Projection of North Atlantic Oscillation and its effect on tracer transport

The North Atlantic Oscillation (NAO) plays an important role in the climate variability of the Northern Hemisphere, with significant consequences on long-range pollutant transport. We investigate the evolution of pollutant transport in the 21st century influenced by the NAO under a global climate ch...

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Published in:Atmospheric Chemistry and Physics
Main Authors: S. Bacer, T. Christoudias, A. Pozzer
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2016
Subjects:
Online Access:https://doi.org/10.5194/acp-16-15581-2016
https://doaj.org/article/6692a755b9c044859f04c558de2d36ce
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spelling ftdoajarticles:oai:doaj.org/article:6692a755b9c044859f04c558de2d36ce 2023-05-15T17:30:54+02:00 Projection of North Atlantic Oscillation and its effect on tracer transport S. Bacer T. Christoudias A. Pozzer 2016-12-01T00:00:00Z https://doi.org/10.5194/acp-16-15581-2016 https://doaj.org/article/6692a755b9c044859f04c558de2d36ce EN eng Copernicus Publications https://www.atmos-chem-phys.net/16/15581/2016/acp-16-15581-2016.pdf https://doaj.org/toc/1680-7316 https://doaj.org/toc/1680-7324 doi:10.5194/acp-16-15581-2016 1680-7316 1680-7324 https://doaj.org/article/6692a755b9c044859f04c558de2d36ce Atmospheric Chemistry and Physics, Vol 16, Pp 15581-15592 (2016) Physics QC1-999 Chemistry QD1-999 article 2016 ftdoajarticles https://doi.org/10.5194/acp-16-15581-2016 2022-12-30T23:13:03Z The North Atlantic Oscillation (NAO) plays an important role in the climate variability of the Northern Hemisphere, with significant consequences on long-range pollutant transport. We investigate the evolution of pollutant transport in the 21st century influenced by the NAO under a global climate change scenario. We use a free-running simulation performed by the ECHAM/MESSy Atmospheric Chemistry (EMAC) model coupled with the ocean general circulation model MPIOM, covering the period from 1950 until 2100. Similarly to other works, the model shows a future northeastward shift of the NAO centres of action and a weak positive trend of the NAO index (over 150 years). Moreover, we find that NAO trends (computed over periods shorter than 30 years) will continue to oscillate between positive and negative values in the future. To investigate the NAO effects on transport we consider carbon monoxide tracers with exponential decay and constant interannual emissions. We find that at the end of the century, the south-western Mediterranean and northern Africa will, during positive NAO phases, see higher pollutant concentrations with respect to the past, while a wider part of northern Europe will, during positive NAO phases, see lower pollutant concentrations. Such results are confirmed by the changes observed in the future for tracer concentration and vertically integrated tracer transport, differentiating the cases of “high NAO” and “low NAO” events. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles Atmospheric Chemistry and Physics 16 24 15581 15592
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Physics
QC1-999
Chemistry
QD1-999
spellingShingle Physics
QC1-999
Chemistry
QD1-999
S. Bacer
T. Christoudias
A. Pozzer
Projection of North Atlantic Oscillation and its effect on tracer transport
topic_facet Physics
QC1-999
Chemistry
QD1-999
description The North Atlantic Oscillation (NAO) plays an important role in the climate variability of the Northern Hemisphere, with significant consequences on long-range pollutant transport. We investigate the evolution of pollutant transport in the 21st century influenced by the NAO under a global climate change scenario. We use a free-running simulation performed by the ECHAM/MESSy Atmospheric Chemistry (EMAC) model coupled with the ocean general circulation model MPIOM, covering the period from 1950 until 2100. Similarly to other works, the model shows a future northeastward shift of the NAO centres of action and a weak positive trend of the NAO index (over 150 years). Moreover, we find that NAO trends (computed over periods shorter than 30 years) will continue to oscillate between positive and negative values in the future. To investigate the NAO effects on transport we consider carbon monoxide tracers with exponential decay and constant interannual emissions. We find that at the end of the century, the south-western Mediterranean and northern Africa will, during positive NAO phases, see higher pollutant concentrations with respect to the past, while a wider part of northern Europe will, during positive NAO phases, see lower pollutant concentrations. Such results are confirmed by the changes observed in the future for tracer concentration and vertically integrated tracer transport, differentiating the cases of “high NAO” and “low NAO” events.
format Article in Journal/Newspaper
author S. Bacer
T. Christoudias
A. Pozzer
author_facet S. Bacer
T. Christoudias
A. Pozzer
author_sort S. Bacer
title Projection of North Atlantic Oscillation and its effect on tracer transport
title_short Projection of North Atlantic Oscillation and its effect on tracer transport
title_full Projection of North Atlantic Oscillation and its effect on tracer transport
title_fullStr Projection of North Atlantic Oscillation and its effect on tracer transport
title_full_unstemmed Projection of North Atlantic Oscillation and its effect on tracer transport
title_sort projection of north atlantic oscillation and its effect on tracer transport
publisher Copernicus Publications
publishDate 2016
url https://doi.org/10.5194/acp-16-15581-2016
https://doaj.org/article/6692a755b9c044859f04c558de2d36ce
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Atmospheric Chemistry and Physics, Vol 16, Pp 15581-15592 (2016)
op_relation https://www.atmos-chem-phys.net/16/15581/2016/acp-16-15581-2016.pdf
https://doaj.org/toc/1680-7316
https://doaj.org/toc/1680-7324
doi:10.5194/acp-16-15581-2016
1680-7316
1680-7324
https://doaj.org/article/6692a755b9c044859f04c558de2d36ce
op_doi https://doi.org/10.5194/acp-16-15581-2016
container_title Atmospheric Chemistry and Physics
container_volume 16
container_issue 24
container_start_page 15581
op_container_end_page 15592
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