黄海冷水团

底层水团配置为黑潮次表层水团（V），黄海冷水团（Ⅵ），台湾暖流水（Ⅲ）等水团。

In the surface layer and Kuroshio Subsurface Water Mass ( V ), Yellow Sea Cold Water Mass ( VI ), Taiwan Warm Water Mass ( Ill ) in the bottom layer .

苏北沿岸水、长江冲淡水及黄海冷水团对影响区域TOC的含量均起到稀释作用。

Northern Jiangsu offshore currents , Changjiang diluted water and cold water mass from Yellow Sea had dilution effects to TOC concentrations in the area .

利用PCR-DGGE技术对长江口外低氧区海域和黄海冷水团海域的细菌群落组成进行了分析。

Bacterial community composition and predominant bacteria were analyzed by PCR-denaturing gradient gel electrophoresis ( DGGE ) in the Yellow Sea Cold Water Mass ( YSCWM ) .

主因子3为Protelphidiumtuberculatum组合，代表外延的古黄海冷水团；

Factor 3 ( Protelphidium tuberculatum assemblage ) represented the extension paleo-cold-water-mass of the Yellow Sea ;

黄海冷水团（YSCWM）及其环流是中国近海最突出的物理现象之一。

The Yellow Sea Cold Water Mass ( YSCWM ) and its circulation are one of the most outstanding phenomena in the China Sea .

对从黄海冷水团附近海域的底泥中分离到的一株新型海洋趋磁细菌YSC-1的磁特性进行了分析。

Magnetic properties of a novel marine magnetotactic bacterium YSC-1 , which was isolated from sediments near cold mass of the Yellow Sea , was analyzed in this study .

黄海冷水团水域水层&底栖耦合生态系统建模研究

Pelagic-benthic Coupling Ecosystem Modeling Research in the Yellow Sea Cold Water Mass

夏季北黄海冷水团多年变化特征分析

Analyses of the variational characteristics of the North Huanghai Sea cold water mass

黄海冷水团声层析监测数值模拟

Numerical Simulation of Acoustic Tomography for Monitoring the Yellow Sea Cold Water Mass

黄海冷水团向东南方向伸展。

The Huanghai Sea Cold Water extends southeastward .

黄海冷水团夏季叶绿素垂向分布结构的影响机制

Effect mechanisms on Chlorophyll-a vertical distribution in the summer within Yellow Sea cold water mass

黄海冷水团水域大型底栖动物生物量秋季比较大，而小型底栖动物生物量存在春、秋两季的高值。

The biomass of macrobenthos is higher in Autumn while that of meiobenthos tends to be higher in both Spring and Autumn .

北黄海冷水团环流结构探讨&潮混合锋对环流结构的影响

A study of the circulations of the northern Yellow Sea cold water mass ( nyscwm )── effects of tidal mixing on them

本文将简正波波数层析法用于冷水团监测，并对简正波波数层析用于反演黄海冷水团声速剖面进行了数值模拟。

A perturbation inversion method is used for inversing the sound speed profile ( SSP ), with empirical orthonormal functions ( EOF ) applied to reduce parameter search space .

黄海冷水团内部结构复杂，黄海的陆架锋对黄海水文要素的分布变化有重要影响；

The interior structure of Yellow Sea Cold Water Mass is very complexi ; the continental shelf fronts have an important influence on the distributions and variations of hydrographic elements ;

将北黄海冷水团强度预报作为示例，给出了筛选因子及建立判别式的全过程。

A multistage strength forecast of the Northern Huanghai Sea Cold Water Mass is taken as an example . The whole process of sifting factors and establishing discriminant is given .

首先根据黄、东海生态综合调查资料和前人的研究成果，分析了黄海冷水团水域水层生态系统的基本特征。

The basic ecosystem characters in the YSCWM are outlined according to former studies and observation in the Yellow Sea and the East China Sea in the first part of this paper .

黄海冷水团及邻近海域小型底栖动物多样性及其环境效应南黄海小型底栖动物分布及其与环境因子的关系

Diversity Pattern and Environmental Response of Meiofauna in China Seas with Special Reference to the Yellow Sea Cold Water Mass Relationship between Distribution of Meiofauna and Environmental Factors in Southern Yellow Sea

黄海冷水团是一个高盐水团，它在5个水团中保守性最强，而从5月至8月范围较大。

The Yellow Sea Cold Water Mass is a high salinity water mass , which is the strongest of the five in conservative property and larger in range from May to August .

东暖舌是在黄海海槽的一逆时针方向的环流的作用下形成，该环流是由夏季和秋季黄海冷水团的温度锋所诱发形成的。

The eastern warm tongue develops under the influence of an anti-clockwise circulation which is induced by the temperature front of the Yellow Sea Cold Water Mass ( YSCWM ) in summer and autumn .

通过建立垂向的一维对流-扩散模型，估算了温盐跃层以下水体（即黄海冷水团内部）由底部向上的垂直涡动扩散系数以及相应的营养盐输送通量。

Similarly , based on a vertical one-dimentional advection-diffusion model ( neglecting advection ), the vertical eddy diffusion coefficients below the thermocline ( within the Yellow Sea Cold Water Mass , YSCWM ) are estimated .

结果表明，黄海冷水团的分布范围具有比较明显的年间变化，强年的相对体积约为弱年的2.2倍。

The results show that the distribution range of the Huanghai Sea Cold Water Mass has the distinct secular variations and its " relative volume " in the stronger year is 2.2 times that in the weaker year ;

根据历史资料，结合本次研究海区的环境因子特征，将研究海区分为长江冲淡水影响区域、近岸水团区域、黄海冷水团区域及各个水团之间的混合水团（海洋锋）区域。

According to the historical data and the characteristics of environmental factors obtained in this survey , the study area can be divided into 4 districts : Changjiang diluted water area , nearshore water mass area , yellow sea cold water mass area , and mixed water mass area .

春季北黄海西部冷水团强度的年际差异及其预报

The annual variation and its fore-casting of the intensity of cold water mass of the western-north Yellow Sea in spring

黄海中部冷水团影响了悬浮体的水平扩散和垂直扩散。

Cold water mass in the central region of the South Yellow Sea also exert influence on horizontal and vertical dispersion of suspended matter .

这种低频振动在冬季与渤海冰情的变化同步；在夏季与黄海底层冷水团的强弱相关。

The low frequecy Oscillations were related to the anomalies of the ice conditions in the Bohai Sea in winter and to the intensities of the cold water masses in the Yellow Sea in summer .

本文取该二指标的多年距平绝对值的平均值之半作为标准，划分1960&1980年四、五月北黄海西部冷水团的强度（表1）。

In this report , taking the half of absolute values of this two indexes in anomaly of many years as a criterion to divide the intensity of Western-North Yellow Sea Cold Water Mass in April and May , 1960-1980 ( Table 1 ) .

模拟结果还表明，黄海暖流的动力仍然是季风环流，而对黄海冷水团的形成和发展有无动力影响提出质疑。

The simulated result shows that the driving power of the Huanghai Sea Warm Current is monsoon circulation , and therefore the question whether there is some dynamic effect on the formulation and development of the Huanghai Sea Cold Water Mass is deduced .

黄海沿岸浅水区与渤海有相似的热结构，黄海冷水团和黄海暖流对其中央槽深水区的热结构有重要影响。

Except for some similar thermal structure between the Bohai Sea and coastal shallow water zone of the Huanghai Sea , for the thermal structure of deep water area in central trough , the Huanghai Sea Cold Water Mass and the Huanghai Sea Warm Current are two special factors .