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heat budget中文是什么意思

  • 热衡算
  • 热量衡
  • 热量平衡
  • 热量收支
  • 热收支
  • 热总量

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  • 例句与用法
  • Annual heat budget
    年热收支量
  • 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。
  • It can be found that a great quantity of vapor is transported to atmosphere from arctic ocean open sea in summer , which is very important to concerns on season change of heat budget on arctic ocean
    由此可见,在北冰洋夏季,无冰海面有大量的水汽向大气输送,这对研究北冰洋地区大气边界层的季节变化过程是至关重要的。
  • 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。
  • In order to study the variation characteristics of heat flux at nansha and xisha islands in the south china sea , the observational data from the ocean stations are calculated to obtain air - sea heat exchanges and the annual circulation of heat budget around the summer monsoon onset in 1998
    摘要为探索西沙和南沙海气热通量时间演变特征,用海洋站观测资料计算了1998年南海夏季风爆发前后,海气界面热量交换值及海面热收支年循环。
  • 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。
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