Trends in ocean waves climate within the Mediterranean Sea: a review

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Climate Dynamics Pub Date : 2023-10-21 DOI:10.1007/s00382-023-06984-4
Francesco De Leo, Riccardo Briganti, Giovanni Besio
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Abstract

Abstract The interest for the impact of climate change on ocean waves within the Mediterranean Sea has motivated a number of studies aimed at identifying trends in sea states parameters from historical multi-decadal wave records. In the last two decades progress in computing and the availability of suitable time series from observations further supported research on this topic. With the aim of identifying consensus among previous research on the Mediterranean Sea and its sub-basins, this review analysed the results presented in peer reviewed articles researching historical ocean waves trends published after the year 2000. Most studies focused on the significant wave height trends, while direction and wave period appear to be under-studied in this context. We analysed trends in mean wave climate and extreme sea states. We divided the Mediterranean basin in 12 sub-basins and analysed the results available in the literature from a wide range of data sources, such as satellite altimetry and numerical models, among others. The consensus on the significant wave height mean climate trends is limited, while statistically significant trends in extreme values are detected in the western Mediterranean Sea, in particular in the Gulf of Lion and in the Tyrrhenian Sea, with complex spatial distributions. Negative extreme sea state trends in the sub-basins, although frequently identified, are mostly not significant. We discuss the sources of uncertainty in results introduced by the data used, statistics employed to characterise mean or extreme conditions, length of the time period used for the analysis, and thresholds used to prove trends statistical significance. The reduction of such uncertainties, and the relationship between trends in sea states and weather processes are identified as priority for future research.
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地中海内海浪气候趋势:综述
气候变化对地中海内海浪影响的兴趣激发了许多旨在从历史多年代际波浪记录中确定海况参数趋势的研究。在过去的二十年中,计算的进步和从观测中获得合适的时间序列进一步支持了这一主题的研究。为了确定先前关于地中海及其子盆地的研究的共识,本综述分析了同行评议的研究2000年以后发表的历史海浪趋势的文章的结果。大多数研究集中在显著的波高趋势上,而方向和波周期在这方面的研究似乎不足。我们分析了平均波浪气候和极端海况的趋势。我们将地中海盆地划分为12个子盆地,并分析了文献中来自广泛数据源的结果,例如卫星测高和数值模型等。关于显著波高平均气候趋势的共识有限,而在地中海西部,特别是在狮子湾和第勒尼安海,发现了具有统计意义的极端值趋势,具有复杂的空间分布。子盆地的负极端海况趋势虽然经常被发现,但大多不显著。我们讨论了所使用的数据、用于描述平均或极端条件的统计数据、用于分析的时间段长度以及用于证明趋势统计显著性的阈值所带来的结果不确定性的来源。减少这种不确定性以及海况趋势与天气过程之间的关系被确定为未来研究的重点。
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来源期刊
Climate Dynamics
Climate Dynamics 地学-气象与大气科学
CiteScore
8.80
自引率
15.20%
发文量
483
审稿时长
2-4 weeks
期刊介绍: The international journal Climate Dynamics provides for the publication of high-quality research on all aspects of the dynamics of the global climate system. Coverage includes original paleoclimatic, diagnostic, analytical and numerical modeling research on the structure and behavior of the atmosphere, oceans, cryosphere, biomass and land surface as interacting components of the dynamics of global climate. Contributions are focused on selected aspects of climate dynamics on particular scales of space or time. The journal also publishes reviews and papers emphasizing an integrated view of the physical and biogeochemical processes governing climate and climate change.
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