Long-term statistics of atmospheric conditions over the Baltic Sea and meteorological features related to wind wave extremes in the Gulf of Gdańsk

IF 2.6 3区 地球科学 Q2 OCEANOGRAPHY
Witold Cieślikiewicz , Aleksandra Cupiał
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Abstract

The goal of this study is to describe wind wave climate and wave extremes of the Gulf of Gdańsk in the southern Baltic Sea and associated meteorological conditions over the Baltic Sea. We obtain the characteristic features of 34 severe historical storms in the Gulf of Gdańsk during the period 1958–2001 and link them with extreme significant wave heights hindcast for five grid points in this gulf. The long-term statistics of atmospheric pressure systems over central and northern Europe, and the north-eastern Atlantic Ocean are derived from a 44-year REMO reanalysis database. A link between the mean, minimum and variability range of atmospheric pressure has been quantified. In general, the higher the mean pressure the smaller its variability and vice versa. Long-term characteristic features of winds over the Baltic Sea have been estimated from the REMO database. Strong winds directions vary from W, WSW to SW in the southern Baltic to more southerly SSW directions in the northern part of the Baltic Sea. The Empirical Orthogonal Functions (EOF) analysis shows that more than 50% of the variability in the atmospheric pressure in the Baltic Sea can be explained by the first EOF mode. The first four EOF modes can reproduce above 90% variability of the hindcast pressure time series. Statistical properties of the hindcast significant wave height over the Gulf of Gdańsk are computed based on the 44-year HIPOCAS database. All the computed statistics of wave heights reveal a very strong sheltering effect caused by the Hel Peninsula.

波罗的海上空大气状况的长期统计数据以及格但斯克湾与极端风浪有关的气象特征
本研究的目的是描述波罗的海南部格但斯克湾的风浪气候和极端波浪以及波罗的海上空的相关气象条件。我们获得了 1958-2001 年期间格但斯克湾 34 次严重历史风暴的特征,并将其与该海湾五个网格点的极端显著波浪高度后报联系起来。欧洲中部和北部以及大西洋东北部大气压力系统的长期统计数据来自 44 年的 REMO 再分析数据库。对大气压力的平均值、最小值和变化范围之间的联系进行了量化。一般来说,平均气压越高,其变化范围就越小,反之亦然。根据 REMO 数据库估算出了波罗的海上空风的长期特征。波罗的海南部的强风方向从西风、西南风到西南风不等,而波罗的海北部的强风方向则更偏南。经验正交函数(EOF)分析表明,波罗的海大气压力变化的 50%以上可以用第一个 EOF 模式来解释。前四个 EOF 模式可以再现后报气压时间序列 90% 以上的变化。根据 44 年的 HIPOCAS 数据库,计算了格但斯克湾后报显著波高的统计特性。所有计算得出的波高统计特性都显示,赫尔半岛具有很强的遮蔽效应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Oceanologia
Oceanologia 地学-海洋学
CiteScore
5.30
自引率
6.90%
发文量
63
审稿时长
146 days
期刊介绍: Oceanologia is an international journal that publishes results of original research in the field of marine sciences with emphasis on the European seas.
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