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北印度洋的英文

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"北印度洋"怎么读用"北印度洋"造句

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  • indian ocean

例句与用法

  • Those unique dynamics have significant effects on the heat budget and sst of the northern indian ocean
    这些特点是印度洋与其他大洋不同之处,对北印度洋的热收支和sst有重要影响。
  • The quantitatively studies of the heat budget in the northern indian ocean are given , focusing on the heat transport and the mechanisms involved in , based on the heat budget equation and data from the ocean model
    根据热量收支方程和海洋模式资料,定量估计了北印度洋的热量收支,重点研究了经向热输送及其影响机制。
  • Further more , the sst warming twice in one year in the northern indian ocean , the mixed layer deepening in the central arabian sea during summer , as well as the equator jet occurred only in transient seasons are all noteworthy
    不仅如此,北印度洋sst在一年有两次增暖、夏季风期间阿拉伯海中部混合层的加深,以及季风转换其间赤道急流的存在等也是季节变化尺度上引人注目的现象。
  • Based on the observation data such as coads and soda , the main climatological features of the tropical indian ocean and relationships of sea surface temperature ( sst ) , heat budget with ocean dynamics and thermodynamics processes are analyzed ; the seasonal and interannual variability of the tropical indian ocean are well simulated using a ocean general circulation model ; based on the thermal equation and model output data , the variation mechanism of sst and heat budget are investigated in the tropical indian ocean ; besides , the effect of seasonal variation of wind stress , ekman pumping and horizontal diffusivity on the ocean current and heat budget are studied , using both ideal model and complex model
    本文根据coads 、 soda等实际观测资料,较全面的分析了热带印度洋主要的气候特点,并研究了海表面温度( sst ) 、热收支与海洋动力、热力过程的联系;利用全球海洋环流模式较好地模拟出热带印度洋的季节和年际变化;基于热力学方程和海洋环流模式输出结果,探讨了热带印度洋sst和北印度洋热量收支的季节和年际变化机制,进一步揭示了海洋动力过程在北印度洋热平衡中的重要作用;在此基础上,利用理想化的数值试验与数值模拟结果相结合的方式,证实了风应力的季节变化和ekman抽吸,以及水平热量扩散系数对北印度洋海洋环流和热收支的影响。
  • All these results confirm the important of wind in meridional circulation and heat transport . based on mom2 model , a rectangular basin model with ideal w ind stress and other ideal conditions is designed to study the main processes and dynamical mechanism in setting the depth of cross - equator flow . the effects of horizontal diffusivity , seasonal variations of
    我们还通过全球海洋环流模式,进一步证实了风应力的季节变化在北印度洋热收支、 sst以及海洋环流变化中的作用:即包含风应力的季节变化将使长期平均的sst降低,海面净热通量增加。
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