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Three-dimensional spatiotemporal simulation of tritium discharge from Fukushima 福岛氚排放的三维时空模拟
IF 2.9 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2025-11-03 DOI: 10.1016/j.ocemod.2025.102652
Yi Liu , Zhen-Zhong Hu , Robert H. Richmond , Jian-Min Zhang , Chang Zhao , Shengli Chen
The ALPS treated water has been discharged into the Pacific Ocean since August 2023. This study investigates this discharge using a newly developed three-dimensional dispersion model that incorporates migration, diffusion, and decay processes of radionuclides. A simulation over ten years is conducted using reanalyzed oceanographic data. The results indicate that tritium released from Fukushima primarily disperses eastward along the 35°N latitude line. In later stages, local concentration peaks emerge in the northeastern Pacific, exceeding those in the northwest Pacific. For the vertical distribution, the tritium is generally reduced greatly with depth, but displays maximum values at subsurface layer (∼50m) in some regions. The concentration reaches a steady state over time, defined as the characteristic concentration, whose spatial distribution and attainment time are detailed. For major fishing grounds in the Pacific Ocean, the Hokkaido area shows the highest tritium levels, followed by Hawaii, California, Zhoushan, the Korean Peninsula, Mexico, the Philippines, Alaska, and Peru in descending order. Critically, simulated tritium concentrations in most North Pacific regions (∼0.01 Bq/m3) remain orders of magnitude below natural background levels (∼50 Bq/m3). This research elucidates three-dimensional radionuclide dispersion mechanisms in global oceans, providing a quantitative methodology for future marine emergency response and contributing to long-term marine conservation efforts.
自2023年8月以来,阿尔卑斯山处理过的水被排放到太平洋。本研究使用一个新开发的三维色散模型来研究这种放电,该模型包含了放射性核素的迁移、扩散和衰变过程。利用重新分析的海洋学资料进行了为期十年的模拟。结果表明,福岛核泄漏的氚主要沿北纬35°向东扩散。在后期,局部浓度高峰出现在东北太平洋,超过西北太平洋。在垂直分布上,氚一般随深度的增加而大幅度减少,但在某些区域在近地表(~ 50m)处达到最大值。浓度随时间达到稳定状态,定义为特征浓度,详细描述了其空间分布和达到时间。在太平洋的主要渔场中,氚含量最高的是北海道地区,依次为夏威夷、加利福尼亚、舟山、朝鲜半岛、墨西哥、菲律宾、阿拉斯加、秘鲁。重要的是,大多数北太平洋地区的模拟氚浓度(~ 0.01 Bq/m3)仍然比自然背景水平(~ 50 Bq/m3)低几个数量级。这项研究阐明了全球海洋中的三维放射性核素扩散机制,为未来的海洋应急反应提供了定量方法,并有助于长期的海洋保护工作。
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引用次数: 0
Investigating the impact of meteorological factors on sea-level variability in the northwestern Arabian gulf: A case study using deep learning and advanced statistical models for enhanced forecasting 调查气象因素对阿拉伯湾西北部海平面变化的影响:使用深度学习和高级统计模型增强预报的案例研究
IF 2.9 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2025-11-02 DOI: 10.1016/j.ocemod.2025.102648
Abather J.B. Alhallaf , Javier Vilcáez , Ye Liang
This study evaluates how incorporating meteorological variables affects the predictive accuracy of sea-level variability (SLV) models in the northwestern Arabian Gulf, utilizing SARIMAX, LSTM, and CNN&LSTM models. The analysis indicates that the total monthly meteorological contributions, as a proportion of overall tidal influences on SLV, reach their peak in summer, with July and August exhibiting the highest total monthly weights, aligning with previous studies. Air Temperature (AT) is the principal parameter influencing SLV, accounting for a maximum of 28.35% in August, highlighting climate change's persistence on sea level. The models consistently identify Atmospheric Pressure (AP) as a consistent contributor with a minor negative effect; Wind Speed (WS), Wind Direction (WD), and Gust Speed (GS) exhibit mixed effects depending on the month. The LSTM and CNN&LSTM models also indicate that some factors inversely affect sea-level changes. This study highlights the significance of integrating metrological factors into sea-level forecasting models in the northwestern Arabian Gulf to enhance flood prediction. It has potential applications in disaster preparedness and the execution of coastal flooding mitigation strategies.
本研究利用SARIMAX、LSTM和CNN&;LSTM模型,评估了纳入气象变量如何影响阿拉伯湾西北部海平面变率(SLV)模型的预测精度。分析表明,月气象总贡献占总潮汐影响SLV的比例在夏季达到峰值,其中7月和8月的月总权重最高,与前人的研究结果一致。气温(AT)是影响SLV的主要参数,在8月份最大占28.35%,突出了气候变化对海平面的持续性。这些模式一致地将大气压力(AP)确定为具有轻微负面影响的一致贡献者;风速(WS)、风向(WD)和阵风速度(GS)在不同月份表现出混合效应。LSTM和CNN&;LSTM模式也表明一些因子对海平面变化有负相关影响。本研究强调了将气象因子整合到阿拉伯湾西北部海平面预报模型中对加强洪水预报的意义。它在备灾和执行沿海洪灾减灾战略方面具有潜在的应用前景。
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引用次数: 0
Local effect of a submesoscale parameterization scheme and its remote influences on large-scale circulation in the Northwest Pacific 一个亚中尺度参数化方案的局地效应及其对西北太平洋大尺度环流的远程影响
IF 2.9 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2025-10-31 DOI: 10.1016/j.ocemod.2025.102650
Ziyi Zhang , Bo An , Zhiwei Zhang , Yuyang Guo , Jinchao Zhang , Zhe Feng , Yongqiang Yu
Submesoscale processes play important roles in vertical heat and mass transport, modulating mesoscale eddies and the energy cycle; thus a parameterization is essential for most ocean models due to submesoscale’s spatial scales (∼100 m–10 km). This study describes the impact of the submesoscale parameterization scheme by Zhang et al. (2023; Zhang23) in a regional eddy-resolving ocean model in the North Pacific. Compared with the numerical experiment without the scheme, the simulated winter mixed-layer depth (MLD) bias is reduced by 70 % in the Kuroshio Extension (KE) region and the KE jet shifted southward from 36.5°N to 35.5°N, closer to observations. Surface cold biases at 32°–34°N and subsurface warm biases at 36–40°N are reduced by ∼1 °C and ∼2 °C across four seasons, respectively. The effect of submesoscale vertical buoyancy fluxes (VBF) on winter MLD is debated. While widely shown to promote basin-scale shoaling via restratification, they are also known to cause powerful, localized deepening in regions with strong fronts and air-sea interaction. Focusing on this latter scenario, our study reveals a more detailed mechanism, notably distinguishing between local (direct) and remote (indirect) impacts on circulation in the mixed layer and subsurface. Enhanced submesoscale VBF drives weather-scale MLD deepening and subduction along tilted isopycnals in boreal winter in the most active eddy region, mainly limited to 38°–42°N/140°–150°E, promoting southward subsurface cooling and strengthening ocean memory. This feedback modulates the KE's large-scale circulation by shifting its path southward, reducing downstream heat transport, and promoting stratification and shoaling in the eastern region throughout all seasons. These findings demonstrate the importance of submesoscale parameterization for improving simulations of western boundary current systems and highlight its effects in representing remote and subsurface dynamic processes.
亚中尺度过程在垂直热质输运、调节中尺度涡旋和能量循环中起重要作用;因此,由于亚中尺度的空间尺度(~ 100 m-10 km),对大多数海洋模式来说,参数化是必不可少的。本文描述了Zhang et al. (2023; Zhang23)的亚中尺度参数化方案对北太平洋区域涡旋解析海洋模式的影响。与不采用该方案的数值试验相比,模拟黑潮延伸(KE)地区冬季混合层深度(MLD)偏差减小了70%,KE急流从36.5°N向南移动至35.5°N,与观测值更接近。在32°-34°N的地表冷偏差和36-40°N的地下暖偏差在四个季节中分别减少了~ 1°C和~ 2°C。讨论了亚中尺度垂直浮力通量(VBF)对冬季MLD的影响。虽然它们被广泛证明可以通过再酸化促进盆地尺度的浅滩化,但在锋面强和海气相互作用的地区,它们也会导致强大的局部深化。针对后一种情况,我们的研究揭示了更详细的机制,特别是区分了对混合层和地下环流的局部(直接)和远程(间接)影响。亚中尺度VBF的增强,在最活跃的涡动区(主要局限于38°-42°N/140°-150°E),驱动了北纬冬季天气尺度MLD沿倾斜等平线加深和俯冲,促进了向南的地下冷却,增强了海洋记忆。这种反馈调节了KE的大尺度环流,使其路径南移,减少了下游的热输送,并在整个季节促进了东部地区的分层和浅滩化。这些发现表明了亚中尺度参数化对于改善西部边界流系统模拟的重要性,并突出了其在表征远程和地下动力过程方面的作用。
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引用次数: 0
Surface current detection in regional seas using Lagrangian coherent structures 基于拉格朗日相干结构的区域海洋表面流探测
IF 2.9 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2025-10-31 DOI: 10.1016/j.ocemod.2025.102647
Huy Cong Vu, Binh Quang Nguyen
Eddies play a vital role in the transport of heat, salt, and other materials, as well as in shaping the circulation structure of the ocean. Understanding eddies is therefore essential for elucidating the mechanisms that govern the formation, evolution, and variability of ocean currents. This study aims to analyze the characteristics of ocean currents in the East Vietnam Sea (South China Sea–SCS) by combining two approaches: the Euler method and the Lagrangian Coherent Structures (LCS) method. This integrated approach provides a comprehensive understanding of current dynamics and eddy formation. Using velocity vector images (Euler method), the study identifies the direction, location, and intensity of major ocean currents in the SCS. Meanwhile, the LCS method is applied to detect and delineate the boundaries and sizes of eddies. The ocean current data were obtained from the global HYCOM model on a daily basis throughout 2023. Our findings indicate that: (i) ocean currents in the SCS exhibit a clear seasonal pattern. In winter, the dominant flow moves from north to south along the Vietnamese coast, while in summer, the flow reverses, moving from south to north, with a disruption near 11 °N close to the Vietnamese coast. The current can extend up to 220 km near China, narrowing to 56 km as it approaches Vietnam. (ii) A table summarizing the characteristics of eddies with diameters greater than 100 km is included. The number of eddies is higher during the summer, but larger eddies tend to occur during the winter. In addition to single eddies, the SCS is also home to double and triple eddies.
漩涡在热、盐和其他物质的运输中起着至关重要的作用,也在塑造海洋的环流结构中起着至关重要的作用。因此,了解涡流对于阐明控制洋流形成、演化和变化的机制至关重要。本研究旨在结合欧拉方法和拉格朗日相干结构(LCS)方法分析东越南海(南中国海)洋流特征。这种综合方法提供了对电流动力学和涡流形成的全面理解。利用速度矢量图像(欧拉法),该研究确定了南海主要洋流的方向、位置和强度。同时,利用LCS方法对涡流的边界和大小进行检测和圈定。2023年的海流数据来自全球HYCOM模型的每日数据。我们的研究结果表明:(1)南海洋流表现出明显的季节性模式。冬季主要气流沿越南海岸由北向南移动,夏季主要气流由南向北移动,在靠近越南海岸的11°N附近出现中断。洋流在中国附近可以延伸220公里,在接近越南时缩小到56公里。(ii)附有一个表,概述了直径大于100公里的涡流的特征。涡旋的数量在夏季较高,但较大的涡旋往往发生在冬季。除了单涡旋外,南海还有双涡旋和三涡旋。
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引用次数: 0
The wave-induced heat transport in the global ocean 全球海洋中的波致热输运
IF 2.9 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2025-10-31 DOI: 10.1016/j.ocemod.2025.102649
Rui Li , Kejian Wu , Qingxiang Liu , Jin Liu , Shang-Min Long , Jian Sun , Alexander V. Babanin
The effect of the small-scale ocean surface waves on large-scale ocean climate has been usually neglected. The Stokes drift-induced water transport has the potential to contribute to ocean heat transport and the wave-induced heat transport (WHT) in the global ocean is quantified for the first time in this research. The magnitude of wave-induced water transport is found to be comparable to Ekman transport in the global ocean. Notably, both of the zonal and meridional surface Stokes drift exhibit a strong correlation with the El Niño-Southern Oscillation and Indian Ocean Dipole (IOD). We found that there is an anomalous increase in wave-induced heat transport towards the equator during El Niño events in the Pacific Ocean. Additionally, an increase in eastward WHT appears during eastern-type El Niño events. Moreover, the zonal WHT anomalies co-vary with IOD phases. The large-scale climate modes drive the ocean wave large-scale anomalies, and then the abnormal WHT leads to redistribution of global ocean heat, even exceeding the heat transport induced by Ekman transport.
小尺度海洋表面波对大尺度海洋气候的影响通常被忽视。Stokes漂移引起的水输运具有促进海洋热输运的潜力,本研究首次对全球海洋的波致热输运进行了量化。发现波浪引起的水输运的强度与全球海洋中的埃克曼输运相当。值得注意的是,纬向和经向表面Stokes漂移都与El Niño-Southern涛动和印度洋偶极子(IOD)有很强的相关性。我们发现,在El Niño事件期间,太平洋向赤道的波致热输送异常增加。此外,东部型El Niño事件期间东向WHT增加。此外,纬向WHT异常与IOD相同时变化。大尺度气候模态驱动海浪大尺度异常,WHT异常导致全球海洋热重新分布,甚至超过了Ekman输运引起的热输运。
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引用次数: 0
Internal solitary waves with different density distribution approximation schemes in background shear currents 背景剪切流中不同密度分布近似格式的内孤立波
IF 2.9 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2025-10-30 DOI: 10.1016/j.ocemod.2025.102644
Zhuoyue Li , Haibao Hu , Chen Chen , Zhan Wang , Zhongliang Xie , Peng Du
The density distribution scheme determines the characteristics of internal solitary waves (ISWs). Based on three typical density distributions, ISWs are modeled in two-layer, three-layer, and continuous-density systems, while also considering the effect of background shear currents. ISWs are generated using high-level Green–Naghdi (HLGN) and Dubreil-Jacotin-Long (DJL) theories, which serve as initial conditions for the computational fluid dynamics (CFD) flume. In all systems, linear background shear currents can significantly affect the ISW properties, such as wave profiles, induced velocity, propagation speed, and energy distribution. Positive-vorticity background shear currents pycnocline thinning, whereas negative-vorticity currents result in thickening. The ISW shear strength is evaluated by the average rate of change of horizontal velocity at the pycnocline. In the two-layer system, positive-vorticity currents reduce the ISW shear effect, whereas the opposite occurs with negative-vorticity currents. The conclusions for the three-layer and continuous-density systems are in contrast to those of the two-layer system. This indicates that consideration or neglect of the pycnocline thickness may lead to opposite conclusions regarding the effects of background shear currents on the ISW shear effect. Furthermore, the influence of the nonlinear background shear currents is discussed. For most properties, the effects of nonlinear currents are consistent with those of linear currents, although they are generally weak.
密度分布方案决定了内孤立波的特性。在三种典型密度分布的基础上,分别建立了两层、三层和连续密度系统的isw模型,同时考虑了背景剪切流的影响。isw是利用高阶Green-Naghdi (HLGN)和Dubreil-Jacotin-Long (DJL)理论生成的,它们是计算流体动力学(CFD)水槽的初始条件。在所有系统中,线性背景剪切流都会显著影响ISW特性,如波廓线、感应速度、传播速度和能量分布。正涡度背景切变流导致斜斜变薄,而负涡度背景切变流导致增厚。ISW抗剪强度由斜斜处水平速度的平均变化率来计算。在两层体系中,正涡度流降低了ISW剪切效应,而负涡度流则相反。三层连续密度系统的结论与两层系统的结论相反。这表明,对于背景剪切流对ISW剪切效应的影响,考虑或忽略斜斜厚度可能会得出相反的结论。进一步讨论了非线性背景剪切流的影响。对于大多数特性,非线性电流的影响与线性电流的影响是一致的,尽管它们通常很弱。
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引用次数: 0
Global wave model performance in the vicinity of the Monterey Bay, California 加州蒙特利湾附近全球波浪模式的表现
IF 2.9 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2025-10-30 DOI: 10.1016/j.ocemod.2025.102645
Agustinus Ribal , Brian K. Haus , Stefan Zieger , Milan Curcic
Accurate wave modeling is crucial for coastal management, navigation, and marine safety, particularly in complex coastal environments like Monterey Bay. Here, we investigated the performance of a global wave model, specifically the third-generation WAVEWATCH III model, downscaled to Monterey Bay, California, over a two-year period. We employed two different source term packages, namely ST4 and ST6, for wind input. Four distinct grids were generated, with three of them being regular grids and one being unstructured. A two-way nesting approach was applied for three grids, with resolutions in the latitude of 0.5°, 0.2°, and 0.05°, respectively. The fourth grid is unstructured, with maximum and minimum resolutions of 2 km and 0.15 km, respectively. Boundary conditions for the unstructured grids were obtained from the two-way nesting grids. Additionally, the model was forced by CFSv2 wind data with resolutions of 0.2°. This study focuses on the highest-resolution model, which utilizes an unstructured grid. Significant wave heights were validated against data from five NDBC buoys, six CDIP buoys, 22 CLASI buoy locations, eight spotter buoys, and altimeter data. Across all 41 buoy locations and altimeter data, the model exhibits excellent agreement with the measurements in terms of statistical properties. Furthermore, we observed that ST4 outperformed ST6 in terms of scatter index and Pearson’s correlation coefficient, while ST6 exhibited lower RMSE and bias. Regarding computational time, it was found that ST4 runs 25 % slower than ST6. In addition to significant wave height, wind sea, and swell were also compared based on one-dimensional wave spectra. Eleven buoys were used to validate the swell, with both ST4 and ST6 showing similar statistical performance for wind sea while ST6 should be used in swell conditions because it runs faster and gives better results.
准确的波浪建模对海岸管理、导航和海洋安全至关重要,尤其是在像蒙特利湾这样复杂的沿海环境中。在这里,我们调查了全球波浪模型的性能,特别是第三代WAVEWATCH III模型,缩小到加利福尼亚州蒙特利湾,为期两年。对于风输入,我们使用了两个不同的源项包,即ST4和ST6。生成了四个不同的网格,其中三个是规则网格,一个是非结构化网格。对纬度分别为0.5°、0.2°和0.05°的三个网格采用双向嵌套方法。第四个网格是非结构化的,最大和最小分辨率分别为2公里和0.15公里。由双向嵌套网格得到非结构化网格的边界条件。此外,模型是由分辨率为0.2°的CFSv2风资料强迫的。本研究的重点是采用非结构化网格的最高分辨率模型。根据5个NDBC浮标、6个CDIP浮标、22个CLASI浮标位置、8个观测浮标和高度计数据验证了显著波高。在所有41个浮标位置和高度计数据中,该模型在统计特性方面与测量结果非常吻合。此外,我们观察到ST4在散点指数和Pearson相关系数方面优于ST6,而ST6的RMSE和偏差更低。在计算时间方面,发现ST4比ST6慢25%。除了显著的波高外,还比较了基于一维波浪谱的风海和涌浪。我们使用了11个浮标来验证涌浪,ST4和ST6在风浪条件下的统计性能相似,而ST6应该在涌浪条件下使用,因为它运行更快,结果更好。
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引用次数: 0
A bias correction method for total water level prediction at continental scale 大陆尺度总水位预报的偏差校正方法
IF 2.9 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2025-10-28 DOI: 10.1016/j.ocemod.2025.102642
Hyungju Yoo , Haocheng Yu , Y. Joseph Zhang , Wenfan Wu , Fei Ye , Saeed Moghimi , Gregory Seroka , Zizang Yang , Edward Myers
Simulating Total Water Level (TWL) at continental scale is inherently challenging and it is often desirable to correct model bias a posteriori. Here we present a simple yet effective bias correction method for NOAA’s STOFS-3D (Three-Dimensional Surge and Tide Operational Forecast System) forecasting system. The method seeks to dynamically correct the model bias, calculated from the results from the previous 2 days, by compensating it with an adjusted non-tidal elevation boundary condition. The adjustment is spatially uniform but varies over each forecast cycle. We demonstrate that the existing 3D model bias is largely attributable to the model’s exclusion of the large-scale steric effect, and therefore the method can be effectively used to incorporate this effect into the 3D model. Assessment at over 140 NOAA stations in US east and Gulf coasts show significant reductions in biases and root-mean-square errors for the non-tidal elevation and TWL, while having a small impact on tides and surges during extreme conditions.
在大陆尺度上模拟总水位(TWL)本身就具有挑战性,通常需要在事后纠正模型偏差。本文针对美国国家海洋和大气管理局(NOAA)的STOFS-3D(三维浪涌和潮汐业务预报系统)预报系统提出了一种简单有效的偏差校正方法。该方法试图通过使用调整后的非潮汐高程边界条件来补偿根据前2天的结果计算出的模型偏差,从而动态修正模型偏差。调整在空间上是均匀的,但在每个预报周期内有所不同。我们证明了现有的三维模型偏差很大程度上归因于模型排除了大尺度立体效应,因此该方法可以有效地将这种效应纳入三维模型。在美国东部和墨西哥湾沿岸的140多个NOAA站点进行的评估显示,非潮汐高程和TWL的偏差和均方根误差显著减少,而在极端条件下对潮汐和浪涌的影响很小。
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引用次数: 0
Improving compound flood modeling skill in coastal transition zones 提高沿海过渡带复合洪水模拟技术
IF 2.9 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2025-10-28 DOI: 10.1016/j.ocemod.2025.102643
Fei Ye , Y. Joseph Zhang , Haocheng Yu , Felicio Cassalho , Julio Zyserman , Soroosh Mani , Saeed Moghimi , Hyungju Yoo , Greg Seroka , Zizang Yang , Edward Myers
Accurate simulation of compound flooding in the coastal transition zone requires a fully coupled hydrologic–hydrodynamic modeling system to capture the complex interactions between inland and oceanic floodwaters. Despite recent advances in fully coupled 3D modeling frameworks, significant challenges persist in resolving flow through intricate river networks, especially where small channels are poorly represented due to limitations in digital elevation models (DEMs). This study addresses these challenges by enhancing the model meshing process and evaluating coupling strategies in the lower Mississippi River region, a representative coastal transition zone with a dense and complex river network. We improve a previously developed semi-automatic meshing approach by incorporating the National Hydrography Dataset to ensure clean delineation and connectivity of small channels where DEM uncertainties often cause artificial blockages. We also assess two strategies for integrating hydrologic model outputs into the hydrodynamic domain: (1) a conventional “hand-off” method that imposes freshwater streamflows at the land boundary combined with spatially varying precipitation, and (2) an alternative scheme that distributes hydrologic outputs at every resolved channel within the hydrodynamic mesh. Results show that the enhanced mesh, combined with updated topographic data, substantially reduces domain-wide bias and improves water-level skill at inland USGS stations. The alternative coupling scheme produces results comparable to the base method, providing an extensible framework for potential future development. By improving inland channel resolution and establishing a pathway for deeper coupling with hydrologic models, this work strengthens the scientific foundation and contributes to the operational readiness of compound flood forecasting.
沿海过渡带复合洪水的精确模拟需要一个完全耦合的水文-水动力模拟系统,以捕捉内陆和海洋洪水之间复杂的相互作用。尽管最近在全耦合3D建模框架方面取得了进展,但在解决复杂河流网络的流量方面仍然存在重大挑战,特别是由于数字高程模型(dem)的限制,小渠道的流量表现不佳。本研究通过加强模型网格化过程和评估密西西比河下游地区的耦合策略来解决这些挑战,这是一个具有密集和复杂河网的代表性沿海过渡区。我们通过整合国家水文数据集改进了以前开发的半自动网格划分方法,以确保DEM不确定性经常导致人工阻塞的小通道的清晰划定和连通性。我们还评估了将水文模型输出整合到水动力域中的两种策略:(1)传统的“移交”方法,该方法在陆地边界施加淡水流量,并结合空间变化的降水;(2)在水动力网格内的每个解决通道中分配水文输出的替代方案。结果表明,增强的网格与更新的地形数据相结合,大大减少了域范围内的偏差,提高了内陆USGS站的水位技能。替代耦合方案产生的结果与基本方法相当,为潜在的未来开发提供了可扩展的框架。通过提高内河航道分辨率,建立与水文模型更深层次耦合的途径,增强了洪水复合预报的科学基础和业务准备。
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引用次数: 0
Application of Gaussian beam superposition method in the Wavefront model for internal tides 高斯波束叠加法在内潮波前模型中的应用
IF 2.9 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Pub Date : 2025-10-27 DOI: 10.1016/j.ocemod.2025.102641
Zijian Cui , Tao Ding , Beifeng Zhou , Chujin Liang , Weifang Jin , Feilong Lin
Modern remote sensing techniques can now systematically extract coherent internal tidal signals (mode-1 and mode-2) from global sea surface height measurements. This capability arises from the accumulation of multi-source satellite altimetry data. However, the steady-state internal tides constructed by this method have limitations. They cannot fully characterize how dynamic oceanographic environmental variations influence internal tides. In realistic oceanic conditions, stratification and background currents significantly modulate the phase velocity and amplitude of internal tides. This modulation significantly enhances the energy proportion of incoherent internal tides. This study proposes applying the Gaussian beam superposition method to the Wavefront model to improve its capability in calculating internal tide energy evolution within complex oceanic environments, with validation provided by two sets of mooring observations from the northern South China Sea. The developed approach demonstrates potential for modeling time-varying patterns in global internal tide energy distribution under varying stratification and background current conditions.
现代遥感技术现在可以系统地从全球海面高度测量中提取连贯的内部潮汐信号(模式1和模式2)。这种能力来自多源卫星测高数据的积累。然而,用这种方法构造的稳态内潮有其局限性。它们不能完全描述动态海洋环境变化如何影响内部潮汐。在实际的海洋条件下,分层和背景海流显著地调节了内部潮汐的相速度和幅度。这种调制显著提高了非相干内潮的能量比例。本研究提出将高斯波束叠加方法应用于波前模型,以提高其在复杂海洋环境下计算内部潮汐能量演变的能力,并通过南海北部两组系泊观测数据进行验证。所开发的方法显示了在不同分层和背景电流条件下模拟全球内部潮汐能量分布时变模式的潜力。
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引用次数: 0
期刊
Ocean Modelling
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