NAO and extreme ocean states in the Northeast Atlantic Ocean
Large scale atmospheric oscillations are known to have an influence on waves in the North Atlantic. In quantifying how the wave and wind climate of this region may change towards the end of the century due to climate change, it is useful to investigate the influence of large scale oscillations using...
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ftcopernicus:oai:publications.copernicus.org:asr56241 2023-05-15T17:30:10+02:00 NAO and extreme ocean states in the Northeast Atlantic Ocean Gleeson, Emily Gallagher, Sarah Clancy, Colm Dias, Frédéric 2018-01-15 application/pdf https://doi.org/10.5194/asr-14-23-2017 https://asr.copernicus.org/articles/14/23/2017/ eng eng doi:10.5194/asr-14-23-2017 https://asr.copernicus.org/articles/14/23/2017/ eISSN: 1992-0636 Text 2018 ftcopernicus https://doi.org/10.5194/asr-14-23-2017 2020-07-20T16:23:50Z Large scale atmospheric oscillations are known to have an influence on waves in the North Atlantic. In quantifying how the wave and wind climate of this region may change towards the end of the century due to climate change, it is useful to investigate the influence of large scale oscillations using indices such as the North Atlantic Oscillation (NAO: fluctuations in the difference between the Icelandic low pressure system and the Azore high pressure system). In this study a statistical analysis of the station-based NAO index was carried out using an ensemble of EC-Earth global climate simulations, where EC-Earth is a European-developed atmosphere ocean sea-ice coupled climate model. The NAO index was compared to observations and to projected changes in the index by the end of the century under the RCP4.5 and RCP8.5 forcing scenarios. In addition, an ensemble of EC-Earth driven WAVEWATCH III wave model projections over the North Atlantic was analysed to determine the correlations between the NAO and significant wave height ( H s ) and the NAO and extreme ocean states. For the most part, no statistically significant differences were found between the distributions of observed and modelled station-based NAO or in projected distributions of the NAO. Means and extremes of H s are projected to decrease on average by the end of this century. The 95th percentile of H s is strongly positively correlated to the NAO. Projections of H s extremes are location dependent and in fact, under the influence of positive NAO the 20-year return levels of H s were found to be amplified in some regions. However, it is important to note that the projected decreases in the 95th percentile of H s off the west coast of Ireland are not statistically significant in one of the RCP4.5 and one of the RCP8.5 simulations (me41, me83) which indicates that there is still uncertainty in the projections of higher percentiles. Text North Atlantic North Atlantic oscillation Northeast Atlantic Sea ice Copernicus Publications: E-Journals Advances in Science and Research 14 23 33 |
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Copernicus Publications: E-Journals |
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ftcopernicus |
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English |
description |
Large scale atmospheric oscillations are known to have an influence on waves in the North Atlantic. In quantifying how the wave and wind climate of this region may change towards the end of the century due to climate change, it is useful to investigate the influence of large scale oscillations using indices such as the North Atlantic Oscillation (NAO: fluctuations in the difference between the Icelandic low pressure system and the Azore high pressure system). In this study a statistical analysis of the station-based NAO index was carried out using an ensemble of EC-Earth global climate simulations, where EC-Earth is a European-developed atmosphere ocean sea-ice coupled climate model. The NAO index was compared to observations and to projected changes in the index by the end of the century under the RCP4.5 and RCP8.5 forcing scenarios. In addition, an ensemble of EC-Earth driven WAVEWATCH III wave model projections over the North Atlantic was analysed to determine the correlations between the NAO and significant wave height ( H s ) and the NAO and extreme ocean states. For the most part, no statistically significant differences were found between the distributions of observed and modelled station-based NAO or in projected distributions of the NAO. Means and extremes of H s are projected to decrease on average by the end of this century. The 95th percentile of H s is strongly positively correlated to the NAO. Projections of H s extremes are location dependent and in fact, under the influence of positive NAO the 20-year return levels of H s were found to be amplified in some regions. However, it is important to note that the projected decreases in the 95th percentile of H s off the west coast of Ireland are not statistically significant in one of the RCP4.5 and one of the RCP8.5 simulations (me41, me83) which indicates that there is still uncertainty in the projections of higher percentiles. |
format |
Text |
author |
Gleeson, Emily Gallagher, Sarah Clancy, Colm Dias, Frédéric |
spellingShingle |
Gleeson, Emily Gallagher, Sarah Clancy, Colm Dias, Frédéric NAO and extreme ocean states in the Northeast Atlantic Ocean |
author_facet |
Gleeson, Emily Gallagher, Sarah Clancy, Colm Dias, Frédéric |
author_sort |
Gleeson, Emily |
title |
NAO and extreme ocean states in the Northeast Atlantic Ocean |
title_short |
NAO and extreme ocean states in the Northeast Atlantic Ocean |
title_full |
NAO and extreme ocean states in the Northeast Atlantic Ocean |
title_fullStr |
NAO and extreme ocean states in the Northeast Atlantic Ocean |
title_full_unstemmed |
NAO and extreme ocean states in the Northeast Atlantic Ocean |
title_sort |
nao and extreme ocean states in the northeast atlantic ocean |
publishDate |
2018 |
url |
https://doi.org/10.5194/asr-14-23-2017 https://asr.copernicus.org/articles/14/23/2017/ |
genre |
North Atlantic North Atlantic oscillation Northeast Atlantic Sea ice |
genre_facet |
North Atlantic North Atlantic oscillation Northeast Atlantic Sea ice |
op_source |
eISSN: 1992-0636 |
op_relation |
doi:10.5194/asr-14-23-2017 https://asr.copernicus.org/articles/14/23/2017/ |
op_doi |
https://doi.org/10.5194/asr-14-23-2017 |
container_title |
Advances in Science and Research |
container_volume |
14 |
container_start_page |
23 |
op_container_end_page |
33 |
_version_ |
1766125989757190144 |