Temporal variability in winter wave conditions and storminess in the northwest of Ireland

Winter storms have significant morphological impacts in coastal areas, often leading to extensive infrastructure damage and socio-economic disruption. While storm-dominated coastal environments, such as the northwest coast of Ireland, are generally attuned to highly energetic wave conditions, morpho...

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Bibliographic Details
Main Authors: Loureiro, Carlos, Cooper, Andrew
Format: Article in Journal/Newspaper
Language:English
Published: 2018
Subjects:
Online Access:https://zenodo.org/record/2591445
https://doi.org/10.2014/igj.v51i2.1369
id ftzenodo:oai:zenodo.org:2591445
record_format openpolar
spelling ftzenodo:oai:zenodo.org:2591445 2023-05-15T17:34:38+02:00 Temporal variability in winter wave conditions and storminess in the northwest of Ireland Loureiro, Carlos Cooper, Andrew 2018-11-19 https://zenodo.org/record/2591445 https://doi.org/10.2014/igj.v51i2.1369 eng eng info:eu-repo/grantAgreement/EC/H2020/661342/ https://zenodo.org/record/2591445 https://doi.org/10.2014/igj.v51i2.1369 oai:zenodo.org:2591445 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode Irish Geography 51(2) 155-170 Northeast Atlantic Seasonality Winter storms Storm-groups Coastal impacts info:eu-repo/semantics/article publication-article 2018 ftzenodo https://doi.org/10.2014/igj.v51i2.1369 2023-03-11T00:28:31Z Winter storms have significant morphological impacts in coastal areas, often leading to extensive infrastructure damage and socio-economic disruption. While storm-dominated coastal environments, such as the northwest coast of Ireland, are generally attuned to highly energetic wave conditions, morphological impacts can be intensified by changes in the frequency and sequencing of storm events, particularly during storm-groups or exceptional winter seasons. Aiming to assess the variability in frequency and sequencing of wintertime wave conditions and storms in the northwest of Ireland, we combine observational records (M4 buoy) with data from two independent wave reanalyses (ERA-Interim and WAVEWATCH III) and perform a statistical analysis of wave conditions over the past six decades. Both reanalyses represent observed wave heights with very good skill. Excellent agreement between modelled data and observations was identified up to the 99th percentile, despite a slight underestimation/ overestimation by ERA-Interim/WAVEWATCH III for waves above the 90% exceedance level. The winter of 2014/15 was the most energetic on record (67 years), but not the stormiest. The results show that highly energetic and stormy winters occur in clusters during positive phases of the North Atlantic Oscillation. Significant positive temporal trends for winter wave height, number of storms per winter and average winter storm wave height, suggest that winters are becoming more energetic and stormier, with potential implications for the erosion and recovery of coastal systems in the northwest of Ireland. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Northeast Atlantic Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic Northeast Atlantic
Seasonality
Winter storms
Storm-groups
Coastal impacts
spellingShingle Northeast Atlantic
Seasonality
Winter storms
Storm-groups
Coastal impacts
Loureiro, Carlos
Cooper, Andrew
Temporal variability in winter wave conditions and storminess in the northwest of Ireland
topic_facet Northeast Atlantic
Seasonality
Winter storms
Storm-groups
Coastal impacts
description Winter storms have significant morphological impacts in coastal areas, often leading to extensive infrastructure damage and socio-economic disruption. While storm-dominated coastal environments, such as the northwest coast of Ireland, are generally attuned to highly energetic wave conditions, morphological impacts can be intensified by changes in the frequency and sequencing of storm events, particularly during storm-groups or exceptional winter seasons. Aiming to assess the variability in frequency and sequencing of wintertime wave conditions and storms in the northwest of Ireland, we combine observational records (M4 buoy) with data from two independent wave reanalyses (ERA-Interim and WAVEWATCH III) and perform a statistical analysis of wave conditions over the past six decades. Both reanalyses represent observed wave heights with very good skill. Excellent agreement between modelled data and observations was identified up to the 99th percentile, despite a slight underestimation/ overestimation by ERA-Interim/WAVEWATCH III for waves above the 90% exceedance level. The winter of 2014/15 was the most energetic on record (67 years), but not the stormiest. The results show that highly energetic and stormy winters occur in clusters during positive phases of the North Atlantic Oscillation. Significant positive temporal trends for winter wave height, number of storms per winter and average winter storm wave height, suggest that winters are becoming more energetic and stormier, with potential implications for the erosion and recovery of coastal systems in the northwest of Ireland.
format Article in Journal/Newspaper
author Loureiro, Carlos
Cooper, Andrew
author_facet Loureiro, Carlos
Cooper, Andrew
author_sort Loureiro, Carlos
title Temporal variability in winter wave conditions and storminess in the northwest of Ireland
title_short Temporal variability in winter wave conditions and storminess in the northwest of Ireland
title_full Temporal variability in winter wave conditions and storminess in the northwest of Ireland
title_fullStr Temporal variability in winter wave conditions and storminess in the northwest of Ireland
title_full_unstemmed Temporal variability in winter wave conditions and storminess in the northwest of Ireland
title_sort temporal variability in winter wave conditions and storminess in the northwest of ireland
publishDate 2018
url https://zenodo.org/record/2591445
https://doi.org/10.2014/igj.v51i2.1369
genre North Atlantic
North Atlantic oscillation
Northeast Atlantic
genre_facet North Atlantic
North Atlantic oscillation
Northeast Atlantic
op_source Irish Geography 51(2) 155-170
op_relation info:eu-repo/grantAgreement/EC/H2020/661342/
https://zenodo.org/record/2591445
https://doi.org/10.2014/igj.v51i2.1369
oai:zenodo.org:2591445
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.2014/igj.v51i2.1369
_version_ 1766133526903652352