Eutrophication hotspots, nitrogen fluxes and climate impacts in estuarine ecosystems: A model study of the Odra estuary system

IF 2.2 3区 地球科学 Q2 OCEANOGRAPHY Ocean Dynamics Pub Date : 2024-03-05 DOI:10.1007/s10236-024-01607-w
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Abstract

The Odra estuary in the southern Baltic Sea comprises the Odra (Szczecin) Lagoon, the Pomeranian Bay and a number of other shallow water areas and channels. Known for its abundance of fish, eutrophication in the Odra Lagoon is a pressing issue for science and environmental management representing a global problem: What determines the seasonal variability of nitrogen and nitrogen turnover in shallow water areas, and how does seasonal variability change due to climatic changes such as warming and sea level rise? How do such changes affect nutrient exports to the regional ocean? This study employs a high-resolution unstructured model system to investigate physical-biogeochemical interactions, nitrogen turnover, and conditions leading to nitrogen export to the Baltic Sea within the Odra estuary. The research comprises hindcast and a climatic experiment with modified water level and temperature inputs. The model reproduces the thermohaline dynamics of brackish shallow water areas, phytoplankton blooms and the variability of inorganic nitrogen. The simulations identify the dynamic partitioning of the Odra Lagoon into the highly eutrophic, lake-like Small Lagoon and more frequently flushed, zooplankton-rich Great Lagoon. Although the two years of the hindcast simulation feature very different boundary conditions in terms of river forcing, comparable patterns of seasonal nitrogen export emerge. In a climate change experiment with increased sea levels and global temperatures, the system appears sensitive, but remains stable with regard to nutrient transport and is therefore predictable. The climate change experiment reveals enhanced primary producer biomass concentrations, suggesting heightened eutrophication. While in the shallow waters of Odra Lagoon oxygen concentration remains relatively stable, oxygen depletion intensifies as the lagoon outflows enter the Pomeranian Bay. This phenomenon is linked to increased denitrification within the stratified Odra plume. Deeper, meandering channels, such as Swina, demonstrate resilience to oxygen reduction, influenced by sea level rise and enhanced currents. Based on the temporal-spatial high-resolution coupled, validated simulations, it is possible to develop tailor-made management solutions without having to run expensive and complicated observation campaigns in the shallow waters with complex topography.

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河口生态系统的富营养化热点、氮通量和气候影响:奥德拉河河口系统模型研究
摘要 波罗的海南部的奥德拉河河口由奥德拉(什切青)泻湖、波美拉尼亚湾以及其他一些浅水区和河道组成。奥德拉泻湖以鱼类丰富而闻名,其富营养化是科学和环境管理的一个紧迫问题,也是一个全球性问题:是什么决定了浅水区氮和氮周转的季节性变化?这些变化如何影响区域海洋的营养物质输出?本研究采用了一个高分辨率非结构化模型系统,以调查物理-生物地球化学相互作用、氮周转以及导致奥德拉河口内氮向波罗的海输出的条件。研究内容包括后报和气候实验,并对水位和温度输入进行了修改。该模型再现了咸水浅水区的温盐动态、浮游植物的繁殖和无机氮的变化。模拟确定了奥德拉泻湖的动态分区,即高度富营养化、类似湖泊的小泻湖和更频繁冲刷、富含浮游动物的大泻湖。虽然后报模拟的两个年份在河流作用力方面的边界条件截然不同,但却出现了类似的季节性氮输出模式。在海平面和全球气温升高的气候变化实验中,该系统似乎很敏感,但在营养物质迁移方面保持稳定,因此是可以预测的。气候变化实验显示初级生产者生物量浓度增加,表明富营养化加剧。虽然奥德拉泻湖浅水区的氧气浓度保持相对稳定,但当泻湖外流进入波美拉尼亚湾时,氧气消耗加剧。这种现象与奥德拉河分层水流中脱氮作用的增强有关。在海平面上升和海流增强的影响下,斯维纳等较深的蜿蜒水道显示出氧气减少的恢复能力。基于时间-空间高分辨率耦合验证模拟,可以制定量身定制的管理解决方案,而无需在地形复杂的浅水区开展昂贵而复杂的观测活动。
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来源期刊
Ocean Dynamics
Ocean Dynamics 地学-海洋学
CiteScore
5.40
自引率
0.00%
发文量
37
审稿时长
6-12 weeks
期刊介绍: Ocean Dynamics is an international journal that aims to publish high-quality peer-reviewed articles in the following areas of research: Theoretical oceanography (new theoretical concepts that further system understanding with a strong view to applicability for operational or monitoring purposes); Computational oceanography (all aspects of ocean modeling and data analysis); Observational oceanography (new techniques or systematic approaches in measuring oceanic variables, including all aspects of monitoring the state of the ocean); Articles with an interdisciplinary character that encompass research in the fields of biological, chemical and physical oceanography are especially encouraged.
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