| 1. | The colour scale on the right indicates the magnitude of the rainfall rate
Hkt代表香港时间，右边的色板指出降雨率的大小。 |
| 2. | Hkt means hong kong time . the colour scale on the right indicates the magnitude of the rainfall rate
Hkt代表香港时间，右边的色板指出降雨率的大小。 |
| 3. | Lightning locations are denoted by white squares while rainfall rates estimated from radar data are represented by different colours
闪电位置以白色方框显示，而雷达估算的降雨率则以不同颜色表示。 |
| 4. | The image shows the rainfall rate at a height of 3 km above mean sea level , as observed by hong kong observatory s weather radar
以上图像显示香港天文台天气雷达观察到在离海平面3公里高的降雨率。 |
| 5. | Furthermore , the rainfall rate refers to the 3 - km level , so that the rainfall reaching ground could be very different
再者，这降雨率只代表离海平面3公里高的情况，所以跟地面的降雨量会有所不同。 |
| 6. | The image shows the rainfall rate at a height of 3 km above mean sea level , as observed by hong kong observatory s weather radar
天气雷达图像注意以上图像显示香港天文台天气雷达观察到在离海平面3公里高的降雨率。 |
| 7. | An empirical formula is used to convert the signal intensity into rainfall rate . thus , the rainfall rate presented here is only an estimate
由于是利用了一经验公式将信号的强弱换算为降雨率，因此图像显示的降雨率仅为一估算数值。 |
| 8. | An empirical formula is used to convert the signal intensity into rainfall rate . thus , the rainfall rate presented here is only an estimate
由于是利用了一经验公式将信号的强弱换算为降雨率，因此图像显示的降雨率仅为一估算数值。 |
| 9. | Flooding occurs when rainfall is so high that natural or engineered drainage fails to drain away the surface runoff . floods are usually fairly transient in the urban areas
当降雨率超过天然或人造排水系统的负荷时，积聚地面的雨水便不能及时排去，因而引致水浸。 |
| 10. | Flooding occurs when rainfall is so high that natural or engineered drainage fails to drain away the surface runoff . floods are usually fairly transient in the urban areas
当降雨率超过天然或人造排水系统的负荷时，积聚地面的雨水便不能及时排去，因而引致水浸。 |
