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Seasonal Variability of Internal Tides Northeast of Taiwan
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作者 ZHAO Xinhua HOU Yijun +2 位作者 LIU Ze zhuang zhanpeng WANG Kaidi 《Journal of Ocean University of China》 SCIE CAS CSCD 2020年第3期740-746,共7页
The spatial-temporal characteristics of the barotropic tides and internal tides(ITs) northeast of Taiwan Island are examined, based on a 1-year mooring current observations from May 23, 2017 to May 19, 2018. The resul... The spatial-temporal characteristics of the barotropic tides and internal tides(ITs) northeast of Taiwan Island are examined, based on a 1-year mooring current observations from May 23, 2017 to May 19, 2018. The results of harmonic tidal analysis show that the barotropic tides are dominated by semidiurnal tides, which is mainly controlled by M2 tidal components. Moreover, the vertical structures of diurnal and semidiurnal ITs show that the semidiurnal IT shows notable seasonal variation, whereas seasonal variations of the diurnal IT energy is not significant. The semidiurnal IT energy in winter half year is twice that in summer half year. The seasonal variation of semidiurnal IT is mainly modulated by the direction change of the current rather than by the topographic features and stratification. In summer(winter) half year cyclonic(anti-cyclonic) eddies meanly control at this point, so the flow direction is mainly in the southwest(northeast) direction, causing the background flow to flow along(perpendicular to) the isobath. When crossing the isobath, the ITs are generated by the interaction of the barotropic tide and the topography, resulting in the increase of the tidal energy in the winter half year. 展开更多
关键词 internal tide seasonal variation EDDY northeast of Taiwan
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基于非结构化的海洋动力模式FVCOM的北印度洋海域数值模拟
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作者 阮宗利 徐丹亚 +4 位作者 王际朝 庄展鹏 吴国丽 张艳华 纪艳菊 《实验技术与管理》 CAS 北大核心 2022年第5期21-28,34,共9页
使用FVCOM对北印度洋海域进行了数值模拟,并对算例的构建过程做了详细的描述。模式中加入了TPXO 7.2的潮位驱动和ERA5的风场强迫,并将FVCOM中输出的水位SSH与国家海洋科学数据中心的历史观测数据进行了对比验证。各观测站的预测与实测SS... 使用FVCOM对北印度洋海域进行了数值模拟,并对算例的构建过程做了详细的描述。模式中加入了TPXO 7.2的潮位驱动和ERA5的风场强迫,并将FVCOM中输出的水位SSH与国家海洋科学数据中心的历史观测数据进行了对比验证。各观测站的预测与实测SSH时间序列的对比曲线和RMSE、RRMSE、相关系数等结果表明,该区域的FVCOM数值模拟是很有效的,并且是高精度的,获得的最小RMSE和RRMSE分别为0.09 m和0.02。 展开更多
关键词 海洋数值模拟 FVCOM SSH 风场强迫 潮汐驱动
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An efficient parallel algorithm for ocean circulation numerical model based on irregular rectangle decomposition scheme
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作者 zhuang zhanpeng YUAN Yeli +2 位作者 ZHANG Jie HAN Lei YANG Jungang 《Acta Oceanologica Sinica》 SCIE CAS CSCD 2016年第5期18-23,共6页
A parallel algorithm of circulation numerical model based on message passing interface(MPI) is developed using serialization and an irregular rectangle decomposition scheme. Neighboring point exchange strategy(NPES... A parallel algorithm of circulation numerical model based on message passing interface(MPI) is developed using serialization and an irregular rectangle decomposition scheme. Neighboring point exchange strategy(NPES) is adopted to further enhance the computational efficiency. Two experiments are conducted on HP C7000 Blade System, the numerical results show that the parallel version with NPES(PVN) produces higher efficiency than the original parallel version(PV). The PVN achieves parallel efficiency in excess of 0.9 in the second experiment when the number of processors increases to 100, while the efficiency of PV decreases to 0.39 rapidly. The PVN of ocean circulation model is used in a fine-resolution regional simulation, which produces better results. The capability of universal implementation of this algorithm makes it applicable in many other ocean models potentially. 展开更多
关键词 irregular rectangle decomposition scheme message passing interface(MPI) neighboring point exchange strategy data communication
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不同层结条件下海浪生湍流混合特征分析及其对上层海洋的影响
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作者 庄展鹏 袁业立 《海洋科学进展》 CAS 2024年第3期437-451,共15页
上层海洋混合过程的动力学研究和数值模拟一直是海洋和气象学家关注的重点之一,其中上层海洋垂向混合参数化方案的不准确直接影响海洋模式的模拟效果。风生海浪对海气相互作用以及上层海洋的内部混合都起到极为重要的作用。本文基于包... 上层海洋混合过程的动力学研究和数值模拟一直是海洋和气象学家关注的重点之一,其中上层海洋垂向混合参数化方案的不准确直接影响海洋模式的模拟效果。风生海浪对海气相互作用以及上层海洋的内部混合都起到极为重要的作用。本文基于包含垂向层结效应的海浪生湍流混合系数理论模型,开展不同层结条件下海浪生湍流混合系数的分布变化特征分析。构建了一维理想解析实验和准全球算例,结果表明,在100 m以浅的上层海洋中,混合层深度与上述混合系数呈现较为显著的负相关关系,当跃层或混合层深度较大时能够显著增强垂向混合过程,进而使表层暖水下降至更深的位置,加深混合层深度模拟结果。主要原因是由于深跃层条件下表层的层结效应较弱,因而对混合的抑制作用较小。此外,在准全球算例中海浪生湍流混合方案可显著提高海洋环流模式对上层海洋温度结构的模拟能力,模式对跃层处WOA13实测数据的模拟精度最高可提升60%以上。 展开更多
关键词 海浪生湍流混合 垂向层结条件 海洋环流数值模拟 跃层深度
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