| 1. | In the open ocean above the deep sea bed, the vertical structure of the water mass is characterized by the presence of one of more thermoclines .
处于深海床之上的外洋中，水体的垂直结构的特点是存在一个或一个以上的温跃层。 |
| 2. | The model is divided into three boxes according to the depths of thermocline and eupthotic layer
模型采用箱式模型，将模型根据温跃层与真光层位置从上至下分为三个箱子。 |
| 3. | Among them the analysis of thermocline distributional pattern and the influence factor of scs are the core contents
其中以探讨分析南海温跃层分布状况、分布规律及影响因素为核心内容。 |
| 4. | The stratification is very obvious in the vertical profiles of chlorophyll and dissolved oxygen , with high content in the subsurface layer when thermocline exists
在温跃层存在季节，黄海冷水团水域的叶绿素和溶解氧含量出现次表层最大值现象。 |
| 5. | This study has done a large amount of work on the thermocline statistical method , the result verification and plotting , and has brought forth some new ideas
南海温跃层的统计分类方法是在各种温跃层类型划分理论的基础上，结合南海温度剖面结构特点确定的。 |
| 6. | Compared with the time of the thermocline in huanghai , east china sea , the thermocline of scs takes shape a month early , and no thermocline period takes place a month later
与黄、东海温跃层相比，南中文摘要海温跃层形成规模的时间早一个月，晚1个月进入无跃层期。 |
| 7. | The approach adopted in the thesis was proven to be successful , and can be generally applied to study the mixing and stratification process in other shallow seas and shelf oceans
且完整、全面地反映了整个渤海温跃层空间分布特征，及其随时间演变的细致过程。这种方法具有适普性，可用于其它陆架海域混合和层化的研究。 |
| 8. | The subduct ion sign propagates toward the western tropical pacif ic ; and the decadal sign from the western tropical pacific propagates toward north - east . they meet at about 160 meter in depth in subtropical pacific
从北太平洋窗口区潜沉的海温年代际信号沿西南路径传播到副热带地区，在温跃层160m上下与热带西太平洋向东北传播的海温异常信号会合。 |
| 9. | Because in july the sun ' s radiation is lower in scs than east china sea and the air temperature difference of winter and summer is smaller , the thermocline intensity is weaker in scs than in huanghai and east china sea
由于夏季日辐射相对低、冬夏季温差小等原因，夏季南海温跃层强度较黄、东海弱。本研究工作在温跃层统计方法的确定、结果验证上作了大量工作，并有所创新。 |
| 10. | The correlation analysi s between sst and sea surface height , heat content and depth of thermocline also shows the important role of ocean dynamic processes in some regions , besides the influence of heat exchange between air and sea
Sst与海表面高度、热含量、温跃层深度等的相关分析也表明，在某些区域，除受海洋-大气之间热交换的影响外，海洋动力过程对sst的影响也占重要地位。 |
