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1)  circumpolar water mass
绕极水团
2)  Circumpolar Deep Water
绕极深层水
1.
Features and Spatial Distributions of Circumpolar Deep Water in the Southern Indian Ocean and Effects of Antarctic Circumpolar Current;
南印度洋绕极深层水的性质和空间分布以及南极绕极流的作用
2.
Features of Circumpolar Deep Water, Antarctic Bottom Water and their movement near the Prydz Bay;
普里兹湾附近绕极深层水和底层水及其运动特征
3)  Antararctic Circumpolar Deep Water
南极绕极深层水
4)  To roll or coil into a ball.
把…绕成线团
5)  Antarctic circumpolar current
南极绕极流
1.
The sea surface variability of Antarctic Circumpolar Current (ACC) is investigated from 8 years of merged Topex/Poseidon data (January 1993 to December 2000).
采用TOPEX/POSEIDON(T/P)卫星高度计 1 993年 1月— 2 0 0 0年 1 2月海面高度数据 ,研究包含了整个南极绕极流流系 (40°— 6 0°S)的海面高度低频变化。
6)  Antarctic circumpolar wave
南极绕极波
1.
The Antarctic circumpolar wave(ACW) has become a focus of the air-sea coupled Southern Ocean study since 1996,when it was discovered as an air-sea coupled interannual signal propagating eastward in the region of the Antarctic Circumpolar Current(ACC).
南极绕极波(ACW)是近10年来海洋和大气科学领域研究的重要内容之一,其特征表现为一种海气耦合的年际信号在南大洋的明显东向传播。
2.
Long-term trend,interdecadal jump and cycles of AAOI and Uaaoi as well as the effect on the Antarctic circumpolar wave are discussed.
用1951年1月~2002年12月共624个月的海平面气压、温度和850hPa西风的NCEP再分析资料,分析定义了南极涛动指数(简称AAOI)和850hPa的南极涛动西风指数(简称Uaaoi),并讨论了它们的长期变化趋势和年代际跃变及其对南极绕极波的影响。
补充资料:南极绕极流
      见南大洋。
  

说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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