Characteristics of Marine Heatwaves of the Baltic Sea for 1993−2022 and Their Driving Factors

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS pure and applied geophysics Pub Date : 2024-05-30 DOI:10.1007/s00024-024-03504-1
Vladimir S. Travkin, Natalia A. Tikhonova, Eugeny A. Zakharchuk
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Abstract

Marine heatwaves (MHWs) are extreme ocean events with prolonged discrete periods of anomalously warm water, that have significant impacts on fisheries, tourism, and marine ecosystems. We identify MHWs as discrete periods (≥ 5 days) when the sea surface temperature exceeds the threshold (90th percentile) of the sea surface temperature distribution for specific calendar days and analyze their main properties in the Baltic Sea for the period 1993−2022. Also, we investigate the main mechanisms of evolution one of the most intense and continuous MHW, observed from October 2000 to March 2001. We use temperature, salinity, mixed layer depth, and current velocity daily data from regional reanalysis of the Baltic Sea (2 nautical mile horizontal resolution, vertical step from 1 m on the surface to 24 m on the bottom). We also use monthly data from global climate reanalysis ECMWF ERA5 (0.25° × 0.25°) and meteorological stations of the Swedish Meteorological and Hydrological Institute. From 40 to 90 MHWs with an average duration and intensity (8−24 days and 1.75−3.25 °C) were detected in various parts of the Baltic Sea during the period 1993−2022. The maximum cumulative values (> 2400 °C days) were observed in the Gotland Basins, the Gulf of Finland, and the Gulf of Riga. The mean intensity and cumulative values of MHWs are stronger in summer (3.6 °C and 740 °C days). A long existence of MHW in the autumn–winter period 2000–2001 was associated with positive air temperature anomalies (> 4 °C) and a sharp weakening of wind speed in the Baltic region.

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1993-2022 年波罗的海海洋热浪的特征及其驱动因素
海洋热浪(MHWs)是一种极端的海洋事件,具有长时间不连续的异常暖水期,对渔业、旅游业和海洋生态系统有重大影响。我们将 MHWs 识别为特定日历日海面温度超过海面温度分布阈值(第 90 百分位数)的离散时段(≥ 5 天),并分析了 1993-2022 年期间波罗的海的 MHWs 主要特性。此外,我们还研究了 2000 年 10 月至 2001 年 3 月期间观测到的一次最强烈、最持续的 MHW 演变的主要机制。我们使用了波罗的海区域再分析的温度、盐度、混合层深度和流速日数据(水平分辨率为 2 海里,垂直步长从海面 1 米到海底 24 米)。我们还使用了全球气候再分析 ECMWF ERA5(0.25°×0.25°)和瑞典气象水文研究所气象站的月度数据。1993-2022 年期间,在波罗的海不同地区检测到 40 至 90 次 MHW,平均持续时间和强度(8-24 天和 1.75-3.25 °C)。最大累积值(> 2400 °C 天)出现在哥特兰盆地、芬兰湾和里加湾。夏季最高气温的平均强度和累积值(3.6 ° C 和 740 ° C 天)较高。在 2000-2001 年秋冬季期间,波罗的海地区长期存在的 MHW 与正气温异常(> 4 °C)和风速急剧减弱有关。
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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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