1) net pyrradiometer
辐射平衡表
2) radiation balance
辐射平衡
1.
Using the IOP,FOP data of GAME-Tibet and HEIFE,the temporal variations of the climatological features of the parameters of the radiation balance of the north of the Tibet Plateau and the desert in HEIFE were calculated and analyzed.
利用中日合作"全球能量与水分平衡试验 青藏高原季风试验(GAME Tibet)"和中日合作"黑河地区地—气相互作用野外观测实验研究(HEIFE)"IOP、FOP资料,计算分析了藏北高原典型草甸下垫面安多站和HEIFE沙漠站的辐射平衡各相关特征量时频变化的气候学特征。
2.
The distributions of annual mean radiation balance .
最后得出福建省各月、年地面辐射平衡的分布。
3) radiation budget
辐射平衡
1.
The data related with radiation,aqueous vapor,and air temperature collected at the urban and suburban sites in Nanjing from 17 February to 2 March,2006 are used in this paper to analyze the radiation budget over urban and suburban different underlying surfaces,and the changes of each component,as well as their differences.
市区水泥下垫面是城市各种人为下垫面类型中占比重最大的一种且具有典型的城市化特征,其热力性质明显有别于郊区接近自然的下垫面,这必然造成地表辐射平衡和能量交换过程发生改变,对城市气候产生影响。
2.
The solar radiation budget and energy balance were anlysed based on a long time series observation in an automatic station setted on the ELA of the glacier.
本文以连续的、至少一年的观测资料，分析青藏高原唐古拉山冬克玛底冰川平衡线高度处的辐射平衡及能量平衡特征。
4) equilibrium radiation
平衡辐射
1.
The essay ,according to the works of Albert Einstein and the documentary materials about the conception of light quantum, explores the close relationship between the conception of light quantum and the theory of Wien s equilibrium radiation as well as the thinking method and process of the conception of light quantum put forward by Albert Einstein.
以爱因斯坦原著及有关文献资料为依据，论述了光量子概念与维恩的平衡辐射理论的密切联系，以及爱因斯坦提出光量子概念的思想方法和过
5) thermal radiation equilibrium
热辐射平衡
1.
For a semitransparent graded index medium with absorbing-transmitting boundary surfaces, the physical and mathematical models of thermal radiation transfer in medium and thermal radiation equilibrium on boundary surfaces are founded.
通过数值模拟,分析了正弦折射率下,边界面的反射特性、吸收率以及介质层光学厚度对介质内热辐射平衡温度场及热流分布的影响。
6) nonequilibrium radiation
非平衡辐射
1.
The formulae of statistical theory of entropy of nonequilibrium radiation which have been cited extensily in various references are applied to calculate the entropy density of isotropic and anisotropic euilbrium radiation respectively.
用现有文献上广泛引用的非平衡辐射熵的统计理论公式，分别计算各向同性与各向异性的平衡辐射的熵密度，与正确的结果比较分析得出结论：这种公式对各向异性的平衡与非平衡辐射都不适用，非平衡辐射熵的统计计算问题并未解决。
补充资料：辐射平衡
| 辐射平衡 radiation balance 地球表面、大气或某一地区辐射能量的收入与支出之间的差值。又称辐射差额或净辐射。 地球或某一区域的地面辐射平衡是其辐射收入（即太阳短波辐射减去地面反射部分）与支出（地面散发的长波辐射减去大气向地面的长波辐射）之间的差值。地球-大气系统的辐射平衡是地面为下底，以大气顶为上顶的整个铅直柱内接收到的太阳短波辐射和大气顶界向太空放出的长波辐射之差值。将地球-大气系统的辐射平衡减去地面的辐射平衡，即得大气的辐射平衡。 辐射平衡随季节、纬度、地面状况、云量和大气成分而变化。平均而言，高纬度地区为负值，低纬度地区为正值。由于地面与大气的热状况多年来无长期变化趋势，所以对整个地球表面与大气而言辐射平衡应为零值。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条