| 1. | Influence on uv intensity at the earth s surface
对到达地面紫外线强度的影响 |
| 2. | Factors affecting the ground - level uv intensity
影响地面紫外线强度的因素 |
| 3. | The fine weather also led to high values of uv radiation intensity
晴朗的天气亦导致较高的紫外线强度。 |
| 4. | Ultraviolet ray intensity meter
紫外线强度计 |
| 5. | Total erythemally weighted uv intensity . ( area under the red line )
图二受红班光谱加权后的总紫外线强度(红线内的面积) |
| 6. | Multiply the total erythemally weighted uv intensity by 0 . 04 to obtain the uv index
将红班光谱加权后的总紫外线强度乘0 |
| 7. | Figure 3 total erythemally weighted uv intensity . area under the red line
图三受红斑光谱加权后的总紫外线强度红线内的面积 |
| 8. | Measured uv intensity across the solar uv spectrum and the erythemal action spectrum
图二太阳紫外线光谱内所量度的紫外线强度及红斑作用光谱曲线 |
| 9. | Measured uv intensity across the solar uv spectrum and the erythemal action spectrum
图一太阳紫外线光谱内所量度的紫外线强度及红班作用光谱曲线 |
| 10. | The uv index is obtained by multiplying the measured uv intensity by a conversion factor
只要将宽波段仪所量度的紫外线强度乘上一个变换常数，便可计算出紫外线指数。 |
