| 1. | Fig . 8 low - level radial winds observed by the tdwr at 10 : 09 p . m . on 6 july 2001
图8 tdwr于二零零一年七月六日晚上十时零九分探测到的低空径向风 |
| 2. | Fig . 13 low - level radial winds observed by the tdwr at 03 : 59 p . m . 16 september 1999 . y . c
图13 1999年9月16日下午3时59分机场多普勒天气雷达扫描所得的低空径向风。 |
| 3. | However , at about 3 nm nautical miles from the rwy 07r threshold , the radial winds away from the radar were apparently weaker
不过，在rwy 07r入口对开约3海里位置，离开雷达的径向风明显较弱。 |
| 4. | In this way the tdwr can accurately measure the radial wind speed and its fluctuation from which low level windshear can be computed
机场多普勒天气雷达设有一套精密的电脑程式，让它能自动探测由雷暴引发的风切变。 |
| 5. | However , at about 3 nm ( nautical miles ) from the rwy 07r threshold , the radial winds away from the radar were apparently weaker . narrow streaks of radial winds
不过，在rwy07r入口对开约3海里位置，离开雷达的径向风明显较弱。 |
| 6. | Radar radial winds in fig . 13 show that behind the valleys of lantau island , several streaks of high - speed airflow were generated over the approach and departure areas
图13的雷达径向风速显示背景气流分别冲过大屿山的多个山谷后，在升降区上产生了数道高速气流。 |
| 7. | Radar radial winds in fig . 13 show that behind the valleys of lantau island , several streaks of high - speed airflow were generated over the approach and departure areas
图13的雷达径向风速显示背景气流分别冲过大屿山的多个山谷后，在升降区上产生了数道高速气流。 |
