1)Kuroshio[英][ku'r?u?i:?u][美][k?'ro?i,o]东海黑潮
1.The study of the temporal and spatial characteristics of western boundary current East of Ruykyu submarne ridge and the transport of Kuroshio in East China Sea;琉球群岛以东的西边界流与东海黑潮流量时空特征的研究
2.Numerical Analysis of Kuroshio Chaos;东海黑潮混沌特征的数值分析
3.Using semidifferential stripping technique combined with pre-equibrium complex-ometric titration, the apparent copper complexing capacity (AXuCC) of seawater and the conditional formation constant (Kc) of copper-natural organic ligand of 65 seawater samples collected in the Kuroshio area in the East China Sea "in 1989 were determined.用半微分极谱溶出技术与预平衡络合滴定相结合的方法,对东海黑潮海域1989年三个航次65个海水样品的表观铜络合容量(ACuCC)及条件形成常数(K_c)进行了测定。
英文短句/例句
1.The Kuroshio East of Taiwan Island and in the East China Sea in the Winter of 19971997年冬季台湾岛以东与东海黑潮
2.Dynamics of Sea Level Variation in the North Pacific Ocean, Kuroshio Region of East Sea of China and Kuroshio Extension北太平洋、东海黑潮及黑潮延伸体海域海平面变化机制研究
3.EDDY ENERGY TRANSPORT OF WAVE CYCLONES OVER KUROSHIO AREA东海黑潮上空气旋波的扰动能量传输
4.DISTRIBUTION OF ZOOPLANKTON IN THE FRONTAL EDDY REGION OF THE KUROSHIO IN THE EAST CHINA SEA东海黑潮锋面涡旋区浮游动物的分布
5.Diagnosis of the Kuroshio in the East China Sea along the PN-line with Geostrophic Empirical Mode Method;PN断面东海黑潮的地转经验模态分析
6.Variations of Sea Surface Temperature over Kuroshio in the East Sea and Its Relationship with El-nino and Global Warming东海黑潮海表温度变化及其与厄尔尼诺和全球变暖的关系
7.THE INTERPRETATION ON THE SURFACE TEMPERATURE FRONTS OF KUROSHIO IN THE EAST CHINA SEA USING NOAA IR DATA利用诺阿卫星红外信息对东海黑潮表层温度锋的解译
8.The Seasonal and Interannual Variation of the Upper Kuroshio Circulation in the East China Sea and Its Relationship with Local Wind Stress;东海黑潮上层环流季节、年际变化与局地风应力的关系
9.A SIMPLE MODEL FOR THE THERMAL STRUCTURE OF KUROSHIO EAST OF TAIWAN台湾以东海域黑潮热结构的一个简单模型
10.The northeast of the Taiwan Island is due to the Kuroshio and its topography.台湾岛东北海域内潮响应强烈主要是受黑潮锋和地形的影响。
11.The water in the west side of Tsushima Warm Current is a mixed water of East China Sea and the water in its east side is a branch water coming from the Kuroshio.对马暖流西侧的水体是东海混合水,而其东侧为黑潮分支。
12.A Correlation Study between SSTA over the Winter Kuroshio Area and East Asian Circhlation and the Climate of China in Summer;冬季黑潮海温与后期夏季东亚大气环流及我国气候的关系
13.In the southeast of the South China Sea, there maybe existed the water from the Sulu Sea, and its temperature and salinity characteristics were similar to that of the Kuroshio water near the Luzon Strait.在南海东南部可能有来自苏禄海的海水 ,其温、盐度特征类似于吕宋海峡中的黑潮水
14.Baroclinic Rossby Wave and the Kuroshio East of Taiwan;斜压Rossby波与台湾以东黑潮
15.THE KUROSHIO IN LUZON STRAIT AND ITS TRANSPORT DURING SEPTEMBER 19851985年9月的吕宋海峡黑潮及其输送
16.The Variability of the Kuroshio and Its Effects on the Current in the Taiwan Strait;黑潮变化及其对台湾海峡流动的影响
17.The red tides covering large areas mainly happened in East Sea, Bo Sea and Yellow Sea.大面积赤潮主要集中在东海、渤海和黄海海域。
18.The Study of the Tidal Numerical Simulation with Assimilation and the Tidal Dissipation in the Bohai Sea, Yellow Sea and East China Sea渤黄东海潮波同化数值模拟和潮能耗散的研究
相关短句/例句
Kuroshio in the East China Sea东海黑潮
1.Diagnosis of the Kuroshio in the East China Sea along the PN-line with Geostrophic Empirical Mode Method;PN断面东海黑潮的地转经验模态分析
2.Kuroshio in the East China Sea is studied as an important impact on the East China Sea circulation.本文的研究区域为东海黑潮。
3)the Kuroshio in the East China Sea东海黑潮区
4)main part of the Kuroshio东海黑潮主段
1.In this paper,a physical pattern of subcirculation system in the main part of the Kuroshio in the East China Sea is suggested by analyzing different survey data,and the subcirculation system is a double-loop circulation structure consisting of a relatively stable main stream of the Kuroshio,a frequently occu-ring right side countercurrent and a conditionally occurring outer shelf countercurrent.通过对多种调查资料的综合分析,提出了东海黑潮主段子环流系统的物理模型,它是由较稳定的东海黑潮主段、经常出现(大概率)的右侧逆流和有条件出现(小概率)的外陆架逆流所构成的一个双环环流结构。
5)Kuroshio area of the southern East China Sea东海南部黑潮区
1.Based on the hydrographic data of five cruises in the Kuroshio area of the southern East China Sea in spring from 1988 to 1996, the geographical distribution of vertical distribution types of temperature and salinity in the area are analyzed, and the causes of the reverse phenomenon of temperature and salinity in spring are discussed in detail.用１９８８～１９９６年在东海南部黑潮区共５个航次的春季水文观测资料，分析了该海区温、盐度垂直分布类型的地理分布，讨论了春季温、盐度逆转现象的形成原因。
6)kuroshio upper circulation in the ECS东海黑潮上层环流
延伸阅读
黑潮黑潮KuroshioCurrent北太平洋副热带总环流系统中的西部边界流。黑潮具有流速强，流量大，流幅狭窄，延伸深邃，高温高盐等特征为其特色。潮即水流，因其水色深蓝，远看似黑色，因而得名。黑潮是由太平洋北赤道流在菲律宾群岛以东向北流动的一个分支延续而来。其源地位于中国台湾省东南和巴士海峡以东海域。它沿台湾东岸北上，通过苏澳和与那国岛之间的水道流入东海。主轴指向东北，在陆架外缘和陆坡之间流动。当它在奄美诸岛西北分出对马暖流分支后，转向东流通过吐噶喇海峡北部流出东海，进入日本以南的太平洋海域；再沿日本诸岛沿岸流向东北，在本州铫子附近离开陆坡向东流去，成为黑潮续流。约至东经165°处再延伸为北太平洋流。狭义的黑潮系指自台湾东南海域至铫子一段紧沿陆坡流动的高速带状水流广义的黑潮流系则包括黑潮续流。吕宋岛以东，北向最大流速约80～100厘米／秒。在巴士海峡和台湾岛南端及东岸最大流速约150厘米／秒或以上。台湾以东，黑潮流幅约125～170千米，向北流幅逐渐变窄；离岸距离为60～100千米。流轴上最大流速平均约为95厘米／秒。流量（相对于800分巴面）的年际变化很大，在（19～42）×106米3／秒之间。东海中的黑潮是黄、东海流系的主干，其影响还远及南海。黑潮在自西向东流动中，沿途还汇合了其他水体，到达日本以南时，流速增强，流量增大，途径变异也最复杂。熊野滩以南经向断面上的地转流速分布显示了黑潮的典型结构。表层最大流速可达190厘米／秒以上，流轴（流速＞50厘米／秒）宽约125千米，深约600米。流量约为71×106米3／秒。约在北纬35°处，黑潮离开日本海岸后分为两支，其一为续流主干，向正东流动，保持狭窄强流性质，直到东经160°附近。它在东经150°附近又分出一支，为黑潮逆流几乎沿椭圆形途径向琉球群岛和台湾岛方向流动。另一支为续流分支，流向东北，直到北纬40°处又转向东流。这一分支与其西、北两侧的亲潮，形成了寒暖两流系十分显著的锋面。这里渔业资源很丰富。黑潮的途径和流轴位置，流幅和伸展深度，流速、流量以及热盐结构等等，都无时不在变化之中。变化周期从十几年、几年直到几小时，甚至更长和更短。其中，日本以南的黑潮，由于其途径曾多次出现周期为几年或十几年的大弯曲现象（日本学者称为大蛇形），并在远州滩外伴生大冷水团。黑潮大弯曲现象的持续性非常突出。在1934～1980年的47年间竟有25年黑潮途径发生弯曲。
