热收支的英文

• heat budget

• "收支"英文翻译    expenses and receipts; reven ...
• "年热收支量" 英文翻译 :    a ual heat budget; annual heat budget
• "收支" 英文翻译 :    expenses and receipts; revenue and expenditure; income and expenses 公布收支帐目 publish a balance sheet; 收支表 balance sheet; 收支不平衡 payment imbalance; payment disequilibrium; 收支簿 account book; 收支差额 gap between revenues and expenditures; deference; 收支范围 division of the revenue and expenditure boundaries; 收支计算书 account of business; 收支逆差 balance of payments deficit; 收支调整 payments adjustments; 收支预算 budget for revenues and expenditures; 收支帐目 income and expenditure account
• "热收入" 英文翻译 :    heat input
• "热收缩" 英文翻译 :    heat shrink-warp; heat shrinkage; shrinkage by heat; thermal contraction; thermal pinch; thermal shrinkage; thermoshrinking
• "加热收缩" 英文翻译 :    firing shrinkage
• "绝热收缩" 英文翻译 :    adiabatic compre ion; adiabatic compression; adiabatic contraction
• "热收集器" 英文翻译 :    heat trap
• "热收缩包装" 英文翻译 :    constitute package/ assembly package
• "热收缩薄膜" 英文翻译 :    shrink film
• "热收缩差异" 英文翻译 :    thermal-shrinkage differential
• "热收缩成形" 英文翻译 :    heat shrink forming
• "热收缩管" 英文翻译 :    heat-shrinkable tube
• "热收缩绝缘" 英文翻译 :    heat shrinkage insulation
• "热收缩率" 英文翻译 :    heat shrinkage
• "热收缩膜" 英文翻译 :    pof; zdf-01
• "热收缩配合" 英文翻译 :    heat shrink fit
• "热收缩试验" 英文翻译 :    heat shrinkage test
• "热收缩套" 英文翻译 :    heat shrink sleeve
• "热收缩套管" 英文翻译 :    sumitube
• "热收缩纤维" 英文翻译 :    heat-shrinkable fibre
• "热收缩效应" 英文翻译 :    thermal pinch effect
• "热收缩应力" 英文翻译 :    thermal shrinkage stress
• "再热收缩" 英文翻译 :    after contraction
• "太阳热收集器" 英文翻译 :    solar heat collector

• 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。
• 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。
• 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。
• 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。