Arctic
Greenland
Ny Ålesund
Ny-Ålesund
Phytoplankton
Sea ice
Svalbard
Thule
op_source Atmosphere; Volume 10; Issue 7; Pages: 349
op_relation Biosphere/Hydrosphere/Land–Atmosphere Interactions
https://dx.doi.org/10.3390/atmos10070349
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos10070349
container_title Atmosphere
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