西班牙沿岸地表和海底海洋热浪评估

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Ocean Modelling Pub Date : 2024-06-18 DOI:10.1016/j.ocemod.2024.102399
Manuel Fernández-Barba, I. Emma Huertas, Gabriel Navarro
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引用次数: 0

摘要

海洋热浪(MHWs)是海洋温度异常升高的离散而持续的事件,由于其对全球海洋生态系统的广泛破坏,已成为气候变化研究的热门话题。因此,全世界通常都采用统一的方法来描述表层海洋高温热事件(SMHWs)及其驱动因素。然而,由于可获得的数据有限,人们对地下和底层的马赫沃事件(BMHWs)知之甚少。此外,最近的进展表明,MHW 的定义需要改进,以便将极端事件与长期海洋变暖区分开来。在此,我们利用 1993 年至 2022 年的高分辨率 GLORYS12V1 再分析数据,描述了《海洋战略框架指令》中定义的西班牙海洋划界(SMD)区域内的 SMHW 和 BMHW 的特征。我们还对它们之间的相互联系进行了广泛分析,并最终对 SMD 与 MHWs 的综合接触情况进行了区域评估。我们发现,在过去的 15 年中,小型、中型和大型水体风暴强度更大、持续时间更长、范围更广。我们还发现,当海洋表层热通量异常时,SMHWs 表现出空间变化,而 BMHWs 则与海洋底层深度成正比,且持续时间比表层异常更长。此外,在混合层延伸到海底的较浅沿岸地区,BMHW 的平均强度可以与同时叠加在表层的 BMHW 相媲美,甚至更高。最后,我们还证明,在沿岸 SMD 区域,SMHWs 和 BMHWs 都更有可能同时出现高累积强度,其 69%的空间范围被归类为高度暴露于 MHWs。这突出表明,在评估和应对预期气候变化情景下当前和未来对野生动物和经济的影响时,迫切需要分析和整合 SMHWs 和 BMHWs,尤其是在沿海地区。
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Assessment of surface and bottom marine heatwaves along the Spanish coast

Marine heatwaves (MHWs) are discrete yet persistent events of anomalously warm ocean temperatures which are becoming a hot topic in climate change research due to their extensive disruption of marine ecosystems worldwide. As a consequence, surface MHW events (SMHWs) and their drivers have been characterised worldwide typically under a consolidated common methodology. However, subsurface and bottom events of MHW (BMHWs) are less known due to the limited availability of data. Furthermore, recent advances suggest an improved MHW definition to distinguish the extreme event from the long-term ocean warming. Here, we use high-resolution GLORYS12V1 reanalysis data from 1993 to 2022 to characterise both SMHWs and BMHWs along the Spanish Marine Demarcation (SMD) areas defined within the Marine Strategy Framework Directive. We also broadly analyse their interconnections and ultimately generate a regional assessment of the integrated exposure of SMD to MHWs. We find that both SMHWs and BMHWs were more intense, longer-lasting, and widespread over the last 15 years. We also find that while SMHWs exhibit spatial variation following heat fluxes anomalies in the ocean surface layers, BMHWs roughly scale with ocean bottom depth and persist longer than their surface counterparts. Further, in shallower coastal regions where the mixed layer extends to the ocean bottom, average BMHW intensities can be comparable or even higher than those concurrently overlaying at the surface. Finally, we also demonstrate that both SMHWs and BMHWs are more likely to co-occur with high cumulative intensities in coastal SMD areas, with the 69% of their spatial extent categorised as highly exposed to MHWs. This highlights the imperative need for analysing and integrating SMHWs and BMHWs, especially in coastal zones, when assessing and addressing present and future impacts on wildlife and economies under the expected climate change scenario.

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来源期刊
Ocean Modelling
Ocean Modelling 地学-海洋学
CiteScore
5.50
自引率
9.40%
发文量
86
审稿时长
19.6 weeks
期刊介绍: The main objective of Ocean Modelling is to provide rapid communication between those interested in ocean modelling, whether through direct observation, or through analytical, numerical or laboratory models, and including interactions between physical and biogeochemical or biological phenomena. Because of the intimate links between ocean and atmosphere, involvement of scientists interested in influences of either medium on the other is welcome. The journal has a wide scope and includes ocean-atmosphere interaction in various forms as well as pure ocean results. In addition to primary peer-reviewed papers, the journal provides review papers, preliminary communications, and discussions.
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