Trans-polar drift-pathways of riverine European microplastic

High concentrations of microplastic particles are reported across the Arctic Ocean–yet no meaningful point sources, suspension timelines, or accumulation areas have been identified. Here we use Lagrangian particle advection simulations to model the transport of buoyant microplastic from northern Eur...

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Published in:Scientific Reports
Main Authors: Huserbråten, Mats Brockstedt Olsen, Hattermann, Tore, Broms, Cecilie, Albretsen, Jon
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://hdl.handle.net/11250/2999732
https://doi.org/10.1038/s41598-022-07080-z
id ftimr:oai:imr.brage.unit.no:11250/2999732
record_format openpolar
spelling ftimr:oai:imr.brage.unit.no:11250/2999732 2023-05-15T14:34:35+02:00 Trans-polar drift-pathways of riverine European microplastic Huserbråten, Mats Brockstedt Olsen Hattermann, Tore Broms, Cecilie Albretsen, Jon 2022 application/pdf https://hdl.handle.net/11250/2999732 https://doi.org/10.1038/s41598-022-07080-z eng eng Norges forskningsråd: 280727 Scientific Reports. 2022, 12 . urn:issn:2045-2322 https://hdl.handle.net/11250/2999732 https://doi.org/10.1038/s41598-022-07080-z cristin:2017196 10 12 Scientific Reports Økosystem Ecosystem Havmodeller Ocean modelling Mikroplast Microplastic Forurensing Pollution Arktis Arctic Peer reviewed Journal article 2022 ftimr https://doi.org/10.1038/s41598-022-07080-z 2022-06-22T22:40:31Z High concentrations of microplastic particles are reported across the Arctic Ocean–yet no meaningful point sources, suspension timelines, or accumulation areas have been identified. Here we use Lagrangian particle advection simulations to model the transport of buoyant microplastic from northern European rivers to the high Arctic, and compare model results to the flux of sampled synthetic particles across the main entrance to the Arctic Ocean. We report widespread dispersal along the Eurasian continental shelf, across the North Pole, and back into the Nordic Seas; with accumulation zones over the Nansen basin, the Laptev Sea, and the ocean gyres of the Nordic Seas. The equal distribution of sampled synthetic particles across water masses covering a wide time frame of anthropogenic influence suggests a system in full saturation rather than pronounced injection from European sources, through a complex circulation scheme connecting the entire Arctic Mediterranean. This circulation of microplastic through Arctic ecosystems may have large consequences to natural ecosystem health, highlighting an ever-increasing need for better waste management. publishedVersion Article in Journal/Newspaper Arctic Arctic Ocean Arktis Arktis* laptev Laptev Sea Nansen Basin Nordic Seas North Pole Institute for Marine Research: Brage IMR Arctic Arctic Ocean Laptev Sea North Pole Scientific Reports 12 1
institution Open Polar
collection Institute for Marine Research: Brage IMR
op_collection_id ftimr
language English
topic Økosystem
Ecosystem
Havmodeller
Ocean modelling
Mikroplast
Microplastic
Forurensing
Pollution
Arktis
Arctic
spellingShingle Økosystem
Ecosystem
Havmodeller
Ocean modelling
Mikroplast
Microplastic
Forurensing
Pollution
Arktis
Arctic
Huserbråten, Mats Brockstedt Olsen
Hattermann, Tore
Broms, Cecilie
Albretsen, Jon
Trans-polar drift-pathways of riverine European microplastic
topic_facet Økosystem
Ecosystem
Havmodeller
Ocean modelling
Mikroplast
Microplastic
Forurensing
Pollution
Arktis
Arctic
description High concentrations of microplastic particles are reported across the Arctic Ocean–yet no meaningful point sources, suspension timelines, or accumulation areas have been identified. Here we use Lagrangian particle advection simulations to model the transport of buoyant microplastic from northern European rivers to the high Arctic, and compare model results to the flux of sampled synthetic particles across the main entrance to the Arctic Ocean. We report widespread dispersal along the Eurasian continental shelf, across the North Pole, and back into the Nordic Seas; with accumulation zones over the Nansen basin, the Laptev Sea, and the ocean gyres of the Nordic Seas. The equal distribution of sampled synthetic particles across water masses covering a wide time frame of anthropogenic influence suggests a system in full saturation rather than pronounced injection from European sources, through a complex circulation scheme connecting the entire Arctic Mediterranean. This circulation of microplastic through Arctic ecosystems may have large consequences to natural ecosystem health, highlighting an ever-increasing need for better waste management. publishedVersion
format Article in Journal/Newspaper
author Huserbråten, Mats Brockstedt Olsen
Hattermann, Tore
Broms, Cecilie
Albretsen, Jon
author_facet Huserbråten, Mats Brockstedt Olsen
Hattermann, Tore
Broms, Cecilie
Albretsen, Jon
author_sort Huserbråten, Mats Brockstedt Olsen
title Trans-polar drift-pathways of riverine European microplastic
title_short Trans-polar drift-pathways of riverine European microplastic
title_full Trans-polar drift-pathways of riverine European microplastic
title_fullStr Trans-polar drift-pathways of riverine European microplastic
title_full_unstemmed Trans-polar drift-pathways of riverine European microplastic
title_sort trans-polar drift-pathways of riverine european microplastic
publishDate 2022
url https://hdl.handle.net/11250/2999732
https://doi.org/10.1038/s41598-022-07080-z
geographic Arctic
Arctic Ocean
Laptev Sea
North Pole
geographic_facet Arctic
Arctic Ocean
Laptev Sea
North Pole
genre Arctic
Arctic Ocean
Arktis
Arktis*
laptev
Laptev Sea
Nansen Basin
Nordic Seas
North Pole
genre_facet Arctic
Arctic Ocean
Arktis
Arktis*
laptev
Laptev Sea
Nansen Basin
Nordic Seas
North Pole
op_source 10
12
Scientific Reports
op_relation Norges forskningsråd: 280727
Scientific Reports. 2022, 12 .
urn:issn:2045-2322
https://hdl.handle.net/11250/2999732
https://doi.org/10.1038/s41598-022-07080-z
cristin:2017196
op_doi https://doi.org/10.1038/s41598-022-07080-z
container_title Scientific Reports
container_volume 12
container_issue 1
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