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Boundary layer interaction of immiscible non-Newtonian nanofluids in distinct shear flows with motile microorganisms 不同剪切流动中非牛顿纳米流体的边界层相互作用
IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-01 Epub Date: 2025-12-03 DOI: 10.1016/j.dynatmoce.2025.101629
Z. Abbas, S. Goher, M.Y. Rafiq
This study presents a comprehensive numerical investigation of two-phase boundary layer shear flows involving immiscible non-Newtonian Carreau and Tangent hyperbolic nanofluids incorporating motile microorganisms. The analysis explores the coupled effects of thermophoresis, Brownian motion, and thermal radiation on velocity, temperature, concentration, and microorganism density profiles across distinct shear regions. Incorporating microorganisms within nanofluids enhances thermal conductivity and stabilizes the flow structure, contributing to improved transport phenomena relevant to biomedical, energy, and environmental systems. The governing nonlinear differential equations are transformed into dimensionless form using similarity transformations and solved via the MATLAB bvp4c collocation method to ensure high numerical accuracy. A grid independence test confirms the convergence and stability of the scheme for all parametric variations. The results demonstrate that the Carreau fluid parameter promotes fluid velocity, while an increase in the viscosity ratio and shear strength ratio reduces it. Brownian motion and thermophoresis parameters suppress temperature near the interface, whereas thermal radiation enhances it. The density of motile microorganisms rises with higher bioconvection and Péclet numbers but decreases with increasing microorganism Schmidt number. Quantitative results for skin friction, Nusselt number, Sherwood number, and microorganism density validate the influence of these parameters in both regions. The findings provide valuable insights for optimizing microfluidic transport, bioconvective systems, and nanofluid-based heat exchangers where multi-phase shear interactions and microorganism activity are significant.
这项研究提出了一个全面的数值研究两相边界层剪切流动涉及非混相非牛顿卡罗和切线双曲纳米流体包含运动微生物。分析探讨了热泳、布朗运动和热辐射对不同剪切区域的速度、温度、浓度和微生物密度分布的耦合效应。在纳米流体中加入微生物可以增强导热性,稳定流动结构,有助于改善与生物医学、能源和环境系统相关的传输现象。采用相似变换将控制非线性微分方程转化为无因次形式,并采用MATLAB bvp4c配置法求解,保证了较高的数值精度。网格无关性测试证实了该方案对所有参数变化的收敛性和稳定性。结果表明:carcarau流体参数对流体速度有促进作用,而黏度比和抗剪强度比的增大对流体速度有抑制作用;布朗运动和热泳参数抑制界面附近的温度,而热辐射则增强界面附近的温度。流动微生物密度随生物对流和psamclet数的增加而升高,随微生物施密特数的增加而降低。皮肤摩擦、努塞尔数、舍伍德数和微生物密度的定量结果验证了这些参数在两个区域的影响。这些发现为优化微流体传输、生物对流系统和基于纳米流体的热交换器提供了有价值的见解,其中多相剪切相互作用和微生物活性是重要的。
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引用次数: 0
Investigation of heat and mass transfer in an electromagnetically driven ionized tri-hybrid nanofluids flow over a convectively heated cylinder 电磁驱动电离三杂化纳米流体在对流加热圆柱体上的传热传质研究
IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-01 Epub Date: 2025-12-20 DOI: 10.1016/j.dynatmoce.2025.101635
Muhammad Naveed Khan , Shafiq Ahmad , Aamir Abbas Khan , Mounirah Areshi , Ibrahim E. Elseesy
Nanofluids are employed in various heat transfer and cooling applications because of their enhanced thermal conductivity, making them useful for electronics cooling, solar collectors, and heat exchangers. The current study explores the behavior of a partially ionized Prandtl fluid with three types of nanoparticles as it flows through a convectively heated cylinder under magnetic influence. The purpose of dispersing three different nanoparticles MWCNT,Al2O3,SiC is to increase the functional fluid heat transfer rate. The study looks at how powerful produced magnetic and electric fields affect fluid flow under the supposition that the magnetic Reynolds number is very high. The study analyzes the mass and heat equations while taking into account factors like Joule heating, activation energy, varying thermal conductivity, and changing mass diffusivity. Additionally, the consequences of Joule heating, viscous dissipation, and thermal radiation are appraised when evaluating the disorder in the flow system through entropy generation. Based on these assumptions, differential equations were employed to create the mathematical model. The differential equations are then subjected to similarity variables to become a dimensionless variant of ordinary differential equations. The numerical scheme BVP4C on MATLAB has been used to find the numerical results. The comparison results are found for ternary nanofluid MWCNT,Al2O3,SiC and unary nanofluid Al2O3 using graphs. It is observed from the figures that in enhancement in Prandtl first parameter, curvature parameter, Hall and ion slip effect, the fluid motion enhances while the reverse behavior is observed for Hartman number. The fluid temperature surges with stronger estimations of the Dufour number, variable thermal conductivity, and radiation parameter.
纳米流体被用于各种传热和冷却应用,因为它们具有增强的导热性,使它们在电子冷却、太阳能集热器和热交换器中非常有用。目前的研究探索了部分电离的普朗特流体与三种类型的纳米颗粒在磁场影响下流经对流加热圆柱体时的行为。分散MWCNT、Al2O3、SiC三种不同纳米颗粒的目的是提高功能流体的传热速率。该研究着眼于在假设磁雷诺数非常高的情况下,产生的强大磁场和电场如何影响流体流动。该研究分析了质量和热量方程,同时考虑了焦耳加热、活化能、热导率变化和质量扩散率变化等因素。此外,焦耳加热,粘性耗散和热辐射的后果评估时,通过熵的产生流动系统的混乱。基于这些假设,采用微分方程建立数学模型。然后对微分方程进行相似变量处理,使其成为常微分方程的无量纲变体。利用MATLAB上的数值格式BVP4C进行了数值计算。用图形对比了三元纳米流体MWCNT、Al2O3、SiC和一元纳米流体Al2O3的效果。从图中可以看出,在普朗特第一参数、曲率参数、霍尔效应和离子滑移效应增强时,流体运动增强,而哈特曼数则相反。流体温度随着Dufour数、变热导率和辐射参数的增强而波动。
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引用次数: 0
Impact of ENSO on the genesis potential index of cyclones over the Bay of Bengal during the post-monsoon season 后季风季节ENSO对孟加拉湾气旋发生势指数的影响
IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-01 Epub Date: 2026-01-02 DOI: 10.1016/j.dynatmoce.2025.101642
P. Suneeta , TVS Udaya Bhaskar , S.S.V.S. Ramakrishna
Tropical Cyclones (TCs) are among the most destructive weather phenomena, causing substantial damage to coastal regions and vulnerable communities along the Bay of Bengal. Predicting their formation remains a significant challenge due to the complex interactions between atmospheric and oceanic processes. This study investigates the influence of the El Niño–Southern Oscillation (ENSO) on the Genesis Potential Index (GPI) and the Total Number of Depressions and Cyclones (TNDC) over the Bay of Bengal (5°–20°N, 80°–100°E) during the post-monsoon season (October–December) from 1995 to 2019. Cyclone activity associated with El Niño, La Niña, and Neutral ENSO phases is examined using four GPI formulations based on key atmospheric and oceanic parameters, including a newly developed index from our previous research. The results reveal pronounced ENSO-dependent variations in vertical wind shear, Upper Ocean Heat Content (UOHC), depth of the 26 °C isotherm (D26), Sea Surface Temperature (SST), Sea Surface Height Anomaly (SSHA), latent heat flux, net longwave radiation, and low-level relative vorticity. During La Niña years, reduced vertical wind shear, enhanced low-level cyclonic vorticity, deeper thermocline, higher UOHC, and increased air–sea heat fluxes create a dynamically and thermodynamically favorable environment for cyclone genesis, leading to GPI values nearly twice those observed during El Niño and Neutral phases. These findings demonstrate the critical role of ENSO-driven atmospheric–oceanic coupling in modulating cyclone genesis over the Bay of Bengal and highlight the importance of incorporating ENSO-related variability into regional cyclone forecasting and disaster risk management strategies.
热带气旋(tc)是最具破坏性的天气现象之一,对孟加拉湾沿岸地区和脆弱社区造成重大破坏。由于大气和海洋过程之间复杂的相互作用,预测它们的形成仍然是一个重大挑战。本文研究了1995 - 2019年季风后季节(10 - 12月),El Niño-Southern涛动(ENSO)对孟加拉湾(5°-20°N, 80°-100°E)发生势指数(GPI)和低压和气旋总数(TNDC)的影响。使用基于关键大气和海洋参数的四种GPI公式,包括我们以前研究中新开发的指数,研究了与El Niño、La Niña和中性ENSO阶段相关的气旋活动。结果表明,垂直风切变、上层海洋热含量(UOHC)、26°C等温线深度(D26)、海面温度(SST)、海面高度异常(SSHA)、潜热通量、净长波辐射和低层相对涡度存在明显的enso相关变化。La Niña年垂直风切变的减少、低层气旋涡度的增强、温跃层的加深、UOHC的增加以及海气热通量的增加为气旋形成创造了动力和热力有利的环境,导致GPI值几乎是El Niño和中性期的两倍。这些发现证明了enso驱动的大气-海洋耦合在调节孟加拉湾气旋形成中的关键作用,并强调了将enso相关变率纳入区域气旋预报和灾害风险管理战略的重要性。
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引用次数: 0
Rainfall extremes variability, teleconnections with atmospheric circulation anomalies in the Indian summer monsoon 降雨极端变率与印度夏季风大气环流异常的遥相关
IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-01 Epub Date: 2025-12-20 DOI: 10.1016/j.dynatmoce.2025.101636
Anmol Yadav , G.P. Singh , Pradeep Kumar Rai , Vijay Kumar Soni , Akhilesh Mishra , Sonu Kumar
We investigate the spatiotemporal variability of Indian Summer Monsoon Rainfall (ISMR) and the anomalies in atmospheric circulation and oceanic conditions during June–September (JJAS) from 1981 to 2022. Using multiple data sources (like IMD, NOAA PSL and HadISST), Empirical orthogonal function (EOF), principal component (PCs) coefficient of variation (CV), precipitation concentration index (PCI), composite analysis of atmospheric and oceanic anomalies determines the variability for exploring extreme wet and dry years. Seasonal rainfall is highest over Northeast India and Western Ghats, while the decadal trend shows increased rainfall in July, August, and September. EOF analysis shows that first mode covers central and southern India, whereas the second mode exhibits a dipole pattern over the Gangetic plains and southern regions with 14.9 % and 9.1 % of the total variance. Eight extremely wet and six extremely dry years were also noted. In composite analysis, wherever extreme wet and dry years are found, these modes correspond to distinct Sea Surface Temperature (SST), Sea Level Pressure (SLP) and wind anomalies across oceanic regions. Wet years exhibit positive rainfall anomalies related with warm SST in Indian Ocean and cooler SST in the Niño 3.4 region, accompanied by low SLP anomalies and enhanced south-westerly wind. Dry years are characterized by cooler SST in the Indian Ocean, warmer Nino 3.4, SST, higher SLP, weak winds, and limited moisture transport, which contribute to the reduction in monsoon activity. These findings underscore the significant role of SST, SLP, wind, and vertical motion, vertically integrated moisture flux and soil moisture anomalies influencing ISMR patterns.
本文研究了1981 - 2022年6 - 9月印度夏季风降水(ISMR)的时空变异性以及大气环流和海洋条件的异常。利用多个数据源(如IMD、NOAA PSL和HadISST),利用经验正交函数(EOF)、主成分变异系数(CV)、降水浓度指数(PCI)对大气和海洋异常进行综合分析,确定了探索极端干湿年的变率。印度东北部和西高止山脉的季节性降雨量最高,而年代际趋势显示,7月、8月和9月降雨量增加。EOF分析表明,第一模态覆盖印度中部和南部,而第二模态在恒河平原和南部地区表现为偶极子型,占总方差的14.9 %和9.1 %。还有8年极度潮湿,6年极度干燥。在复合分析中,无论在哪里发现极端干湿年份,这些模态都对应不同的海表温度(SST)、海平面压力(SLP)和海洋区域的风异常。湿润年表现出与印度洋海温偏暖和Niño 3.4区域海温偏冷相关的正降水异常,伴随着低SLP异常和西南风增强。干燥年印度洋海温偏冷,Nino 3.4偏暖,海温升高,SLP升高,风弱,水汽输送受限,导致季风活动减弱。这些发现强调了海温、SLP、风和垂直运动、垂直整合的水分通量和土壤水分异常对ISMR模式的重要影响。
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引用次数: 0
Deep learning for sea surface temperature prediction in the Indian Ocean: A comparative study using 1D-CNN, LSTM, 1DCNN-LSTM and attention based 1DCNN-LSTM architectures 深度学习在印度洋海表温度预测中的应用:基于1D-CNN、LSTM、1DCNN-LSTM和基于注意力的1DCNN-LSTM架构的比较研究
IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-01 Epub Date: 2025-12-13 DOI: 10.1016/j.dynatmoce.2025.101632
B. Sheela Rani , D. Sathya Narayanan , M.B. Salma Jasmine , N.R. Krishnamoorthy , M. Roja Raman , Aneesh A. Lotliker , Abhisek Chatterjee
Anthropogenic activities had led to major climate changes, causing the oceans to warm rapidly. Subsequently, there is a need for accurate prediction of sea surface temperature (SST). The dynamic Indian Ocean climate, weather and marine ecology is significantly affected by SST changes. In this study, hourly and daily SST data, specifically from 15 and 7 RAMA stations (1 m deep) respectively, at different parts of Indian Ocean is utilized to forecast SST using four deep learning techniques; 1D Convolutional Neural Network (1D-CNN), Long Short-Term Memory (LSTM) network, 1DCNN-LSTM network and attention based 1DCNN-LSTM Architecture. The SST data obtained from RAMA buoy is trained using a sliding window method and model performance is evaluated based on evaluation matrices like Mean Squared Error (MSE), Root Mean Squared Error (RMSE), and Mean Absolute error (MAE). The results indicated that 1DCNN-LSTM outperforms 1D-CNN and LSTM at most sites, consistently achieving lower MSE, RMSE and MAE. The findings also revealed that in places where SST shifts significantly, the new attention based 1DCNN-LSTM model often competes with or does better than all the other models in MAE. Distinctive physical phenomena like equatorial jets, thermohaline stratification, monsoon, Indian Ocean Bipolar (IOD) and El Niño-Southern Oscillation (ENSO) bring about geographical difference in performance. Hence, the study illustrates how deep learning frameworks make better SST predictions in complex ocean basins and thereby aids in anticipating climate change.
人为活动导致了重大的气候变化,导致海洋迅速变暖。因此,需要对海温(SST)进行准确的预报。海温变化对印度洋气候、天气和海洋生态的影响是显著的。本研究利用印度洋不同地区15个和7个RAMA站(1 m深)的逐时和逐日海温数据,采用4种深度学习技术预测海温;一维卷积神经网络(1D- cnn)、长短期记忆(LSTM)网络、1DCNN-LSTM网络和基于注意力的1DCNN-LSTM架构。采用滑动窗口法对RAMA浮标获取的海表温度数据进行训练,并基于均方误差(MSE)、均方根误差(RMSE)和平均绝对误差(MAE)等评价矩阵对模型性能进行评价。结果表明,1DCNN-LSTM在大多数位点上优于1D-CNN和LSTM,均获得较低的MSE、RMSE和MAE。研究结果还表明,在海表温度发生显著变化的地方,新的基于注意力的1DCNN-LSTM模型通常与MAE中的所有其他模型竞争或做得更好。赤道喷流、温盐层、季风、印度洋双极(IOD)和厄尔尼诺Niño-Southern涛动(ENSO)等不同的物理现象造成了地理上的表现差异。因此,该研究说明了深度学习框架如何在复杂的海洋盆地中更好地预测海温,从而有助于预测气候变化。
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引用次数: 0
Transient mixed convection in coaxial pipes with temperature-dependent variable density 变密度温度同轴管内瞬态混合对流
IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-01 Epub Date: 2026-02-02 DOI: 10.1016/j.dynatmoce.2026.101649
Bakhtawar Bibi , Ali B.M. Ali , Muhammad Ashraf , Ghulam Rasool , Muhammad Usman Rashid , Abduvali Sottarov
This study investigates the effects of temperature-dependent variable density on mixed convective heat transfer in coaxial pipes. The inner pipe’s surface is stationary and uniformly heated, with flow along its axis, while the outer wall is placed at infinity. A two-dimensional time-dependent flow and temperature field are modeled using coupled nonlinear partial differential equations, solved numerically via the implicit finite difference method. Simulations explore a range of parameters to predict thermal efficiency, steady-state velocity, temperature distribution, dynamic surface shear, and energy shear. Results show that increasing the density variation parameter (m = 0.1, 1.5, 2.0, 2.5) enhances fluid velocity and thermal distribution, peaking at m = 2.5. Energy shear increases with mm, reaching a maximum at m = 0.7, while surface shear remains uniform. These findings provide insights into optimizing thermal performance in coaxial flow systems.
本文研究了变密度对同轴管内混合对流换热的影响。管内表面是静止的,受热均匀,流体沿其轴线流动,而外壁则处于无穷远处。采用耦合非线性偏微分方程对二维随时间变化的流场和温度场进行建模,并采用隐式有限差分法进行数值求解。模拟探索了一系列参数来预测热效率、稳态速度、温度分布、动态表面剪切和能量剪切。结果表明:增大密度变化参数(m = 0.1、1.5、2.0、2.5),流体速度和热分布得到增强,在m = 2.5处达到峰值;能量剪切随mm增大,在m = 0.7处达到最大值,表面剪切保持均匀。这些发现为优化同轴流系统的热性能提供了见解。
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引用次数: 0
Surface wave-induced modulation of submesoscale fronts: A process governed by model resolution 亚中尺度锋面的表面波诱导调制:一个由模式分辨率控制的过程
IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-01 Epub Date: 2026-01-13 DOI: 10.1016/j.dynatmoce.2026.101645
Cheng Peng , Peng Wang , Dongxiao Wang
Submesoscale fronts in marginal seas typically exhibit complex generation mechanisms that are highly dependent on local background flows and various forcing factors, such as winds, tides, etc. Among these forcing factors, the influence of waves remains under-research. This study investigates the effects of surface gravity waves on submesoscale fronts in the Northern South China Sea using numerical simulations. Simulation results indicate that the intensity of submesoscale fronts is significantly affected by waves. However, unlike previous studies in which the wave-induced Stokes vortex force is found to enhance frontal structures, in the present study, the Stokes vortex force is weak and negligible at kilometer-scale model resolution. Instead, the Stokes Coriolis force, another wave-induced force, contributes to the momentum balance, resulting in the transition of turbulent thermal wind (TTW) to Stokes-TTW at the submesoscale fronts. Furthermore, the Stokes Coriolis force triggers an anti-Stokes flow, which opposes the Eulerian current in the study area. As a result, the current is weakened, reducing the current-induced frontogenesis and ultimately diminishing the intensity of submesoscale fronts.
边缘海的亚中尺度锋面通常表现出复杂的形成机制,高度依赖于当地背景流和各种强迫因子,如风、潮汐等。在这些强迫因素中,波浪的影响仍在研究中。本文利用数值模拟方法研究了表面重力波对南海北部亚中尺度锋面的影响。模拟结果表明,亚中尺度锋面的强度受波浪的影响较大。然而,与以往的研究发现波浪诱导的Stokes涡旋力可以增强锋面结构不同,在本研究中,Stokes涡旋力在千米尺度模型分辨率下是微弱的,可以忽略不计。相反,另一种波致力Stokes- Coriolis力有助于动量平衡,导致湍流热风(TTW)在亚中尺度锋面向Stokes-TTW过渡。此外,斯托克斯-科里奥利力在研究区域内引发反斯托克斯流,与欧拉流相对立。因此,电流减弱,减少了电流诱导的锋生,最终降低了亚中尺度锋的强度。
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引用次数: 0
Sensitivity analysis of the physics options in the Weather Research and Forecasting model and its impact on storm surge simulations during two tropical cyclones over the Bay of Bengal 天气研究与预报模式中物理选项的敏感性分析及其对孟加拉湾两个热带气旋风暴潮模拟的影响
IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-01 Epub Date: 2026-01-03 DOI: 10.1016/j.dynatmoce.2025.101643
Vyshnavi Sai Yalla , A.N.V. Satyanarayana , P.L.N. Murty , K.Siva Srinivas
Accurate prediction of tropical cyclones and associated storm surges over the Bay of Bengal (BoB) is crucial for disaster risk reduction and coastal planning. In the present study, a high-resolution mesoscale model, WRF-ARW 4.0 is used and conducted sensitivity experiments with eight combinations of four cloud microphysics schemes (Lin, WSM6, Thompson, WDM6) and two planetary boundary layer schemes (YSU and MYJ) to evaluated the best combination in simulating the outer and inner core wind intensity and cyclone track of two severe cyclones, Amphan and Yaas over BoB. The simulations of wind and cyclone tracks are validated along the best track of the India Meteorological Department. The analysis of the results reveals that the combination of physical schemes, Thompson with YSU, and WSM6 with YSU, reasonably captures the inner and outer core winds and track of cyclones with a mean error of 4.2–8.5 ms−1 and 48–105 km, respectively. The simulations of the eight combinations of physics schemes are utilised in a coupled hydrodynamic model of ADCIRC and SWAN to assess storm surges and significant wave heights. The simulated storm surges are validated using available tide gauge observations at Paradip (20.2817° N, 86.6727° E) and Dhamra (20.8237° N, 86.9640° E) port for the Amphan and Yaas cyclone, and simulations of significant wave heights are validated against moored buoy observations at BD08 (18.1613° N, 89.6702° E) and BD09 (17.8563° N, 89.6772° E) locations. Statistical analysis using Taylor diagrams revealed that the WRF model with the two physics combinations, Thompson–YSU and WSM6–YSU, demonstrated improved accuracy in predicting storm surges and significant wave heights during both cyclones. The findings identify the performance of an appropriate physics combination of the WRF model for improved storm surge predictions over the BoB cyclones.
孟加拉湾热带气旋和相关风暴潮的准确预报对减少灾害风险和沿海规划至关重要。本文利用WRF-ARW 4.0高分辨率中尺度模式,对4种云微物理方案(Lin、WSM6、Thompson、WDM6)和2种行星边界层方案(YSU和MYJ)的8种组合进行了灵敏度试验,评价了模拟BoB上空两个强气旋Amphan和Yaas的内外核风强度和气旋路径的最佳组合。沿印度气象部门的最佳路径对风和气旋路径的模拟进行了验证。结果表明,Thompson + YSU和WSM6 + YSU两种物理方案能较好地捕捉气旋的内、外核心风和路径,平均误差分别为4.2 ~ 8.5 ms−1和48 ~ 105 km。在ADCIRC和SWAN的耦合水动力模型中,利用8种物理方案组合的模拟来评估风暴潮和显著浪高。利用Paradip(20.2817°N, 86.6727°E)和Dhamra(20.8237°N, 86.9640°E)港口对Amphan和Yaas气旋的潮汐计观测验证了模拟的风暴潮,并根据BD08(18.1613°N, 89.6702°E)和BD09(17.8563°N, 89.6772°E)位置的系泊浮标观测验证了显著浪高的模拟。利用泰勒图进行统计分析,结果表明,WRF模型采用了两种物理组合,Thompson-YSU和WSM6-YSU,在预测两个气旋期间的风暴潮和显著浪高方面表现出更高的准确性。研究结果确定了WRF模式的适当物理组合的性能,以改进对BoB气旋的风暴潮预测。
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引用次数: 0
Coastal water level trends and ENSO-related variability in the northeastern Mekong Delta (1979–2024) 湄公河三角洲东北部沿海水位趋势及enso相关变率(1979-2024)
IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-01 Epub Date: 2026-01-29 DOI: 10.1016/j.dynatmoce.2026.101648
Vu Duy Vinh , Sylvain Ouillon , Nguyen Minh Hai
Coastal water levels in the northeastern Mekong Delta exhibit pronounced long-term trends and interannual variability linked to large-scale climate forcing. Using tide-gauge observations at the Vam Kenh station (1979–2024) and CMEMS (Copernicus Marine Environment Monitoring Service) satellite altimetry (1993–2024), we assess long-term, seasonal, and ENSO-related water level variability. The results reveal a statistically significant and evidence of recent acceleration inferred from sub-period trends in mean relative water level, with rates exceeding approximately 6 mm yr⁻¹ over the last two decades (2005–2024), compared to about 5 mm yr⁻¹ over the full 46-year record. Seasonal variability shows modulation of the rise by the monsoon cycle, with faster increases during the northeast monsoon and slower rises during the southwest monsoon. Interannual variability is clearly modulated by the El Niño–Southern Oscillation, with strong La Niña events elevating water levels by up to about 5 cm in anomaly magnitude, while El Niño phases are generally associated with negative anomalies. Atmospheric pressure acts as a secondary control, contributing approximately 5–20 % of interannual variance through the inverse barometer effect. Tide-gauge and CMEMS data exhibit strong agreement (r = 0.95), supporting their combined use for coastal monitoring. Overall, the results highlight accelerating relative rise in a subsiding deltaic environment, with important implications for coastal vulnerability.
湄公河三角洲东北部沿海水位表现出明显的长期趋势和年际变化,与大规模气候强迫有关。利用Vam Kenh站的潮汐计观测(1979-2024)和CMEMS(哥白尼海洋环境监测服务)卫星测高(1993-2024),我们评估了长期、季节性和与enso相关的水位变化。结果显示,从平均相对水位的子周期趋势推断出的统计显著性和最近加速的证据,在过去二十年(2005-2024年)中,速度超过约6 毫米 yr⁻¹ ,而在整个46年的记录中,速度约为5 毫米 yr⁻¹ 。季节变化显示季风周期对上升的调节,东北季风期间上升较快,西南季风期间上升较慢。年际变率明显受到El Niño-Southern振荡的调制,强烈的La Niña事件使水位升高了约5 cm的异常量级,而El Niño期通常与负异常有关。大气压力作为次要控制,通过逆气压计效应贡献了大约5 - 20% %的年际变化。潮汐计和CMEMS数据显示出很强的一致性(r = 0.95),支持它们在海岸监测中的联合使用。总体而言,研究结果表明,在下沉的三角洲环境中,海平面相对上升速度加快,这对沿海地区的脆弱性具有重要意义。
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引用次数: 0
Risk mapping of dynamic dust storms and multi-hazard maritime navigation in the red sea using machine learning and MODIS Data 利用机器学习和MODIS数据绘制红海动态沙尘暴和多灾种海上航行风险图
IF 2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Pub Date : 2026-03-01 Epub Date: 2025-12-01 DOI: 10.1016/j.dynatmoce.2025.101621
Yazeed Alsubhi , Bassam M. Aljahdali , Ayman F. Alghanmi , Hussain T. Sulaimani , Ahmad E. Samman
Dust storms represent a significant hazard to maritime navigation, particularly in regions such as Saudi Arabia, where frequent dust events, driven by vast desert landscapes and oceanic wind patterns, reduce visibility and disrupt maritime operations. This paper proposes a comprehensive framework for evaluating visibility risks posed by dust storms in Saudi Arabian maritime zones, specifically focusing on the Red Sea. The methodology considers MODIS AOD (Aerosol Optical Depth) data, wind speed, and cloud cover to develop a dynamic risk assessment model using random forest (RF) for dust storm detection and visibility risk prediction. The model integrates spatial data layers for environmental factors (wind, waves, and depth), creating seasonal risk maps that dynamically adjust based on changing environmental conditions. GIS technology was used to visualize risk zones, and the RF model provided data-driven weighting of risk factors. The model’s performance was validated using metrics such as probability of detection (POD) (0.92), probability of false detection (PFD) (0.05), and equitable threat score (ETS) (0.85), demonstrating superior accuracy over traditional methods like analytic hierarchy process (AHP) and CRiteria importance through intercriteria correlation (CRITIC). The findings indicate that Autumn represents the most hazardous season for maritime navigation due to frequent dust storms, with the central Red Sea being the most impacted area. The results demonstrate the potential of this approach for improving navigation safety and early warning tools in the Red Sea and similar arid coastal regions.
沙尘暴对海上航行构成重大危害,特别是在沙特阿拉伯等地区,在那里,由于广阔的沙漠景观和海风模式,频繁发生沙尘暴,降低了能见度,扰乱了海上作业。本文提出了一个综合框架,用于评估沙尘暴在沙特阿拉伯海域造成的能见度风险,特别是关注红海。该方法考虑了MODIS AOD(气溶胶光学深度)数据、风速和云量,开发了一个使用随机森林(RF)进行沙尘暴探测和能见度风险预测的动态风险评估模型。该模型集成了环境因素(风、波浪和深度)的空间数据层,创建了基于不断变化的环境条件动态调整的季节性风险图。利用GIS技术可视化风险区域,RF模型提供数据驱动的风险因素加权。通过检测概率(POD)(0.92)、误检概率(PFD)(0.05)和公平威胁评分(ETS)(0.85)等指标验证了该模型的性能,显示出比传统方法(如层次分析法(AHP)和标准间相关性(CRITIC)标准重要性)更优的准确性。研究结果表明,由于沙尘暴频繁,秋季是海上航行最危险的季节,其中红海中部是受影响最严重的地区。结果表明,这种方法在改善红海和类似干旱沿海地区的航行安全和预警工具方面具有潜力。
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引用次数: 0
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Dynamics of Atmospheres and Oceans
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