温跃层

wēn yuè céng
  • thermocline
温跃层温跃层
温跃层[wēn yuè céng]
  1. 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。

    The correlation analysis 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 .

  2. 结果表明:(1)以水温为主要分析指标,调查海区自上而下(0~500m层)可分为上匀和层、温跃层、中层冷水和下匀和层;

    The results indicate that : ( 1 ) The water column ( 0 ~ 500m ) can be roughly divided into four layers , i. e. , the upper homogeneous layer , the thermocline , the middle cold water and the lower homogeneous layer .

  3. 潮汐作用使得叶绿素最大值的深度存在周期性垂直移动.叶绿素A最大值层厚度与温跃层强度具有密切的反相关关系。

    The thickness of the chlorophyll A maximum layer was contrarily closely related to thermocline strength .

  4. 海洋中温度的垂直结构大体可以分为三层:上混合层、温跃层和底层弱垂直温度梯度层。

    The vertical temperature structures of the ocean generally can be divided into three layers : the surface mixed layer , the thermocline and the layer with weak vertical temperature gradient .