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| 1 | 北太平洋西边界流的低频变化特征显示文摘基于日本气象厅长时间序列的温、盐度再分析资料,利用动力计算方法分析了北太平洋西边界的北赤道流及其下游黑潮和棉兰老流流量的年际和年代际变化,并探讨了北赤道流变化的可能原因。结果表明,北赤道流和黑潮具有比较一致的年际和年代际变化,均在1976年前后发生了一次气候跃变,之后有长期偏强的趋势,而棉兰老流的年际和年代际变化则有所不同。特别是,北赤道流1976年之后增加的流量似乎大多进入黑潮,而流入棉兰老流的流量则减少。进一步的分析还表明,西传的Rossby波和棉兰老冷涡的变动可能对北赤道流的年际变化有重要影响。 | 蔡榕硕 齐庆华 张启龙 | 2013 | 海洋学报2013，35，1： | 7 |
| 2 | Physical oceanography of the Caroline M4 seamount in the tropical Western Pacific Ocean in summer 2017显示文摘Physical oceanography plays an important role in the formation of submarine sediments,and the distribution of nutriments and biocenoses in seamounts.The M4 seamount is located in the Caroline Island Ridge of the Western Pacific Ocean.The physical properties around M4 seamount are preliminarily analyzed based on the in-situ data obtained in summer 2017 in Caroline M4 seamount and open-sourced data.We found that the water in the upper 200 m is controlled by the westward North Equatorial Current(NEC),while the water between 300-1000 m is dominated by the eastward North Equatorial Undercurrent(NEUC).The current direction fluctuates significantly below 300 m at upstream stations.At the same depth of the lee sides,the current direction changes with the distance from seamount.These are likely caused by the obstacle of M4 seamount.The calculation results show that there is an anticyclonic cap above M4 seamount caused by tidal rectification.Tidal currents in M4 seamount are squeezed by the topography and amplified,and the amplified tidal currents play a dominant role in M4 seamount.First,the circulation system generated by the interaction of the amplified tidal current and M4 seamount drives the upward/downward movement of the isotherms.Secondly,the thickness of the surface turbulent layer is changed with the tidal phase.Thirdly,high turbulent diffusivities are found in the bottom of M4 seamount,and these are most likely attributed to the turbulent mixing induced by the mutual effect between semidiurnal tidal currents and steep bathymetry.This article of physical oceanography provides scientific basis for further analysis of the distribution of biological community and deposition mechanism in M4 seamount. | Xingyu SHI Zhenyan WANG Haijun HUANG | 2021 | Journal of Oceanology and Limnology2021，39，5： | 3 |
| 3 | 越南东部海域一个气旋涡的特征分析显示文摘为探究越南东部海域中尺度涡的表层特征和垂向结构,基于卫星高度计资料,采用涡旋自动识别方法对该区域一个中尺度涡的演变和移动特征进行分析,同时结合走航调查资料对该涡旋的垂直结构进行了分析。结果表明:该涡旋总体向西北方向移动,其速度不具有一阶斜压罗斯贝波的传播特性;涡旋会造成其内部温度和盐度等值线的抬升,并引起涡内温盐异常,在25~75m深度分别存在温度负异常的'冷核'结构和盐度正异常的'高盐核'结构;与气候态相比,涡旋内部温跃层深度变浅,厚度变小,强度变大;涡旋对上混合层的影响很小,没有造成明显的温盐异常;基于实测流场与由温盐诊断的斜压流场的共同数据可知,涡旋内部流场呈明显气旋式环流,涡中心流速接近0,边缘附近流速最大。 | 胡冬 陈希 李妍 毛科峰 张守业 | 2017 | 解放军理工大学学报(自然科学版)2017，18，2： | 1 |
| 4 | 棉兰老隆起三维结构特征及变化规律显示文摘利用日本气象厅(JAMSTEC)所提供的Argo格点温盐资料,系统地研究了棉兰老隆起(Mindanao Dome;MD)的三维结构及变化特征。结果表明,MD的水平位置大致在5°N^10°N,127°E^145°E范围内1个纬向延伸的狭长带状结构。其垂向范围大致在50~600m之间,强度在次表层100~200m附近最显著。温盐结构表现为深层低温、低盐水向上涌升增强,温跃层深度变浅,上混合层厚度变薄的特征。功率谱分析结果表明,MD具有明显的季节变化信号,表现为冬强秋弱,具有一年和半年的较为显著的变化周期。在El Ni珘no期间,MD的次表层水温明显下降,MD增强。局地风场对MD的变异起着重要作用,MD的变化与该处风应力旋度的变化的相关系数为-0.346。MD的变化和暖池的变化具有较好的负相关关系,在暖池发展比较充分时候,由于其暖水范围增大,暖水厚度增加,在某种程度上会抑制MD的发展;反之亦然。 | 徐智昕 周慧 郭佩芳 侍茂崇 | 2014 | 中国海洋大学学报(自然科学版)2014，44，1： | 1 |
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