浮力通量 meaning in Chinese
buoyance flux
Examples
- The mld of the ocean near the equator from 10 ? s to 10 ? n are less than 50 m and have no evident seasonal variability
而在10 s 10 n之间的赤道附近海域，因风应力和净热通量的季节变化不大，且该区降水量较大，浮力通量增加， mld较浅，低于50米，且没有明显的季节变化。 - The understanding of the effects of atmospheric forcings , including mainly the surface wind stress , net heat flux and buoyant flux , on the dynamical and thermal structure of the ocean surface mixed layer necessitates a proper knowledge of the mechanisms and influences of the different turbulent mixing processes involved in the upper ocean
海洋上混合层的动力学和热力学结构特征主要受到海表风应力、净热通量和浮力通量的影响，而混合层的形成与维持依赖于混合层内的湍流生成和湍流垂向混合。 - The methods reported by g . s . young in 2000 , are applied on sea surface sar images featured by three dimensional convective cells . then the following parameters are retrieved from sar images : the characteristic wave length of three dimensional convective cell , the mabl depth , the vertical convective scale velocity , the surface buoyancy flux , obukhov length and the stability correction factor for sar derived sea surface wind speed
针对海洋大气边界层中三维对流涡旋sar图像，用g . s . young在2000年发表的方法，反演三维对流涡旋的特征长度、海洋大气边界层高度、以及海洋大气边界层垂直对流尺度速度、表面浮力通量、海面风速稳定性校正因子和obukhov长度。