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: Bacer, Sara, Christoudias, Theodoros, Pozzer, Andrea
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/acp-16-15581-2016
https://www.atmos-chem-phys.net/16/15581/2016/
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spelling ftcopernicus:oai:publications.copernicus.org:acp51323 2023-05-15T17:30:51+02:00 Projection of North Atlantic Oscillation and its effect on tracer transport Bacer, Sara Christoudias, Theodoros Pozzer, Andrea 2018-09-09 application/pdf https://doi.org/10.5194/acp-16-15581-2016 https://www.atmos-chem-phys.net/16/15581/2016/ eng eng doi:10.5194/acp-16-15581-2016 https://www.atmos-chem-phys.net/16/15581/2016/ eISSN: 1680-7324 Text 2018 ftcopernicus https://doi.org/10.5194/acp-16-15581-2016 2019-12-24T09:51:46Z 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. Text North Atlantic North Atlantic oscillation Copernicus Publications: E-Journals Atmospheric Chemistry and Physics 16 24 15581 15592
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
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 Text
author Bacer, Sara
Christoudias, Theodoros
Pozzer, Andrea
spellingShingle Bacer, Sara
Christoudias, Theodoros
Pozzer, Andrea
Projection of North Atlantic Oscillation and its effect on tracer transport
author_facet Bacer, Sara
Christoudias, Theodoros
Pozzer, Andrea
author_sort Bacer, Sara
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
publishDate 2018
url https://doi.org/10.5194/acp-16-15581-2016
https://www.atmos-chem-phys.net/16/15581/2016/
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source eISSN: 1680-7324
op_relation doi:10.5194/acp-16-15581-2016
https://www.atmos-chem-phys.net/16/15581/2016/
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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