ACC:南极绕极流
南极绕极流(Antarctic Circumpolar Current,简称ACC)是环绕南极洲流动的全球最强洋流,因其名称较长,在海洋科学及相关学术领域中常缩写为ACC,以方便书写与交流。这一洋流对全球气候系统和海洋环流具有重要影响,是极地研究的关键对象之一。
Antarctic Circumpolar Current具体释义
Antarctic Circumpolar Current的英文发音
例句
- The Antarctic Circumpolar Current(ACC) in this area is wind-induced and is also forced by density field.
- 该海区的南极绕极流(ACC)既是风生的,也受到密度场的影响。
- Study of Interaction between Antarctic Circumpolar Current(ACC) and Antarctic Coastal Current in the Indian Section of the Southern Ocean
- 南大洋印度扇形区南极绕极流(ACC)和南极沿岸流的相互作用研究
- Residual-mean solutions for the Antarctic Circumpolar Current(ACC) and its associated overturning circulation.
- 南极环极环流和反环流的残差-平均解。
- Simulations of magnetic fields generated by the Antarctic Circumpolar Current(ACC) at satellite altitude : Can geomagnetic measurements be used to monitor the flow?
- 在卫星高度南极周围电流所产生磁场的模拟:地磁测量能用监视器流的吗?
- Features and Spatial Distributions of Circumpolar Deep Water in the Southern Indian Ocean and Effects of Antarctic Circumpolar Current(ACC)
- 南印度洋绕极深层水的性质和空间分布以及南极绕极流(ACC)的作用
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