| 1. | The effect of cloud on net radiation flux is not the same at the top and bottom of the atmosphere .
云对净辐射通量的影响在大气顶和大气底是不一样的。 |
| 2. | Radiation flux density
辐射通量密度 |
| 3. | Radiant flux test
辐射通量试验 |
| 4. | Study on the uncertainties of methods and precision of net radiation flux measurement
净辐射通量观测方法及观测精度的不确定性研究 |
| 5. | Flux of radiation
辐射通量 |
| 6. | Test method for critical radiant flux of exposed attic floor insulation using a radiant heat energy source
利用辐射热能源测定暴露的顶楼地板绝缘临界辐射通量的方法 |
| 7. | Standard test method for critical radiant flux of exposed attic floor insulation using a radiant heat energy source
暴露于辐射热能源的搁楼地板绝缘的临界辐射通量的标准试验方法 |
| 8. | ( 4 ) without consideration of the heterogeneity of topography , the radiation flux is not sensitive to sub - gri d heterogeneity
( 4 )不考虑地形的非均匀性时，地表辐射通量对次网格的非均匀性并不敏感。 |
| 9. | The relative difference could larger than 10 % and the grid infrared radiation flux value calculated by present models would possibly have the same error correspondingly
在各向同性的假设下，模式中网格区的区域长波辐射通量计算有相应量级大小的误差。 |
| 10. | But if there is a topographic heterogeneity , the maximum relative difference of surface grid effective infrared radiation is about 30 % ~ 40 % . the magnitude of deviation is mainly determined by grid average elevation
而当考虑海拔高度的非均匀性时，有效辐射通量计算的相对误差可达30 40 ，取决于平均高度和变差系数大小。 |
