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Bottom depth carving the pelagic spatial organisation in large marine ecosystem: The case of North West Africa
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2024-11-27 DOI: 10.1016/j.csr.2024.105372
Anne Mouget , Patrice Brehmer , Mohamed Ahmed Jeyid , Yannick Perrot , Ndague Diogoul , Momodou Sidibeh , Kamel Mamza , Anthony Acou , Abdoulaye Sarré
This study aimed to examine the spatial organization of pelagic communities within the water column along a horizontal gradient extending from the coast to the offshore area, categorized into three zones: inshore, offshore, and transition. Using fisheries acoustics, a total of 29 000 nautical miles of acoustic transects collected during 14 annual standardized surveys were analyzed using two complementary acoustic methods: (i) extraction of sound scattering layers (SSL) and (ii) echointegration (EI) across the entire water column, both horizontally and vertically averaged. The results revealed significant differences between the three bathymetric areas based on SSL and EI descriptors, with micro-nektonic communities in the transition area exhibiting intermediate characteristics between those in the inshore and offshore areas. The relative abundance of micro-nektonic communities decreased from shallow coastal areas to deep offshore areas, with a mean Sv from echointegration of −66.43, −74.39 and −73.65 dB for inshore, transition and offshore, respectively. The inshore area is different from the transition and offshore areas, which is confirmed by diel vertical migration (DVM) analyze through vertical profiles. All areas exhibited classic DVM type I; however, offshore and transition areas also presented unexpected DVMs of type II, i.e., organisms descend deeper during the night, displaying distinct vertical profiles compared to the inshore area. This suggests that the functional and specific composition of pelagic micro-nektonic communities differed between inshore and offshore areas, indicating that organisms adjust their responses to their environment. Over two decades, the three bathymetric areas showed a significant increase in pelagic relative biomass and variation in SSL spatial structure. The number of SSLs significantly increase, from 0.97 to 1.05 inshore, from 1.75 to 2.25 in the transition area and from 2.2 to 2.7 offshore. Nevertheless, micro-nektonic communities reacted differently to interannual changes depending on the bathymetric areas, such as the minimal depth of the shallowest SSL. Fluctuations in SSL descriptors were highlighted over the study period, which may be related to multi-decadal oscillations in the Atlantic Ocean.
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引用次数: 0
Environmental control of Arctic marine zooplankton near a large archipelago during the summer season 夏季大型群岛附近北极海洋浮游动物的环境控制
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2024-11-23 DOI: 10.1016/j.csr.2024.105363
Vladimir G. Dvoretsky, Denis V. Moiseev, Marina P. Venger, Anastasya V. Vashchenko, Veronika V. Vodopianova
In order to assess the impact of environmental conditions on marine zooplankton, we conducted a survey around Novaya Zemlya (NZ), a large archipelago located within the Arctic Ocean, during the summertime of 2022. Observations were made by employing net hauls that spanned the entire water column. Through the use of cluster analysis, we ascertained the existence of two unique assemblages inhabiting the Barents and Kara seas. The highest zooplankton abundance, biomass, and diversity were observed at the intersection of the warm Atlantic Water and the comparatively colder Barents Sea Water along the western coast of NZ. Copepods were the predominant species within the zooplankton population in both regions, registering similar numbers, while other groups were noticeably more numerous in the Barents Sea. The distribution of different plankton groups predominantly correlated with the current systems encircling NZ. The inshore waters proximate to the eastern segment of NZ were influenced by the presence of cold currents, while the western part was subjected to the effects of warmer currents. A strong association was observed between zooplankton and microbial variables, such as the abundance and biomass of prokaryoto- and virioplankton. Redundancy analysis indicated close interactions within the plankton ecosystems of the region. These findings may be valuable for assessing the potential impacts of recent climatic perturbations in the Arctic and establishing a baseline for studying Arctic plankton communities in coastal ecosystems.
为了评估环境条件对海洋浮游动物的影响,我们于 2022 年夏季在位于北冰洋的大群岛新亚泽姆利亚(NZ)周围进行了一次调查。观测采用的是横跨整个水体的拖网。通过聚类分析,我们确定巴伦支海和喀拉海存在两个独特的浮游动物群。在新西兰西海岸沿岸温暖的大西洋海水和相对较冷的巴伦支海海水交汇处,浮游动物的丰度、生物量和多样性最高。桡足类是这两个区域浮游动物群中的主要物种,数量相近,而巴伦支海的其他种类浮游动物明显更多。不同浮游生物群的分布主要与环绕新西兰的洋流系统有关。靠近新西兰东部的近岸水域受到寒流的影响,而西部则受到暖流的影响。浮游动物与微生物变量(如原核生物和病毒浮游生物的丰度和生物量)之间存在密切联系。冗余分析表明,该地区浮游生物生态系统内部存在密切的相互作用。这些发现可能对评估北极地区近期气候扰动的潜在影响以及为研究沿海生态系统中的北极浮游生物群落建立基线很有价值。
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引用次数: 0
Multiscale sea level variability on the western Bay of Bengal: A study using tide gauge and satellite observations 孟加拉湾西部的多尺度海平面变化:利用验潮仪和卫星观测数据进行的研究
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2024-11-16 DOI: 10.1016/j.csr.2024.105361
Arkaprava Ray , Sourav Sil , Samiran Mandal
The study examines the tidal variability and intraseasonal oscillations (ISOs) of sea level using tide gauge observations collected during the year 2014 at four stations: Gardenreach, Paradeep, Kakinada, and Ennore along the western Bay of Bengal (BoB). In the first part, the tidal analysis of sea level data shows the dominance of M2 tides followed by S2, N2, K1, and O1 at all the stations. The tides are usually semidiurnal in nature over BoB, represented through the form factor, which is maximum over Ennore (0.21) and minimum over Gardenreach (0.10). The tidal amplitudes increase gradually northward along the western BoB due to interaction with the shallow continental shelf. The topography and coastal geometry also impact the shallow-water constituents (M4 and MS4) significantly at all the locations. Another noteworthy finding is the higher amplitude of M2 tide during the post-monsoon seasons because of the higher stratification of the water column. In the second part, the presence of different non-tidal signals from the residual sea level and altimetry gridded data are studied as well. The correlation coefficient between Sea Level Anomaly (SLA) data from altimetry and the Tide Gauge data are as high as 0.94, 0.91, and 0.90 at Paradeep, Kakinada and Ennore, respectively. The spectral analysis ensures the dominance of the signals with periodicity of 20–60 days in the BoB, which is probably caused due to the monsoon ISOs and Madden Julian Oscillations. The 10–20 days oscillations are also observed with significant amplitudes primarily at Gardenreach which attributes to the Quasi-Biweekly Oscillations. The signature of seasonally varying coastally trapped Kelvin Waves is also identified on the western BoB from both the satellite and Tide Gauge data. The strength of the intraseasonal variability significantly increases during negative Indian Ocean Dipole years with respect to the positive years. The study identified the usefulness of the sea level observation to monitor the multiscale variation within the tides to the interannual scales along the Indian coast.
本研究利用 2014 年在四个站点收集的验潮仪观测数据,研究了海平面的潮汐变化和季内振荡 (ISOs):Gardenreach、Paradeep、Kakinada 和 Ennore 四个站点。在第一部分,海平面数据的潮汐分析表明,所有站点的潮汐都以 M2 潮汐为主,其次是 S2、N2、K1 和 O1。波罗的海潮汐通常是半周期性的,通过形式因子可以看出,恩诺尔潮汐最大(0.21),加登里奇潮汐最小(0.10)。由于与浅大陆架的相互作用,潮汐振幅沿 BoB 西部向北逐渐增大。地形和沿岸几何形状对所有地点的浅水成分(M4 和 MS4)也有很大影响。另一个值得注意的发现是,在季风后季节,由于水体分层程度较高,M2 潮汐的振幅较大。第二部分还研究了残余海平面和测高网格数据中存在的不同非潮汐信号。在 Paradeep、Kakinada 和 Ennore,测高法海平面异常(SLA)数据与验潮仪数据的相关系数分别高达 0.94、0.91 和 0.90。频谱分析表明,在 BoB 中,周期为 20-60 天的信号占主导地位,这可能是季风 ISO 和马登-朱利安振荡造成的。此外,还观测到 10-20 天的振荡,振幅很大,主要发生在加登里奇,这是准双周振荡造成的。从卫星和验潮仪数据中,还可以发现博白西部存在季节性变化的海岸滞留开尔文波。在印度洋偶极子负年与正年相比,季节内变化的强度明显增加。研究表明,海平面观测有助于监测印度沿岸潮汐的多尺度变化和年际尺度变化。
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引用次数: 0
Satellite-based evidence of upwelling separation off NW Iberia 伊比利亚西北部近海上升流分离的卫星证据
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2024-11-15 DOI: 10.1016/j.csr.2024.105356
Pedro R. Nunes , Vanda Brotas , Rita Nolasco , Jesus Dubert , Paulo B. Oliveira
A high-resolution image sequence of sea surface temperature (SST) and Chlorophyll-a (Chl-a), together with numerical model solutions, is used to study the spatio-temporal variability of the two variables under intermittent upwelling-favourable winds. It is shown that the evolution of the cross-shore SST and Chl-a profiles over the shelf is linked to the intensity, duration and temporal separation between the wind events. The model's realistic representation of the cross-shore SST supports the interpretation that the observed variability is governed, in the inner-shelf, by the offshore separation of upwelling divergence and, over the mid-shelf, by offshore Ekman transport and mesoscale circulation. The observation of an alongshore low SST/low Chl-a band, bounded by the 30 m and 50 m isobaths, for the days of maximum wind stress, matching the model's solution for the outcrop of colder subsurface waters, constitute a satellite-based evidence of upwelling separation from the coast. The results are in close agreement with previous works on upwelling in shallow waters, straight coastline and gentle slope, but were not yet reported in the study area off NW Portugal. This evidence prompts for the need to use high-resolution (<1 km) numerical models/imagery to properly assess the inner-shelf circulation in the region, and the effects on the marine ecosystem, namely the offshore transport of marine organisms or pollutants.
利用高分辨率海表温度(SST)和叶绿素 a(Chl-a)图像序列以及数值模式解,研究了在间歇性上升流顺风条件下这两个变量的时空变化。结果表明,陆架上的跨岸 SST 和 Chl-a 剖面的演变与风事件的强度、持续时间和时间间隔有关。该模式对跨岸海温的逼真再现支持了这样一种解释,即在内侧陆架,观测到的变化受上升流离岸辐散的影响,而在陆架中部,则受离岸埃克曼输送和中尺度环流的影响。在风压最大的日子里,沿岸观测到以 30 米和 50 米等深线为界的低海温/低 Chl-a 带,这与模型对较冷的表层下水域的解法相吻合,构成了上升流从海岸分离的卫星证据。这些结果与之前关于浅水、直线海岸线和缓坡上升流的研究结果非常吻合,但在葡萄牙西北部近海的研究区域尚未见报道。这些证据表明,需要使用高分辨率(1 千米)数值模型/图像来正确评估该区域的内 陆环流以及对海洋生态系统的影响,即海洋生物或污染物的近海迁移。
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引用次数: 0
Assessing the conservation status of Mediterranean coastal ponds: Checklist, ecological and functional diversity of diatom communities 评估地中海沿岸池塘的保护状况:硅藻群落的清单、生态和功能多样性
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2024-11-14 DOI: 10.1016/j.csr.2024.105359
Davide Taurozzi , Massimiliano Scalici
Coastal ponds are peculiar and threatened habitats, considered biodiversity hotspots. In many ecosystems ponds can be a valuable resource for the conservation of freshwater biodiversity. The Castelporziano Presidential Estate is a Mediterranean protected area hosting numerous ponds which are suffering severe droughts and a general decline in number and hydroperiod length. Hydroperiod changes can be particularly relevant for biodiversity inhabiting ponds, in particular diatom communities. Here, for the first time, we evaluate the conservation status of Mediterranean ponds inside the Castelporziano Reserve. The aims of this research are to i) investigate the influence of environmental variables on diatom communities of ponds; (ii) analyse diatom community structure in function of species richness and competitive interactions; (iii) highlight the potential and effectiveness of diatom ecological guilds in supporting the interpretation of the ecological status of threatened small waterbodies. Overall, 122 diatom taxa in the 29 ponds were described. Nitzschia (18 species) was the most species-rich genus, followed by Gomphonema (14) and Navicula (13). 17 species were included in the Red List of endangered species. Intra-pond distance and anthropogenic impacts didn't influence diatom assemblages. On the contrary, diatom communities were influenced by altitude and the distance from the sea. Furthermore, temporary ponds showed the lowest values for Shannon, evenness and Simpson indexes Considering Beta-diversity, both Bray-Curtis and Jaccard dissimilarity matrices highlighted a large dissimilarity between sampling sites. Inter-variability between sites and intra-variability within the sites resulted both very low. Our results highlight that diatom species are not influenced by hydroperiod length. Moreover, a structured diatom community emerged, where segregation processes predominating over aggregation ones. Finally, the average water quality of the ponds, calculated using the EPI-D index, was described as “good”. This study represents the most complete checklist of diatom communities inside coastal ponds of Castelporziano, providing valuable insights into the effects of natural and anthropogenic influences on ponds conservation and management activities. However, spatial-temporal changes and anthropogenic impacts should be deeply investigated.
沿海池塘是一种奇特且濒临灭绝的栖息地,被视为生物多样性的热点。在许多生态系统中,池塘都是保护淡水生物多样性的宝贵资源。卡斯特波齐亚诺总统庄园是一个地中海保护区,这里有许多池塘,但由于严重干旱,池塘数量和水文周期长度普遍下降。水文周期的变化对栖息在池塘中的生物多样性尤其重要,特别是硅藻群落。在此,我们首次对卡斯特波齐亚诺保护区内地中海池塘的保护状况进行了评估。这项研究的目的是:(i) 调查环境变量对池塘硅藻群落的影响;(ii) 分析硅藻群落结构对物种丰富度和竞争性相互作用的作用;(iii) 强调硅藻生态区系在支持解释受威胁小水体生态状况方面的潜力和有效性。29 个池塘中共有 122 个硅藻分类群被描述。Nitzschia(18 种)是物种最丰富的属,其次是 Gomphonema(14 种)和 Navicula(13 种)。有 17 个物种被列入濒危物种红色名录。塘内距离和人为影响对硅藻群落没有影响。相反,硅藻群落受到海拔高度和离海距离的影响。考虑到 Beta 多样性,Bray-Curtis 和 Jaccard 差异矩阵都突出显示了采样点之间的巨大差异。取样点之间的差异和取样点内部的差异都非常小。我们的研究结果表明,硅藻物种不受水文周期长度的影响。此外,硅藻群落出现了结构化现象,其中分离过程比聚集过程占主导地位。最后,根据 EPI-D 指数计算,池塘的平均水质为 "良好"。这项研究是卡斯特波齐亚诺沿海池塘硅藻群落最完整的清单,为了解自然和人为因素对池塘保护和管理活动的影响提供了宝贵的信息。然而,时空变化和人为影响还需要深入研究。
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引用次数: 0
A century of tidal evolution around the Panama Canal 巴拿马运河周边一个世纪的潮汐演变
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2024-11-10 DOI: 10.1016/j.csr.2024.105357
Haidong Pan , Min Gan , Tengfei Xu , Zexun Wei
As one of the most vital passageways worldwide, the Panama Canal plays essential roles in global trade and maritime logistics. Sea levels around the Panama Canal are dominated by ocean tides but local tidal evolution is still unexplored to date, which motivates present study. Two secular tide gauges longer than 110 years (Cristobal and Balboa) around the Panama Canal are analyzed to explore multi-time scale tidal variability. It is found that observed nodal modulations of major constituents are generally consistent with the equilibrium tidal theory. M4 and Mf nodal modulations notably deviate from the theory possibly due to non-linear processes. Long-term trends exist in main semi-diurnal tides, while main diurnal tides do not have significant secular trends. It is worth mentioning that M4 and MS4 amplitudes at Cristobal have halved in the past century. Moreover, tidal parameters of major constituents at Cristobal and Balboa show abnormal mutations in 1908, 1990–1998, and 2013–2018. As a result of changing tides, tidal asymmetries at Cristobal are significantly weakened while the number of high tides per year is notably decreased. Tides at Balboa are almost symmetric. Tidal regimes at Cristobal can periodically shift between mixed diurnal tides and mixed semi-diurnal tides following the 18.61-year nodal cycle. However, such regime shift has disappeared since 1997 due to secular negative trends in M2 amplitudes. In general, the findings of this study can be helpful for ships navigating in the Panama Canal.
作为全球最重要的通道之一,巴拿马运河在全球贸易和海运物流中发挥着至关重要的作用。巴拿马运河附近的海平面主要受海洋潮汐的影响,但当地潮汐的演变至今仍未得到探索,这也是本研究的动机所在。本研究分析了巴拿马运河周围两个超过 110 年的常规验潮仪(克里斯托巴尔验潮仪和巴尔博亚验潮仪),以探索多时间尺度的潮汐变化。研究发现,观测到的主要成分的节点模态与平衡潮汐理论基本一致。M4 和 Mf 节点调制明显偏离理论,可能是由于非线性过程造成的。主半日潮存在长期趋势,而主日潮没有明显的世俗趋势。值得一提的是,克里斯托巴尔的 M4 和 MS4 振幅在上个世纪减小了一半。此外,克里斯托巴尔和巴尔博亚主要成分的潮汐参数在 1908 年、1990-1998 年和 2013-2018 年出现异常突变。由于潮汐的变化,克里斯托巴尔的潮汐不对称性明显减弱,同时每年的高潮次数显著减少。巴尔博亚的潮汐几乎是对称的。克里斯托巴尔的潮汐系统会根据 18.61 年的交点周期在混合日潮和混合半日潮之间周期性地转换。然而,自 1997 年以来,由于 M2 振幅的长期负值趋势,这种潮汐机制的转变已经消失。总之,这项研究的结果对在巴拿马运河航行的船只很有帮助。
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引用次数: 0
Flow characterization and turbulence in the eastern section of the Strait of Magellan, Southern Chile 智利南部麦哲伦海峡东段的水流特征和湍流情况
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2024-11-09 DOI: 10.1016/j.csr.2024.105344
Leandro Suarez , Maricarmen Guerra , Megan E. Williams , Cristián Escauriaza , Iossif Lozovatsky , Ronald Coppersmith , Harindra Joseph S. Fernando
The Strait of Magellan connects the Pacific and Atlantic oceans in South America’s southern region, and it has been recognized for centuries as an important transoceanic navigation route as well as a unique marine environment with a rich ecological diversity. Evaluations of the impact of human activities in the channel and multiple potential future developments require a better understanding of the physical environment to design sustainable strategies aimed at preserving these characteristics. In this investigation, we study the flow near the Atlantic inlet of the Strait where the dynamics is characterized by the interactions of the tide propagation within two narrows, which are the predominant features of the channel morphology. Tides amplified by the Patagonian shelf generate strong currents through these narrows and control the exchange between the Atlantic and central regions of the Strait. We employ bottom-mounted and vessel-mounted Acoustic Doppler Current Profilers (ADCPs) with tide gauges to analyze the mean flow, tidal propagation, and turbulence, complementing the data with previous available measurements. The analysis reveals residual flows directed toward ebb flow at the channel center and flood near the edges, showing a significant spring-neap variation. Turbulence statistics in the second narrows exhibit a significant variability between ebb and flood, with a balance between production and dissipation observed only during ebb phases.
麦哲伦海峡位于南美洲南部地区,连接太平洋和大西洋,数百年来一直被认为是重要的跨洋航道,也是具有丰富生态多样性的独特海洋环境。要评估人类活动对航道的影响以及未来的多种潜在发展,就必须更好地了解物理环境,以设计旨在保护这些特征的可持续战略。在这项调查中,我们研究了海峡大西洋入口附近的水流,其动态特征是潮汐在两个狭长地带内传播的相互作用,这是海峡形态的主要特征。经巴塔哥尼亚大陆架放大的潮汐通过这些狭窄处产生强大的水流,控制着海峡大西洋和中部地区之间的水流交换。我们利用安装在海底和船上的声学多普勒海流剖面仪(ADCP)和验潮仪来分析平均流、潮汐传播和湍流,并将这些数据与之前的测量数据进行补充。分析结果显示,残余水流在水道中心为退潮流,在边缘为洪峰流,显示出显著的春-夏变化。第二窄河道的湍流统计在退潮和洪水之间表现出明显的变化,只有在退潮阶段才能观察到产生和消散之间的平衡。
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引用次数: 0
Machine learning reveals biological activities as the dominant factor in controlling deoxygenation in the South Yellow Sea 机器学习揭示生物活动是控制南黄海脱氧的主导因素
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2024-11-07 DOI: 10.1016/j.csr.2024.105348
Qingyi Liu , Chunli Liu , Qicheng Meng , Bei Su , Haijun Ye , Bingzhang Chen , Wei Li , Xinyu Cao , Wenlong Nie , Nina Ma
Dissolved oxygen (DO) is a crucial element for both biotic and abiotic processes in marine ecosystems, but has declined globally in recent decades. Therefore, there is an urgent need for solid large-scale and continuous estimation of DO concentration in vital ecosystems, such as coastal areas. A random forest (RF) model for DO in South Yellow Sea (SYS) was developed by integrating satellite data and simulation data during 2011–2019. The root mean squared error (RMSE) for the training and test sets were 0.514 mg/L and 0.732 mg/L, respectively. Spatiotemporal distributions of DO of multiple layers in the study area during 2011–2019 were very well reproduced by the RF model and showed a slight decline trend in most SYS areas, while more intense decline occurred in the deep central SYS. The analysis of the mechanisms of DO decline in the South Yellow Sea cold water mass (SYSCWM), located in the deep central SYS, indicates that the deoxygenation here is largely due to biological activities. This finding may have implications for studies on drivers of deoxygenation in coastal areas. Furthermore, integrating satellite data with machine learning models can offer a powerful approach to capturing the continuous spatiotemporal characteristics of ocean parameters over large spatial scales.
溶解氧(DO)是海洋生态系统中生物和非生物过程的关键元素,但近几十年来,全球溶解氧浓度都在下降。因此,迫切需要对沿海地区等重要生态系统的溶解氧浓度进行大规模、连续的可靠估算。通过整合 2011-2019 年期间的卫星数据和模拟数据,建立了南黄海溶解氧随机森林(RF)模型。训练集和测试集的均方根误差(RMSE)分别为 0.514 mg/L 和 0.732 mg/L。射频模型很好地再现了 2011-2019 年期间研究区多层溶解氧的时空分布,大部分 SYS 区域的溶解氧呈轻微下降趋势,而中部深层 SYS 区域的溶解氧下降更为剧烈。对位于 SYS 中部深层的南黄海冷水团溶解氧下降机理的分析表明,这里的脱氧主要是由生物活动引起的。这一发现可能会对沿岸地区脱氧驱动因素的研究产生影响。此外,将卫星数据与机器学习模型相结合,可以为捕捉大空间尺度上海洋参数的连续时空特征提供一种强有力的方法。
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引用次数: 0
Observations and generation of internal waves in the Strait of Sicily 西西里海峡内波的观测与生成
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2024-11-07 DOI: 10.1016/j.csr.2024.105349
Francesco Bignami , Werner Alpers , Davide Cavaliere , Giovanni La Forgia , Gianmaria Sannino
Oceanic internal solitary waves (ISWs) can be generated by several mechanisms, among which by tidal flow over shallow bathymetry, atmospheric forcing, unbalanced sub-mesoscale flow without external forcing and rapid displacements of the sharp fronts separating e.g. cold ocean water masses or river plumes from the ambient seawater. In this paper, we analyze synthetic aperture radar (SAR) images acquired by the Sentinel-1 satellites over the Adventure Bank area, located on the western side of the Strait of Sicily in the years 2018–2021 showing numerous radar signatures of ISWs. This is the first time that massive presence of ISWs is reported in this area of the Mediterranean Sea. The internal wave field, observed primarily in the months from May to September, is very heterogeneous, with wavelengths ranging from a few hundred meters to a few kilometers, wave front lengths from a few km to about 40 km, and propagating in almost any direction. This suggests that the internal waves detected in the SAR images are generated by a variety of mechanisms and not by a specific one. Although in general tidal currents are weak in the Mediterranean Sea, the sum of the tidal flow and the Atlantic-Ionian Stream current can attain values up to 0.3 m s−1 such that ISW generation by interaction with shallow underwater bottom topography becomes possible. Furthermore, cold filaments and sub-mesoscale cyclonic eddies generated by upwelling at the south coast of Sicily, feature sharp and rapidly moving fronts, from which ISWs may originate. Theoretical evidence for these two types of ISW generation mechanisms is provided by model results obtained from the 1/48° resolution ENEA model and the 100 m resolution Delft3D model.
海洋内孤波(ISWs)可由多种机制产生,其中包括浅水深潮汐流、大气强迫、无外部强迫的不平衡次中尺度流以及将冷水团或河流羽流等从环境海水中分离出来的锋面的快速位移。在本文中,我们分析了 Sentinel-1 号卫星在 2018-2021 年期间在位于西西里海峡西侧的冒险滩地区获取的合成孔径雷达(SAR)图像,这些图像显示了大量 ISW 的雷达特征。这是首次报道在地中海的这一区域存在大规模的 ISWs。主要在 5 月至 9 月观测到的内波场非常不均匀,波长从几百米到几千米不等,波前长度从几千米到约 40 千米不等,传播方向几乎不限。这表明合成孔径雷达图像中探测到的内波是由多种机制而非特定机制产生的。虽然地中海的潮汐流一般较弱,但潮汐流和大西洋-爱奥尼亚海流的总和可达到 0.3 米/秒-1,因此通过与水下浅层地形相互作用产生内波是可能的。此外,西西里岛南岸上升流产生的冷丝和亚中尺度气旋漩涡具有锋利和快速移动的特点,ISW 可能就源于此。1/48° 分辨率的 ENEA 模型和 100 米分辨率的 Delft3D 模型得出的结果为这两种 ISW 生成机制提供了理论证据。
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引用次数: 0
Echoes of a Cold War 冷战的回声
IF 2.1 3区 地球科学 Q2 OCEANOGRAPHY Pub Date : 2024-11-06 DOI: 10.1016/j.csr.2024.105347
Valeriy Y. Rusakov , Ruslan A. Lukmanov , Bulat R. Soktoev , Andrey Y. Mishan'kin
The Kara Sea was an area of radionuclide contamination as a result of nuclear weapons testing, since it is located in close proximity to the nuclear test site on the Novaya Zemlya archipelago. The vertical distribution of 137Cs and 210Pb in 15 sediment cores from the sea made it possible to reconstruct the chronology of 137Cs entry into marine sediments. The reconstruction was based on the age-depth model RUS2023 (Rusakov et al., 2024) for 210Pbex, taking into account the grain-size composition and sorption capacity of sediments. Our study showed that higher 137Cs concentrations in sediments of the Novaya Zemlya Trough correspond to the time of active nuclear weapons testing in 1961–63 (about 9.0 ± 1.6 Bq kg‒1), as well as in estuarine sediments of the Yenisei Bay in 1986 (85.2 ± 3.2 Bq kg‒1). The abnormally high flux in 1980s represents the superposition of 137Cs fluxes as a result of global fallout (Chernobyl trace) and as a result of the release of radionuclide from regional source located in the Yenisei River catchment. Both of these events are associated with increased the sedimentation and mass accumulation rates of marine sediments. In 1961‒63, this was a consequence of the release of sediment into the atmosphere due to nuclear explosions, and in the 1980s, as a result of an increase in sediment supply with river runoff. Currently, against the backdrop of a decrease in sediment fluxes into the sea, Novaya Zemlya and Yenisei River remain the main sources of 137Cs supply to marine sediments. Background values for recent sediments in the Kara Sea are <2.0 Bq kg‒1.
卡拉海是核武器试验造成放射性核素污染的地区,因为它毗邻新泽姆利亚群岛上的核试验场。根据该海域 15 个沉积岩芯中 137Cs 和 210Pb 的垂直分布情况,可以重建 137Cs 进入海洋沉积物的时间顺序。重建是基于 210Pbex 的年龄深度模型 RUS2023(Rusakov 等人,2024 年),并考虑了沉积物的粒度组成和吸附能力。我们的研究表明,新泽姆利亚海槽沉积物中较高的 137Cs 浓度与 1961-63 年核武器试验活跃时期(约 9.0 ± 1.6 Bq kg-1)以及 1986 年叶尼塞湾河口沉积物中较高的 137Cs 浓度(85.2 ± 3.2 Bq kg-1)相对应。20 世纪 80 年代异常高的通量是 137Cs 通量的叠加,它是全球尘降(切尔诺贝利痕量)的结果,也是位于叶尼塞河流域的区域源释放放射性核素的结果。这两个事件都与海洋沉积物的沉积和堆积速度加快有关。1961-63 年,这是核爆炸导致沉积物释放到大气中的结果;20 世纪 80 年代,则是河流径流导致沉积物供应增加的结果。目前,在入海沉积物通量减少的背景下,新谢姆利亚和叶尼塞河仍然是海洋沉积物中 137Cs 的主要供应来源。喀拉海近期沉积物的背景值为 2.0 Bq kg-1。
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Continental Shelf Research
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