波罗的海物理再分析数据与库尔斯沙嘴沿岸海水温度原位测量数据间的偏差

作者

  • E. A. Vasilyeva Shirshov Institute of Oceanology, Russian Academy of Sciences; Immanuel Kant Baltic Federal University
  • A. V. Kileso Shirshov Institute of Oceanology, Russian Academy of Sciences; Immanuel Kant Baltic Federal University
  • A. E. Isachenko Shirshov Institute of Oceanology, Russian Academy of Sciences

DOI:

https://doi.org/10.29006/1564-2291.JOR-2025.53(4).1

关键词:

原位测量, 热敏链, 海水温度, 再分析数据, 温度偏差, 沿岸水域, 波罗的海

摘要

本研究对波罗的海物理再分析数据与库尔斯沙嘴(俄罗斯加里宁格勒州)沿岸波罗的海海域海水 温度原位测量数据之间的偏差进行了最新评估。评估的必要性在于需重建和诊断分析波罗的海沿岸区域 既往发生的极端事件,并需利用数值模拟方法对极端天气条件可能加剧沿岸带岩石动力过程的潜在影响 进行预测性分析。 通过将BALTICSEA_REANALYSISPHY_03_011计算数据与仪器测量数据进行对比,获得了水 温偏差的定量评估结果。仪器测量数据由安装在距岸约20公里的D6平台上的热敏链式传感器获得。分析 发现, 2018年近岸水域表层(5米)、中层(13米)和深层(20米)的计算温度与实测温度存在显著偏差( 最高达6°C)。 2018年10月和5月的水体密度偏差分别为-0.2至-0.13 kg/m³和0.025至0.25 kg/m³,并伴有 相应的温度偏差。这可能影响水体动力学计算的准确性,在极端天气条件下的数值模拟中尤为显著。本研 究结果表明,在数值模拟库尔斯沙嘴沿岸水域动力过程时,直接使用BALTICSEA REANALYSIS数据 可能导致结果不准确。

参考


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已出版

2025-12-21

期次

栏目

海洋物理学与气候

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