结果表明,春季从加里曼丹岛至巴拉望岛以西附近海区的上层流场基本表现为反气旋性弯曲(涡),南沙群岛海区北部的深层水大体呈偏东向流动;

结果表明,春季从加里曼丹岛至巴拉望岛以西附近海区的上层流场基本表现为反气旋性弯曲(涡),南沙群岛海区北部的深层水大体呈偏东向流动;的英文翻译

基本释义

• Computational results show that, in spring, it is basically anticyclonic meander (eddy) in the upper current field to the west of the adjacent sea area from Borneo to Palawan Island, while the flow in the deep layer is eastward by and large in the north of the Nansha Islands sea area.