Wind Waves in the Mediterranean Sea: An ERA5 Reanalysis Wind-Based Climatology
A climatology of the wind waves in the Mediterranean Sea is presented. The climate patterns, their spatio-temporal variability and change are based on a 40-year (1980–2019) wave hindcast, obtained by combining the ERA5 reanalysis wind forcing with the state-of-the-art WAVEWATCH III spectral wave mod...
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Frontiers Media S.A.
2021
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oai:doaj.org-article:b393a234db234052a9c7f5666191f6fa2021-11-16T15:54:00ZWind Waves in the Mediterranean Sea: An ERA5 Reanalysis Wind-Based Climatology2296-774510.3389/fmars.2021.760614https://doaj.org/article/b393a234db234052a9c7f5666191f6fa2021-11-01T00:00:00Zhttps://www.frontiersin.org/articles/10.3389/fmars.2021.760614/fullhttps://doaj.org/toc/2296-7745A climatology of the wind waves in the Mediterranean Sea is presented. The climate patterns, their spatio-temporal variability and change are based on a 40-year (1980–2019) wave hindcast, obtained by combining the ERA5 reanalysis wind forcing with the state-of-the-art WAVEWATCH III spectral wave model and verified against satellite altimetry. Results are presented for the typical (50th percentile) and extreme (99th percentile) significant wave height and, for the first time at the regional Mediterranean Sea scale, for the typical and extreme expected maximum individual wave height of sea states. The climate variability of wind waves is evaluated at seasonal scale by proposing and adopting a definition of seasons for the Mediterranean Sea states that is based on the satellite altimetry wave observations of stormy (winter) and calm (summer) months. The results, initially presented for the four seasons and then for winter and summer only, show the regions of the basin where largest waves occur and those with the largest temporal variability. A possible relationship with the atmospheric parameter anomalies and with teleconnection patterns (through climate indices) that motivates such variability is investigated, with results suggesting that the Scandinavian index variability is the most correlated to the Mediterranean Sea wind-wave variability, especially for typical winter sea states. Finally, a trend analysis shows that the Mediterranean Sea typical and extreme significant and maximum individual wave heights are decreasing during summer and increasing during winter.Francesco BarbariolSilvio DavisonFrancesco Marcello FalcieriRossella FerrettiRossella FerrettiAntonio RicchiAntonio RicchiMauro SclavoAlvise BenetazzoFrontiers Media S.A.articlewave climateMediterranean SeaERA5maximum wavesclimate indicesclimate trendsScienceQGeneral. Including nature conservation, geographical distributionQH1-199.5ENFrontiers in Marine Science, Vol 8 (2021) |
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wave climate Mediterranean Sea ERA5 maximum waves climate indices climate trends Science Q General. Including nature conservation, geographical distribution QH1-199.5 |
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wave climate Mediterranean Sea ERA5 maximum waves climate indices climate trends Science Q General. Including nature conservation, geographical distribution QH1-199.5 Francesco Barbariol Silvio Davison Francesco Marcello Falcieri Rossella Ferretti Rossella Ferretti Antonio Ricchi Antonio Ricchi Mauro Sclavo Alvise Benetazzo Wind Waves in the Mediterranean Sea: An ERA5 Reanalysis Wind-Based Climatology |
description |
A climatology of the wind waves in the Mediterranean Sea is presented. The climate patterns, their spatio-temporal variability and change are based on a 40-year (1980–2019) wave hindcast, obtained by combining the ERA5 reanalysis wind forcing with the state-of-the-art WAVEWATCH III spectral wave model and verified against satellite altimetry. Results are presented for the typical (50th percentile) and extreme (99th percentile) significant wave height and, for the first time at the regional Mediterranean Sea scale, for the typical and extreme expected maximum individual wave height of sea states. The climate variability of wind waves is evaluated at seasonal scale by proposing and adopting a definition of seasons for the Mediterranean Sea states that is based on the satellite altimetry wave observations of stormy (winter) and calm (summer) months. The results, initially presented for the four seasons and then for winter and summer only, show the regions of the basin where largest waves occur and those with the largest temporal variability. A possible relationship with the atmospheric parameter anomalies and with teleconnection patterns (through climate indices) that motivates such variability is investigated, with results suggesting that the Scandinavian index variability is the most correlated to the Mediterranean Sea wind-wave variability, especially for typical winter sea states. Finally, a trend analysis shows that the Mediterranean Sea typical and extreme significant and maximum individual wave heights are decreasing during summer and increasing during winter. |
format |
article |
author |
Francesco Barbariol Silvio Davison Francesco Marcello Falcieri Rossella Ferretti Rossella Ferretti Antonio Ricchi Antonio Ricchi Mauro Sclavo Alvise Benetazzo |
author_facet |
Francesco Barbariol Silvio Davison Francesco Marcello Falcieri Rossella Ferretti Rossella Ferretti Antonio Ricchi Antonio Ricchi Mauro Sclavo Alvise Benetazzo |
author_sort |
Francesco Barbariol |
title |
Wind Waves in the Mediterranean Sea: An ERA5 Reanalysis Wind-Based Climatology |
title_short |
Wind Waves in the Mediterranean Sea: An ERA5 Reanalysis Wind-Based Climatology |
title_full |
Wind Waves in the Mediterranean Sea: An ERA5 Reanalysis Wind-Based Climatology |
title_fullStr |
Wind Waves in the Mediterranean Sea: An ERA5 Reanalysis Wind-Based Climatology |
title_full_unstemmed |
Wind Waves in the Mediterranean Sea: An ERA5 Reanalysis Wind-Based Climatology |
title_sort |
wind waves in the mediterranean sea: an era5 reanalysis wind-based climatology |
publisher |
Frontiers Media S.A. |
publishDate |
2021 |
url |
https://doaj.org/article/b393a234db234052a9c7f5666191f6fa |
work_keys_str_mv |
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1718426322547507200 |