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Environmental DNA (eDNA) detection reveals strong connectivity and similar co-occurrence patterns of planktonic and benthic eukaryote communities in Dinghai bay 环境DNA (Environmental DNA, eDNA)检测显示,定海湾浮游生物和底栖真核生物群落具有较强的连通性和相似的共生模式
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-07-18 DOI: 10.1016/j.csr.2025.105525
Qiushi Chen , Qianqian Liu , Peng Xiao , Yifan Ma , Zhongzhou Lin , Zhuoyi Zhu , Lianming Zheng , Wenjing Zhang
Exploring the relationship between planktonic and benthic eukaryotes in coastal zones is of great significance for us to further understand the influence of environmental conditions on microbial ecosystems and the integrated management of biological resources and ecological landscape in coastal areas. In this study, environmental DNA (eDNA), co-occurrence network analysis and the SourceTracker analysis were used to analyze seawater and sediment samples from Dinghai Bay, Fujian Province. Community structure, diversity, and co-occurrence patterns of eukaryotes, especially microeukaryotes in different habitats were compared. The results showed that: (1) There are differences between planktonic and benthic eukaryote communities to some extent. The diversity of benthic eukaryotes is significantly higher than that of planktonic eukaryotes. Environmental factors such as transparency, TDS (total dissolved solids) and salinity are significantly correlated with planktonic eukaryotes, while benthic eukaryotes are only correlated with conductivity. In addition, the planktonic community shows a strong distance-decay pattern while the benthic community did not. (2) There is strong connectivity between planktonic and benthic eukaryotes. The proportion of shared zero-radius operational taxonomic units (ZOTUs) in planktonic and benthic eukaryotes was 96.70% and 77.65%, respectively, and more than 92% of shared ZOTUs were not significantly different between two habitats. In addition, SourceTracker analysis showed that 59.70% of the benthos came from the planktonic community and 91.22% of the plankton from the benthic community. Plankton such as copepod, diatoms, dinoflagellata and ciliates live in sediments at some life stages,and there is often a planktonic larval stage in the life cycle of benthos. On the other hand, our study area is located in the intertidal zone and subtidal zone with special environmental conditions, which is influenced by tides, winds and river freshwater, and the constant mixing of surface and bottom water is also a possible reason. (3) The co-occurrence network analysis shows that the co-occurrence patterns of eukaryotes in the two habitats are similar to a considerable degree. Positive correlations are dominant in both planktonic and benthic communities, and the ratio of positive and negative correlations has no significant difference between two communities.
探索海岸带浮游生物与底栖真核生物之间的关系,对于我们进一步了解环境条件对微生物生态系统的影响,以及海岸带生物资源与生态景观的综合管理具有重要意义。本研究采用环境DNA (environmental DNA, eDNA)、共生网络分析和SourceTracker分析方法对福建定海湾海水和沉积物样本进行了分析。比较了不同生境真核生物,特别是微真核生物的群落结构、多样性和共生模式。结果表明:(1)浮游与底栖真核生物群落存在一定差异。底栖真核生物的多样性明显高于浮游真核生物。透明度、TDS (total dissolved solids)和盐度等环境因子与浮游真核生物显著相关,而底栖真核生物仅与电导率相关。此外,浮游生物群落表现出强烈的距离衰减模式,而底栖生物群落则没有。(2)浮游真核生物与底栖真核生物之间存在较强的连通性。浮游和底栖真核生物共享零半径操作分类单元(ZOTUs)的比例分别为96.70%和77.65%,其中92%以上的共享ZOTUs在两种生境间差异不显著。此外,SourceTracker分析显示,59.70%的底栖生物来自浮游生物群落,91.22%的浮游生物来自底栖生物群落。桡足类、硅藻、鞭毛类和纤毛虫等浮游生物在某些生命阶段生活在沉积物中,底栖动物的生命周期中往往有一个浮游幼虫阶段。另一方面,我们的研究区域位于潮间带和潮下带,环境条件特殊,受潮汐、风和河流淡水的影响,地底水的不断混合也是一个可能的原因。(3)共现网络分析表明,两个生境真核生物的共现模式具有相当程度的相似性。浮游和底栖群落均以正相关为主,正相关和负相关比例在群落间无显著差异。
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引用次数: 0
Effects of wave-current interaction on water exchange in the Bohai Sea 渤海波流相互作用对水交换的影响
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-07-18 DOI: 10.1016/j.csr.2025.105531
Sheng Wang , Xueen Chen , He Jiang , Peng Zheng
The Bohai Sea is a typical continental shelf region, and its water exchange capacity has long been the focus of research. Wave-current interaction (WCI), as an important physical process for the continental shelf hydrodynamics, is worthy of further investigation due to its impact on water exchange in the Bohai Sea. In this study, based on the FVCOM-UnSWAN wave-current coupling model, the water exchange characteristics of the Bohai Sea under the influence of WCI were discussed using the conservative material tracer method. The effects of WCI on water exchange and hydrodynamics were further analyzed under both seasonal variations and extreme weather events. As the only channel connecting the Yellow Sea and the Bohai Sea, changes in the water exchange capacity of the Bohai Strait can reflect the change of the Bohai Sea. Focusing on this region, our results show that WCI modulates water exchange rates: enhancing exchange by approximately 1.3 % in winter, while exhibiting complex behavior in summer, initially suppressing and subsequently enhancing water exchange. During storm surge events, WCI plays a crucial role in modifying hydrodynamic conditions, increasing water elevation by 20 %–35 %, with changes in water velocity up to an order of magnitude larger compared to seasonal scales. During the water exchange process, WCI modifies the current velocity structure by introducing a non-conservative force Fw, among which the white-capping dissipation term plays a dominant role.
渤海是典型的大陆架区域,其水交换能力一直是研究的热点。波流相互作用(WCI)作为大陆架水动力学的一个重要物理过程,对渤海水体交换的影响值得进一步研究。本研究基于FVCOM-UnSWAN波流耦合模型,采用保守示踪法讨论了WCI影响下渤海水体交换特性。进一步分析了季节变化和极端天气条件下WCI对水交换和水动力的影响。作为连接黄海和渤海的唯一通道,渤海海峡换水量的变化可以反映渤海的变化。针对这一区域,我们的研究结果表明,WCI调节水交换率:在冬季增加约1.3%的交换,而在夏季表现出复杂的行为,最初抑制,随后增加水交换。在风暴潮事件中,WCI在改变水动力条件方面起着至关重要的作用,使水位升高20% - 35%,与季节尺度相比,水流速度的变化要大一个数量级。在换水过程中,WCI通过引入非保守力Fw改变了水流速度结构,其中白盖耗散项起主导作用。
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引用次数: 0
Spatial-temporal reliability of satellite-derived temperature and thermal stress in the abrolhos bank, Brazil 巴西abrolhos银行卫星温度和热应力的时空可靠性
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-07-17 DOI: 10.1016/j.csr.2025.105529
Renato D. Ghisolfi , Natiely Monteiro , Guilherme N. Mill , Ruy K.P. Kikuchi , Rodrigo L. Moura
Accurate estimates of ocean temperatures are needed to assess the consequences and improve predictions of thermal stress over coral reefs, which are declining globally due to mass coral bleaching and mortality episodes caused by maritime heatwaves. Here, we contrasted satellite-derived sea surface temperatures (SSTs) recovered from NOAA Coral Reef Watch (CoralTemp) with in situ temperatures measured between 2012 and 2018 in nine locations within the Southwestern Atlantic's largest coral reefs (Abrolhos Bank, Brazil), at different depths. Our results revealed a strong correlation (over 0.95) between the two datasets for measurements carried out to 10 m depths or within the mixed layer. In the dry period (April to September), when the water column is homogenous and the net heat flux through the air-sea interface is negative, temperature data collected below the mixing layer or at the bottom were consistent with CoralTemp. However, in situ measurements were much lower (up to 4 °C at some sites) during the rainy period (from October to March) due to cold water occurrence in the bottom half of the water column. During the Third Global Bleaching Event (2016–2017) bleaching levels in shallow reefs were more intense than the thermal stress estimated by CoralTemp. Still, they were lower in the deeper reefs that remained with lower in situ temperatures throughout the summer and autumn. While we confirm that CoralTemp data provide a reliable source of sea surface temperatures (SSTs), caution is advised when inferring thermal stress at greater depths, particularly in mesophotic sites deeper than 20 m.
需要对海洋温度进行准确估计,以评估其后果并改进对珊瑚礁热应力的预测。由于海洋热浪造成的大规模珊瑚白化和死亡事件,珊瑚礁在全球范围内正在减少。在这里,我们将从NOAA珊瑚礁观察(CoralTemp)中恢复的卫星获得的海面温度(SSTs)与2012年至2018年在西南大西洋最大的珊瑚礁(巴西Abrolhos Bank)内九个地点不同深度测量的原位温度进行了对比。我们的结果显示,在10米深度或混合层内进行的测量中,两个数据集之间存在很强的相关性(超过0.95)。在干旱期(4 ~ 9月),当水柱均匀且海气界面净热通量为负时,混合层以下或底部的温度数据与CoralTemp一致。然而,在雨季(10月至3月),由于水柱下半部分出现冷水,现场测量值要低得多(在某些地点高达4°C)。在第三次全球白化事件(2016-2017)期间,浅层珊瑚礁的白化程度比CoralTemp估计的热应力更严重。尽管如此,它们在整个夏秋季节保持较低原位温度的较深珊瑚礁中的位置较低。虽然我们确认CoralTemp数据提供了可靠的海表温度(SSTs)来源,但在推断更深深度的热应力时,特别是在深度超过20米的中深水点,建议谨慎。
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引用次数: 0
A three-year survey of hatched elasmobranch egg capsules on Santa Catarina Island, Southern Brazil 在巴西南部的圣卡塔琳娜岛,一项为期三年的对已孵化的依拉斯莫科卵囊的调查
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-07-17 DOI: 10.1016/j.csr.2025.105528
Carlos Alberto da Silva Junior , Guilherme Burg Mayer , Áthila Andrade Bertoncini , Rafael de Lima , Renato Hajenius Aché de Freitas
Over a three-year survey, the present study investigated the diversity of hatched elasmobranch egg capsules along the six beaches of Santa Catarina Island, Southern Brazil. Egg capsules (1,773) from seven elasmobranch taxa were record, including six skate taxa (Atlantoraja castelnaui, Atlantoraja spp., Psammobatis spp., Rioraja agassizii, Sympterygia acuta, and Sympterygia bonapartii) and, notably, the first report of a shark egg capsules on a Brazilian beach, the frecked catshark Scyliorhinus haeckelii. The three species with the highest number of collected egg capsules (>90) were selected to assess the influence of temperature on their reproductive cycles. There was a predominance of capsules in the warm (spring and summer) season for S. acuta and Psammobatis spp. There was no significant difference in the number of egg capsules between warm and cold (autumn and winter) seasons for R. agassizii, suggesting an active reproductive pattern throughout the year. We also verified the difference in the number of egg capsules among six beaches using data from R. agassizii which was related to areas sheltered (rocky coastline, island) from winds and prevailing ocean currents along the island. These findings were important to increase the knowledge of oviparous elasmobranch species from the Western South Atlantic, underscoring the importance of egg capsule monitoring to understand the biodiversity and reproductive ecology of the local species, which are crucial for effective conservation strategies.
在一项为期三年的调查中,本研究调查了巴西南部圣卡塔琳娜岛六个海滩上孵化的依丝木纲卵囊的多样性。记录了7个鲨科分类的卵囊(1773个),其中包括6个鳐分类(Atlantoraja castelnaui, Atlantoraja spp, Psammobatis spp, Rioraja agassizii, Sympterygia acuta和Sympterygia bonapartii),值得注意的是,在巴西海滩上首次报道了鲨鱼卵囊,斑点猫鲨Scyliorhinus haeckelii。选取采集卵囊数最多的3种(90粒),评价温度对其繁殖周期的影响。有优势的胶囊在温暖的季节(春季和夏季)acuta和Psammobatis spp。没有显著差异的数量卵囊在冷与热之间(秋季和冬季)季节r . agassizii暗示一个活跃的生殖模式。我们还利用阿加assizii的数据验证了6个海滩之间卵囊数量的差异,这些数据与岛上受风和盛行洋流保护的地区(岩石海岸线,岛屿)有关。这些发现对于增加对南大西洋西部板鳃纲卵生物种的认识具有重要意义,强调了卵囊监测对了解当地物种的生物多样性和生殖生态的重要性,这对制定有效的保护策略至关重要。
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引用次数: 0
Evaluating influencing factors of methane interception in Bohai bay basin's aerobic zone based on experiment coupled with modeling 基于实验与模拟的渤海湾盆地好氧带甲烷截留影响因素评价
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-07-14 DOI: 10.1016/j.csr.2025.105527
Songhua Shang , Jiehao Li , Hailong Tian , Tianfu Xu , Wei Wang , Wei Yuan , Qinghe Niu , Yongxiang Zheng , Jing Li
Marine sediments serve as reservoirs for methane, a potent greenhouse gas and a promising clean energy source. As methane migrates from deep to shallow layers, it undergoes oxidation-reduction reactions with various electron acceptors, such as sulfate, nitrate, and oxygen. Aerobic Oxidation of Methane (AeOM) plays a crucial role where dissolved oxygen is available, particularly in marginal seas with shallow water depths. For now, research on AeOM is not in-depth, especially quantitative works. In the Bohai Sea's petroleum and natural gas basins, methane leakage from sediments is common, and conditions for methane oxidation are present. The sediments play a significant role in oxidizing methane, presenting a highly worthwhile subject for research. Therefore, utilizing laboratory data on AeOM, we employed the TOUGH + HR simulation platform to reproduce the AeOM process by an experimental conceptual model. The calibration of microbial kinetic parameters was conducted using sampling and testing data to analyze the characteristics of methane oxidation. Moreover, relationships between kinetic parameters and temperature were established, facilitating parameter estimation. The maximum oxidation rate (qm) shows an exponential relationship with temperature, whereas the microbial decay constant (b) displays a linear relationship. We quantitatively analyzed the characteristics of methane oxidation under different influencing factors, including temperature, pressure, and gas migration velocity. The results revealed that temperature is a key factor in determining methane consumption rates, with higher temperatures leading to significantly faster methane consumption due to its influence on microbial activity. The average oxidation rate was recorded as 0.35 μmol/day at 4 °C. This rate increased to 3.05 μmol/day at 10 °C and further rose to 3.96 μmol/day at 15 °C. Notably, there was a dramatic jump to 15.13 μmol/day when the temperature reached 28 °C. By enhancing methane supply (solubility), pressure can boost methane oxidation consumption. 1 MPa–5 MPa pressure increase raises average methane oxidation rates by 93 %. Methane migration velocity primarily affects the supply efficiency of methane and a 50 μL/min to 150 μL/min velocity increase raises rates by 10.3 %. Compared with the results across various temperatures, pressures, and methane migration velocities, we believe that temperature and pressure have a significant impact on methane oxidation consumption, while methane migration velocity has no significant impact. The temperature and pressure changes should be focused on to evaluate the effect of sediment on methane oxidation interception. This study enhances the understanding of the quantitative assessment of seabed methane leakage and the marine sediment carbon cycle.
海洋沉积物是甲烷的储存库,甲烷是一种强有力的温室气体,也是一种有前途的清洁能源。当甲烷从深层迁移到浅层时,它与各种电子受体(如硫酸盐、硝酸盐和氧气)发生氧化还原反应。甲烷的有氧氧化(AeOM)在溶解氧可用的地方起着至关重要的作用,特别是在水深较浅的边缘海域。目前,对AeOM的研究还不够深入,尤其是定量研究。渤海油气盆地沉积物中甲烷泄漏较为普遍,具有甲烷氧化的条件。沉积物在氧化甲烷中起着重要的作用,是一个非常值得研究的课题。因此,我们利用AeOM的实验室数据,采用TOUGH + HR模拟平台,通过实验概念模型再现AeOM过程。利用采样和检测数据对微生物动力学参数进行标定,分析甲烷氧化特性。建立了动力学参数与温度之间的关系,便于参数估计。最大氧化速率(qm)与温度呈指数关系,而微生物衰变常数(b)与温度呈线性关系。定量分析了温度、压力、运移速度等不同影响因素下的甲烷氧化特征。结果表明,温度是决定甲烷消耗速率的关键因素,由于温度对微生物活性的影响,较高的温度导致甲烷消耗明显加快。4℃时平均氧化速率为0.35 μmol/d。该速率在10℃时增加到3.05 μmol/d,在15℃时进一步增加到3.96 μmol/d。当温度达到28℃时,浓度急剧上升至15.13 μmol/d。通过增加甲烷供应(溶解度),压力可以促进甲烷氧化消耗。压力增加1 MPa - 5 MPa,平均甲烷氧化率提高93%。甲烷运移速度主要影响甲烷的供给效率,50 μL/min ~ 150 μL/min速率可使甲烷供给效率提高10.3%。对比不同温度、压力和甲烷迁移速度的结果,我们认为温度和压力对甲烷氧化消耗有显著影响,而甲烷迁移速度没有显著影响。评价沉积物对甲烷氧化截留的影响应重点关注温度和压力的变化。该研究增强了对海底甲烷泄漏和海洋沉积物碳循环定量评价的认识。
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引用次数: 0
The role of sediment transport processes in shaping offshore sand waves 泥沙输运过程在近海沙浪形成中的作用
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-07-13 DOI: 10.1016/j.csr.2025.105513
Pauline H.P. Overes , Bas W. Borsje , Arjen P. Luijendijk , Johan Reyns , Suzanne J.M.H. Hulscher
Sand waves, large scale dynamic bedforms, which are found on sandy, shallow seabeds worldwide, present an immediate risk to offshore structures, raising a pressing need for predicting related bed level dynamics on decadal timescales. Numerical models can help us understand and predict sand wave dynamics, but have shown difficulties with preserving sand wave shapes. Using the process-based Delft3D Flexible Mesh model, we have found that the choice of sediment transport formulation has a significant effect on the stability of sand wave shapes. The widely used Van Rijn (1993) sediment transport formulation predicts relatively high bed load transport rates, thereby raising a need for more dominant slope-induced transport. The simulations revealed that the Van Rijn (2007) formulation, which predicts relatively lower transport rates, and thus allows for lower bed slope-induced transports, is better capable of preserving the steep slopes of sand waves, while limiting sand wave growth. By considering various shape characteristics in our model assessment, more insight is gained about the improvements as well as adverse effects of changes in the parameterization of physical processes. These characteristics show that only with the less dominant bed slope-induced transport the crest levels are stable, while trough levels still lower slowly over time. This indicates that local processes are responsible for limiting the growth of sand waves and the importance of slope-induced transport has been overstated in previous works. With the adapted, non-upscaled set-up, the evolution of sand waves over multiyear timescales is represented well in the model compared to bathymetric field data for two contrasting sand wave field sites.
沙波是一种分布在世界各地沙质浅海床上的大尺度动态床型,对近海结构构成直接威胁,因此迫切需要在年代际尺度上预测相关的床位动力学。数值模型可以帮助我们理解和预测沙波动力学,但在保存沙波形状方面存在困难。利用基于过程的Delft3D柔性网格模型,我们发现泥沙输沙公式的选择对沙波形状的稳定性有显著影响。广泛使用的Van Rijn(1993)泥沙输运公式预测了相对较高的河床输运率,从而提出了对更主要的斜坡诱导输运的需求。模拟结果表明,Van Rijn(2007)公式预测了相对较低的输运率,从而允许较低的床坡引起的输运,能够更好地保持沙波的陡坡,同时限制沙波的增长。通过在我们的模型评估中考虑各种形状特征,对物理过程参数化变化的改进和不利影响有了更多的了解。这些特征表明,只有在坡面输运不占优势的情况下,波峰水平是稳定的,而波谷水平随时间缓慢下降。这表明,局部过程对沙波的增长起着限制作用,而斜坡引起的输运的重要性在以前的工作中被夸大了。与两个对比沙波场的水深场数据相比,采用经过调整的、非升级的设置,该模型可以很好地代表多年时间尺度上的沙波演变。
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引用次数: 0
Seasonal variation and response of surf zone fish assemblages to environmental variables in the Northeast Pacific 东北太平洋冲浪带鱼类群落的季节变化及其对环境变量的响应
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-07-12 DOI: 10.1016/j.csr.2025.105526
Gammon N. Koval , Jenifer E. Dugan , Scott L. Hamilton
Located at the land-sea interface, the highly dynamic sandy beach and surf zone ecosystem is one of the coastal zones used most intensely by humans (e.g., recreation, fishing, tourism). Surf zones are also important as fish habitat; however, the factors structuring fish assemblages in the surf zone are relatively understudied due to challenges associated with sampling this dynamic environment. To investigate temporal influences on surf zone fish communities, we evaluated seasonal trends in the fish assemblage and associations with environmental conditions using baited remote underwater video stations (BRUVS) at four beaches on the Northeast Pacific coast (California, USA) from July 2020 to June 2021. Our study region is characterized by strong seasonality in productivity (due to spring upwelling) and the wave climate (in response to winter storms), making it an ideal location for evaluating seasonal change in surf zone fish. We found that surf zone fish assemblages exhibited marked seasonality and site-to-site variability. Two species of surfperch (Amphistichus argenteus and A. koelzi) and leopard sharks (Triakis semifasciata) were more common in the winter and spring, corresponding with surfperch spawning, while flatfishes were more abundant in the summer. Fish species composition was most affected by distance from shore (as a proxy for surf zone width), visibility, water temperature, percent cover of combined macroalgae and surfgrass, and breaker wave height, with significant effects detected for distance from shore and breaker height. Fish species that exhibited higher abundance in the winter, including A. argenteus, A. koelzi, and T. semifasciata, were associated with larger waves and wider surf zones. Our results highlight the influence of seasonal variation in environmental conditions on fish communities in the dynamic, coastal surf zone ecosystem, with potential management implications for several highly abundant species targeted by recreational fisheries.
高度动态的沙滩和冲浪带生态系统位于海陆界面,是人类最频繁使用的海岸带之一(如娱乐、捕鱼、旅游)。冲浪区也是鱼类的重要栖息地;然而,由于对这种动态环境进行采样的挑战,对冲浪区鱼类组合的结构因素的研究相对不足。为了研究对冲浪区鱼类群落的时间影响,我们从2020年7月至2021年6月在东北太平洋海岸(美国加利福尼亚州)的四个海滩使用带饵的远程水下视频站(BRUVS)评估了鱼类种群的季节性趋势及其与环境条件的关系。我们的研究区域在生产力(由于春季上升流)和波浪气候(响应冬季风暴)方面具有强烈的季节性特征,使其成为评估冲浪区鱼类季节性变化的理想地点。我们发现,冲浪区鱼类组合表现出明显的季节性和地点间的变异性。冬季和春季两种银鲈(Amphistichus argenteus和A. koelzi)和豹鲨(Triakis semifasciata)较为常见,与银鲈产卵相对应,而比目鱼在夏季较为丰富。鱼类种类组成受离岸距离(代表冲浪带宽度)、能见度、水温、大型藻类和水面草组合覆盖百分比和破浪高度的影响最大,其中离岸距离和破浪高度的影响显著。在冬季表现出较高丰度的鱼类,包括A. argenteus、A. koelzi和T. semifasciata,与更大的波浪和更宽的冲浪区有关。我们的研究结果强调了环境条件的季节性变化对动态沿海冲浪带生态系统中鱼类群落的影响,并对休闲渔业针对的几种高度丰富的物种具有潜在的管理意义。
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引用次数: 0
A numerical study of the morphodynamic response of reef islands under spectral waves 谱波作用下岛礁形态动力响应的数值研究
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-07-11 DOI: 10.1016/j.csr.2025.105524
Yu Yao , Yuting Song , Long Chen , Changshen Li
Most existing studies reports that many low-lying reef atoll islands are vulnerable to the sea level rise and increased storminess in the context of global climate change. The positive adjustment of these reef islands to such extreme oceanographic conditions still needs to be further verified. In this study, the open-source XBeach numerical model using its phase-resolving nonhydrostatic module (XB-NH) combined with its morphodynamic module is adopted to investigate the morphodynamic response of reef islands under spectral waves. The model is firstly validated by two published datasets with and without the presence of sandy island located on the reef flat. The model is then applied to examine the effects of a series of incident wave forcing conditions (significant wave height, peak wave period, reef flat water depth) and island initial morphological features (island height, island top width, island beach slope, island location) on the morphodynamic evolution of reef island. Model applications show that two main morphodynamic responses: the elevated reef island crest and the lagoonward migration of the whole island are identified with larger waves and increased water level. One or two of such morphodynamic self-adjustment can be also found for smaller island with steeper beach slope located more closer to the reef edge. These insights highlight the necessity to consider the island morphological features in the coastal management of low-lying reef atoll nations to better resolve their future stability and persistence.
大多数现有研究报告说,在全球气候变化的背景下,许多低洼的珊瑚礁环礁岛屿容易受到海平面上升和风暴增加的影响。这些岛礁是否对如此极端的海洋条件作出了积极的调整,还有待进一步验证。本研究采用开源的XBeach数值模型,利用其相分辨非静力模块(XB-NH)及其形态动力学模块,研究波谱下岛礁的形态动力学响应。首先用两组已发表的数据集对模型进行了验证,其中包含和不包含位于礁滩上的沙岛。然后应用该模型研究了一系列入射波强迫条件(有效波高、峰值波周期、礁面水深)和岛屿初始形态特征(岛屿高度、岛屿顶宽、岛屿滩坡、岛屿位置)对礁岛形态动力学演化的影响。模型应用表明,岛礁波峰升高和整个岛屿的泻湖迁移是两种主要的形态动力学响应,波浪变大,水位升高。在离礁缘较近、滩坡较陡的小岛上,也会出现一到两次形态动力学的自我调节。这些见解突出了在低洼珊瑚礁环礁国家的沿海管理中考虑岛屿形态特征以更好地解决其未来稳定性和持久性的必要性。
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引用次数: 0
Characterization of two channels of the Chiloé Inland sea used by aquaculture farming: An observational approach to water exchange chilo<s:1>内海水产养殖用两条渠道的特征:水交换的观测方法
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-07-09 DOI: 10.1016/j.csr.2025.105512
Zeneida Wong , Richard Muñoz , Marcus Sobarzo
This study characterizes the hydrodynamics of the Dalcahue and Yal channels, key aquaculture areas within the Chiloé Inland Sea (CIS). It demonstrates the significant influence of bathymetric constrictions on local circulation patterns, tidal modulation, and biogeochemical variability. Dalcahue exhibits distinct bidirectional residual flows, characterized by intensified central inflows (NW-NE) and reinforced outflows (SE-SW) along the Quinchao coast, driven by channel curvature and bathymetry, with velocities reaching up to 70 cm/s in constrictions. In contrast, Yal shows a weak surface residual layer and persistent northwestward mid-depth flow, indicative of vertical tidal energy variations. Semidiurnal tidal forcing (M2, S2) predominantly drives current variability, explaining 50–75 % of observed fluctuations. A significant presence of the M4 overtide (up to 33 % in C2) highlights non-linear tidal interactions, crucial for understanding tidal asymmetry and net material transport. Weak correlations between sea level and dissolved oxygen suggest that strong tidal currents and mixing in constrictions counteract stratification, ventilating deeper layers. These findings enhance our understanding of physical oceanography in the context of the CIS, providing vital insights for environmental management and aquaculture planning by highlighting the role of constriction-induced hydrodynamics in estuarine systems worldwide.
本研究描述了chilo内海(CIS)内主要水产养殖区Dalcahue和Yal河道的水动力学特征。它证明了水深收缩对局部环流模式、潮汐调制和生物地球化学变异的显著影响。达尔卡休表现出明显的双向残余流,其特征是在通道曲率和水深测量的驱动下,沿昆潮海岸中心流入(NW-NE)增强,流出(SE-SW)增强,收缩时速度可达70厘米/秒。而Yal则表现出微弱的表层残留层和持续的西北中深流,表明垂直潮能的变化。半日潮强迫(M2, S2)主要驱动洋流变率,解释了观测到的波动的50 - 75%。M4溢出的显著存在(在C2中高达33%)突出了非线性潮汐相互作用,这对于理解潮汐不对称性和净物质输送至关重要。海平面和溶解氧之间的弱相关性表明,强烈的潮汐流和收缩的混合抵消了分层,使更深的层通风。这些发现增强了我们在CIS背景下对物理海洋学的理解,通过强调收缩引起的水动力学在全球河口系统中的作用,为环境管理和水产养殖规划提供了重要的见解。
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引用次数: 0
Weakening trend of Bohai Sea cold water mass revealed by a ten-year regional ocean simulation with data assimilation 十年区域海洋模拟资料同化揭示的渤海冷水团减弱趋势
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2025-07-07 DOI: 10.1016/j.csr.2025.105511
Hongliang Yu , Zheen Zhang , Lan Li , Chunxin Yuan , Zhen Gao , Xueen Chen
The high-resolution Oceanic Regional Circulation and Tide Model (ORCTM) with a compatible Ensemble Adjustment Kalman Filter (EAKF) assimilation module is implemented to investigate the general evolution and long-term trend of the Bohai Sea cold water mass (BHSCWM). Through comparison with multiple observational data, it can be proved that the reliability of model results is significantly improved after the data assimilation. The assimilated results from 2011 to 2020 show that the BHSCWM occurs from May to August, and its formation is closely related to the seasonal thermocline at a depth of about 10 m. There is a vertically uniform high-temperature water column in the central bank, which divides the BHSCWM into the south part (SBHSCWM) and the north part (NBHSCWM). It is noteworthy that there is a remarkable warming trend in the BHSCWM core, the warming rate reaches 0.24 °C/yr and 0.15 °C/yr for the SBHSCWM and the NBHSCWM, respectively. Meanwhile, whether in terms of cold water mass affected area or volume, a significant decreasing trend for both the SBHSCWM and the NBHSCWM is revealed by our assimilated results, suggesting that the Bohai Sea may be dramatically impacted in the context of global warming.
利用高分辨率海洋区域环流与潮汐模式(ORCTM)和兼容的集合平差卡尔曼滤波(EAKF)同化模块,研究了渤海冷水团(BHSCWM)的一般演变和长期趋势。通过与多个观测资料的对比,可以证明同化后的模型结果的可靠性得到了显著提高。2011 - 2020年同化结果表明,BHSCWM发生在5 - 8月,其形成与10 m左右深度的季节性温跃层密切相关。中央银行内存在垂直均匀的高温水柱,将BHSCWM分为南段(shbhscwm)和北段(NBHSCWM)。值得注意的是,BHSCWM核心增温趋势明显,shbhscwm和NBHSCWM核心增温速率分别达到0.24°C/yr和0.15°C/yr。与此同时,同化结果显示,无论是从影响面积还是从影响体积来看,渤海冷水质量都有显著减少的趋势,表明全球变暖对渤海冷水质量的影响可能很大。
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引用次数: 0
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Continental Shelf Research
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