The thermalbuoyancy effect of the cooling water is clear in deeper water areas because the heat quantity of the cooling water is diffused at certain depth below water surface.
当水深较大时，温排水热上浮效应明显，温排水的热量仅在水体表层的一定深度内扩散。
2
That extra thermal energy gives the ocean plates more buoyancy as they move farther away from the ridges.
海底板块移动得离中部山脊越远，额外的热能给予板块的浮力就越大。
3
Furthermore, the influence of centrifugal buoyancy on the performance of heat transfer was more distinct in the case of swirling flow existing in the side of larger thermal resistance.