海洋和大气是地球气候系统关键组成部分,其相互作用对全球气候及人类生活产生深远影响。为了分析海气相互作用的研究现状与未来的发展趋势。采用文献计量分析方法,运用VOSviewer和CiteSpace工具,筛选了中国知网(China National Knowledg...海洋和大气是地球气候系统关键组成部分,其相互作用对全球气候及人类生活产生深远影响。为了分析海气相互作用的研究现状与未来的发展趋势。采用文献计量分析方法,运用VOSviewer和CiteSpace工具,筛选了中国知网(China National Knowledge Infrastructure,CNKI)和Web of Science核心合集数据库中关于海气相互作用的文献,通过分析关键词共现网络图谱、时间序列图谱、突现网络图谱以及文献的发文国家和机构分布,对1981-2021年中国在该领域的研究进展和未来发展趋势进行了综合评估。同时,本研究还选取了2001-2021年的国际文献,对全球范围内的研究进展和热点问题进行了分析。研究表明,国内外在海气相互作用领域的研究均从宏观到微观角度深入探讨,着重研究了大气和海洋的基本作用机理,并进一步分析了影响地球气候系统的多种因素,目前研究重点转向了极端天气系统的预测及其运行机制。从研究机构和国家分布来看,高校与政府机构是主要的研究主体,国内研究机构之间的合作联系较为紧密。研究关键方向和方法,从宏观层面的基础研究转向更为深入的海气通量和大尺度过程研究。这一转变反映了国际海洋发展战略的调整,同时为未来的研究方向提供了新的视角和思路。展开更多
为研究波流共同作用下珊瑚礁海岸附近水动力特性,本文基于雷诺平均的Navier-Stokes方程(Reynolds-averaged Navier-Stokes equations,RANS)建立了2维数值波流水槽,分别采用k-ωSST湍流模型模拟湍流和流体体积法(volume of fluid,VOF)追...为研究波流共同作用下珊瑚礁海岸附近水动力特性,本文基于雷诺平均的Navier-Stokes方程(Reynolds-averaged Navier-Stokes equations,RANS)建立了2维数值波流水槽,分别采用k-ωSST湍流模型模拟湍流和流体体积法(volume of fluid,VOF)追踪自由液面。模拟定常正向流和反向流,并与只考虑波浪的情形进行对比,重点分析了水流对沿礁波高、平均水位以及破碎带附近波生流、湍动能和雷诺剪切应力的影响。结果表明,相对于纯波浪的情况,正向流使礁坪波高和增水减小,反向流使礁坪波高和增水增大,增减幅度随水流流量的增加而增大,正向流影响下破碎带附近沿水深方向整个水体均为向岸流,反向流影响下破碎带附近波谷上方为向岸流下方为离岸流,波谷下方水流强度均随着流量的增加而增大;破碎带附近的湍动能和雷诺剪切应力的随着正向流流量的增加而减小,随着反向流流量的增加而增大。展开更多
Employing the nonlinear local Lyapunov exponent (NLLE) technique, this study assesses the quantitative predictability limit of oceanic mesoscale eddy (OME) tracks utilizing three eddy datasets for both annual and seas...Employing the nonlinear local Lyapunov exponent (NLLE) technique, this study assesses the quantitative predictability limit of oceanic mesoscale eddy (OME) tracks utilizing three eddy datasets for both annual and seasonal means. Our findings reveal a discernible predictability limit of approximately 39 days for cyclonic eddies (CEs) and 44 days for anticyclonic eddies (AEs) within the South China Sea (SCS). The predictability limit is related to the OME properties and seasons. The long-lived, large-amplitude, and large-radius OMEs tend to have a higher predictability limit. The predictability limit of AE (CE) tracks is highest in autumn (winter) with 52 (53) days and lowest in spring (summer) with 40 (30) days. The spatial distribution of the predictability limit of OME tracks also has seasonal variations, further finding that the area of higher predictability limits often overlaps with periodic OMEs. Additionally, the predictability limit of periodic OME tracks is about 49 days for both CEs and AEs, which is 5-10 days higher than the mean values. Usually, in the SCS, OMEs characterized by high predictability limit values exhibit more extended and smoother trajectories and often move along the northern slope of the SCS.展开更多
Elucidating the flow features around piles in local scouring processes is crucial for studies of local scouring mechanisms and scour depth estimates.This study details the flow turbulence characteristics of two submer...Elucidating the flow features around piles in local scouring processes is crucial for studies of local scouring mechanisms and scour depth estimates.This study details the flow turbulence characteristics of two submerged piles that are determined by solving the Navier-Stokes equations with the improved delayed detached eddy simulation model.This model is verified by comparing experimental and numerical results for hydrodynamic parameters with the literature for both square-crossing piles(SCPs)and circular-crossing piles(CCPs).Original topographies of flat and scoured beds(i.e.,the initial and equilibrium scouring stages)are based on experimental results obtained by the authors in the present paper.SCP and CCP flow features in the scouring process are discussed.The results indicate that during the scouring process,the time-averaged drag coefficient and root mean square(rms)of the lift coefficient increase linearly in the CCP test,while the rms of the lift coefficient in the SCP test decreases linearly.Moreover,the minimum pressure coefficient is always located in the upstream corners in the SCP case but moves from 72.5°to 79.5°when the scour hole is completely developed in the CCP case.Downward flow behind the pile,which is generated by separated boundary layers above the top face of the pile,can reach the sand bed and turn the separated shear layers into patches of small vortices in the near-wake regions.Thus,the high shear stress zones are mainly at the scour edges under scoured-bed conditions.展开更多
文摘海洋和大气是地球气候系统关键组成部分,其相互作用对全球气候及人类生活产生深远影响。为了分析海气相互作用的研究现状与未来的发展趋势。采用文献计量分析方法,运用VOSviewer和CiteSpace工具,筛选了中国知网(China National Knowledge Infrastructure,CNKI)和Web of Science核心合集数据库中关于海气相互作用的文献,通过分析关键词共现网络图谱、时间序列图谱、突现网络图谱以及文献的发文国家和机构分布,对1981-2021年中国在该领域的研究进展和未来发展趋势进行了综合评估。同时,本研究还选取了2001-2021年的国际文献,对全球范围内的研究进展和热点问题进行了分析。研究表明,国内外在海气相互作用领域的研究均从宏观到微观角度深入探讨,着重研究了大气和海洋的基本作用机理,并进一步分析了影响地球气候系统的多种因素,目前研究重点转向了极端天气系统的预测及其运行机制。从研究机构和国家分布来看,高校与政府机构是主要的研究主体,国内研究机构之间的合作联系较为紧密。研究关键方向和方法,从宏观层面的基础研究转向更为深入的海气通量和大尺度过程研究。这一转变反映了国际海洋发展战略的调整,同时为未来的研究方向提供了新的视角和思路。
文摘为研究波流共同作用下珊瑚礁海岸附近水动力特性,本文基于雷诺平均的Navier-Stokes方程(Reynolds-averaged Navier-Stokes equations,RANS)建立了2维数值波流水槽,分别采用k-ωSST湍流模型模拟湍流和流体体积法(volume of fluid,VOF)追踪自由液面。模拟定常正向流和反向流,并与只考虑波浪的情形进行对比,重点分析了水流对沿礁波高、平均水位以及破碎带附近波生流、湍动能和雷诺剪切应力的影响。结果表明,相对于纯波浪的情况,正向流使礁坪波高和增水减小,反向流使礁坪波高和增水增大,增减幅度随水流流量的增加而增大,正向流影响下破碎带附近沿水深方向整个水体均为向岸流,反向流影响下破碎带附近波谷上方为向岸流下方为离岸流,波谷下方水流强度均随着流量的增加而增大;破碎带附近的湍动能和雷诺剪切应力的随着正向流流量的增加而减小,随着反向流流量的增加而增大。
基金supported by the National Key R&D Program for Developing Basic Sciences(2022YFC3104802).
文摘Employing the nonlinear local Lyapunov exponent (NLLE) technique, this study assesses the quantitative predictability limit of oceanic mesoscale eddy (OME) tracks utilizing three eddy datasets for both annual and seasonal means. Our findings reveal a discernible predictability limit of approximately 39 days for cyclonic eddies (CEs) and 44 days for anticyclonic eddies (AEs) within the South China Sea (SCS). The predictability limit is related to the OME properties and seasons. The long-lived, large-amplitude, and large-radius OMEs tend to have a higher predictability limit. The predictability limit of AE (CE) tracks is highest in autumn (winter) with 52 (53) days and lowest in spring (summer) with 40 (30) days. The spatial distribution of the predictability limit of OME tracks also has seasonal variations, further finding that the area of higher predictability limits often overlaps with periodic OMEs. Additionally, the predictability limit of periodic OME tracks is about 49 days for both CEs and AEs, which is 5-10 days higher than the mean values. Usually, in the SCS, OMEs characterized by high predictability limit values exhibit more extended and smoother trajectories and often move along the northern slope of the SCS.
基金support from the National Natural Science Foundation of China (Nos.52301324 and 52001276)the Natural Science Foundation of Zhejiang Province (No.LQ24E090001)+2 种基金the Open Fund of Key Laboratory of Estuary and Coast of Zhejiang Province (No.ZIHE21005)the Natural Science Foundation of Ningbo (No.2021J096)the Zhejiang Transportation Science and Technology (No.2021064)。
文摘Elucidating the flow features around piles in local scouring processes is crucial for studies of local scouring mechanisms and scour depth estimates.This study details the flow turbulence characteristics of two submerged piles that are determined by solving the Navier-Stokes equations with the improved delayed detached eddy simulation model.This model is verified by comparing experimental and numerical results for hydrodynamic parameters with the literature for both square-crossing piles(SCPs)and circular-crossing piles(CCPs).Original topographies of flat and scoured beds(i.e.,the initial and equilibrium scouring stages)are based on experimental results obtained by the authors in the present paper.SCP and CCP flow features in the scouring process are discussed.The results indicate that during the scouring process,the time-averaged drag coefficient and root mean square(rms)of the lift coefficient increase linearly in the CCP test,while the rms of the lift coefficient in the SCP test decreases linearly.Moreover,the minimum pressure coefficient is always located in the upstream corners in the SCP case but moves from 72.5°to 79.5°when the scour hole is completely developed in the CCP case.Downward flow behind the pile,which is generated by separated boundary layers above the top face of the pile,can reach the sand bed and turn the separated shear layers into patches of small vortices in the near-wake regions.Thus,the high shear stress zones are mainly at the scour edges under scoured-bed conditions.
