×

热收支 meaning in English

heat budget

Examples

  1. Annual heat budget
    热收支
  2. 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。
  3. 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。
  4. The results demonstrate that the upper limit of permafrost in this area had declined from 1970s to the middle phase of 1990 , and permafrost has appeared degenerate tendecy , but since middle 1990s , permafrost have a stable state ; ground temperature of roadbed near the earth surface is higher than that of the natural ground , thawing time of roadbed near the earth surface is longer than that of the natural ground , the heat income within the permafrost is greater than the heat release from the permafrost during anannual period , the heat accumulation within the permafrost is temporarily appeared as temperature rising , but with the heat accumulation within permafrost growing up year by year , permafrost temperature will become higher gradually , and strong thawing of permafrost could be happened in the region
    结果表明:风火山地区从20世纪70年代到90年代中期冻土上限下降,冻土出现退化现象,从90年代至今冻土趋于稳定;路基近地表地温明显高于对应天然地表下的地温,路基近地表经历的融化期长于对应天然地表,进入多年冻土区的热收支也呈现出吸热明显大于放热的周期性变化,进入多年冻土的热积累暂时以增高地温耗热为主,但随着冻土吸热量的逐年积累、冻土温度的不断升高,本区冻土可能发生强烈融化。
  5. 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。
More:   Next

Related Words

  1. 收支状况
  2. 收支对照表
  3. 劳务收支
  4. 辐射收支
  5. 收支顺差
  6. 养分收支
  7. 收支相等
  8. 现金收支
  9. 收支图
  10. 收支机构
  11. 热收缩效应
  12. 热收缩应力
  13. 热寿命
  14. 热受体
PC Version

Copyright © 2018 WordTech Co.