黄海暖流

对黄海暖流形成机理的分析表明，压强梯度力、垂向摩擦力和柯氏力占主要地位。

It is shown from the analysis of formation mechanism that the pressure gradient force , vertically frictional force and Coriolis force play the leading roles in forming the YSWC .

同时，模式很好地模拟了该海域的黑潮、台湾暖流、对马暖流、黄海暖流以及沿岸流等主要环流。

The model has simulated Kuroshio , Taiwan Warm Current , Tsushima Current , the Yellow Sea Warm Current , and Coast Current .

冬季因受黄海暖流及水体垂直混合的影响，此海域表现为大气CO2的强源区。

This area is affected by the Warm Current of Yellow Sea in winter , and it is saturated to the atmosphere CO2 .

此按钮将无法修复丢失黄海暖流，CCC认证，全国人大证书。

This button will not repair missing HWC , CCC , NPC certificates .

钙质超微化石分异度DH以及主要化石种相对百分含量的高值区的主轴线的走向与现代黄海暖流的流路密切相关。

The trend of the main axis of the high-value area of the Shannon-Wiener Index ( D_H ) and the relative Content ( % ) of the principal calcareous nannofossil is closely related to the flow way of the warm current of the Huanghai Sea .

关于黄海暖流某些特征的分析

Analysis on some characteristics of the warm current in the Yellow Sea

冬至初春黄海暖流的路径和起源

On the origin and path of the Huanghai Warm Current during winter and early spring

冬季黄海暖流区的空间变化和年际变化特征

Characteristics of Spatial and Interannual Variation in the Yellow Sea Warm Current Area in Winter

黄海暖流源区海表面温度锋面的结构及季节内演变

Distributions and intra-seasonal evolutions of the sea surface thermal fronts in the Yellow Sea warm current origin area

黄海暖流东西两侧分别为2支向南流动的沿岸流。

On the eastern and western sides of the Huanghai Sea warm current there are 2 branches , flowing southward along the coast .

冬季黄海暖流的诊断计算东海西北部密度流计算和分析

Diagnostic Computation of the Yellow Sea Warm Current in Winter COMPUTATION AND ANALYSIS OF DENSITY CURRENT IN NORTHWESTERN PART OF THE EAST CHINA SEA

经分析发现，这个沉积体系，完全受控于黄海暖流、冷涡及其相关的环流体系。

It is discovered , that sedimentary system have been controled by the Yellow Sea warm current and its derivative ( cold eddy system ) .

黄海暖流从东海向南黄海输送高温高盐水，从而大大改变了冬季南黄海的浮游动物群落结构。

It advects warmer and saltier water from the East China Sea into the Southern Yellow Sea and changes the zooplankton community structure greatly in winter .

太阳辐射、黄海暖流余脉、深层冷水涌升对海洋岛附近海域夏季水温分布与变化的影响

Impact of solar radiation , remanent of Yellow Sea warm current and upwelling of DEEP-COLD-WATER on water temperature distribution and variation around Haiyang island in summer

此外，黄海暖流引起的上升流和垂直混合搅拌驱动的底层补充所输入的营养盐也对生产力的高值起到一定的增强作用。

In addition , the bottom nutrients from upwelling and vertical mixing caused by Yellow Sea Warm Current also played a certain role in enhancing the productivity .

黄、渤海表层沉积物中钙质超微化石分布规律与黄海暖流流路

The Distributive Law of Calcareous Nannofossil in the Surficial Sediments from the Huanghai Sea and the Bohai Sea And Flow Way of Warm Current in the Huanghai Sea

本章通过数值实验来研究双暖舌结构的形成机制及其与黄海暖流的关系。

Numerical experiments based on POM are carried out to study the forming mechanism of this thermal structure and its relation to the Yellow Sea Warm Current ( YSWC ) .

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 .

研究结果更加清晰、形象、直观地展示了黑潮及其向对马暖流的分支，台湾暖流的分叉，和黄海暖流、长江冲淡水及涡旋发达海区的若干主要特征。

The results demonstrate more clearly and directly some main features about the Kuroshio and its branch ( to the Tsushima Warm Current ), the separation of the Taiwan Warm Current , the Huanghai Sea Warm Current , the Changjiang diluted water and the eddy developing area .

南黄海北部细粒沉积物在全新世海泛面之上的稳定堆积，反映了全新世中期最大海泛面以来伴随着黄海暖流的出现在黄海海域现代环流格局的形成并维持至今。

The stable accumulation of the fine-grained sediments above the Holocene maximum flooding surface in the north of the South Yellow Sea have probably indicated the formation of the modern Yellow Sea circulation pattern following the appearance of the Warm Current in the Sea since the middle time of Holocene .

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 .

黄海北部表层水温为北黄海沿岸水（水团）、渤海沿岸水（水团）、朝鲜西部冷水团和黄海暖流余脉所控制。

The surface temperature in the area was controlled by water bodies of coastal water in northern Yellow Sea , coastal water in the Bohai Sea , cold water mass west of the Korea Peninsula and the remainder of the warm current in the Yellow Sea .

这些都表明晚全新世晚期低温、低盐、高营养的黄海沿岸流加强。3.6-1.95kaB.P.碳氧同位素的高值表明这一阶段，研究区主要受高温、高盐、低营养的黄海暖流的影响。

All of this shows that the study area was strong influenced by Yellow sea coast current which has a characteristic of low temperature , low salinity and high nutrient during the late of late Holocene .