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本文分析了渤海、黄海、东海海面热量平衡诸分量及其总和的季节变化,结果表明,进入海面的太阳总辐射是海洋从海面得到热量的主要来源;海洋从海面失去热量的主要原因,在黑潮海域是海面蒸发潜热耗失引起的,在近海海域,春、夏季海面有效回辐射耗热超过蒸发耗热,秋冬季相反。海气之间的感热交换量较小,冬季较明显。结果还指出,在3—8月海洋计温期,海洋从海面得到热量,在9—翌年2月海洋降温期,海洋从海面失去热量。
The results show that the total solar radiation entering the sea surface is the main source of the ocean’s heat gain from the sea. The main reason why the ocean loses heat from the sea surface is that in the black The tide sea area is caused by the loss of latent heat of evaporation from the sea surface. In the offshore waters, the effective heat radiation of the sea surface in spring and summer exceeds the evaporative heat consumption, contrary to the autumn and winter. Air-sea heat exchange between the smaller, more obvious in winter. The results also point out that during the March-August ocean temperature period, the ocean receives heat from the sea surface and the ocean loses heat from the sea during the ocean cooling period in February of the next year.