查询词典 WNW

At 08 HKT, HAIYAN was centred 1280 km (700 NM) WNW of Midway Atoll.

在08HKT，海燕集结在中途岛之西北偏西约1280公里(700海里)。

Approaching the Brazil coast near Recife the current diverges, the N part continuing WNW towards the Caribbean Sea (see 2.15) and the S part turning S as the warm Brazil Current.

Approaching在Recife附近的巴西海岸潮流分流， N零件继续往加勒比海的WNW (参见2.15)和转动S的S零件作为温暖的巴西潮流。

Late Quaternary right-lateral displacement and slip rates have been determined along WNW-ESE trending active faults in the intermontane Yanqi basin on the southeastern flank of the Chinese Tian Shan.

本研究对天山东南侧山间盆地－焉耆盆地的晚第四纪右行走滑活动断层的位移和滑动速率进行了测量。

These dust events were characterized by about 1-3 day duration, and NNW, NW, WNW.

而每逢降雨增加时，在之后的1～3年内，出现降尘的高峰期。

The Taichung Domain was moving northwestwards before the 1999 Chi-Chi earthquake: in the footwall of Chelungpu Fault the slip rate was ~10 mm/yr, while in the hanging wall the rate increased eastwards up to 10-30 mm/yr. Two years prior to the earthquake, in the footwall of Changhua Fault the deformation direction changed from WNW to almost due N, and velocity gradient changed from increasing northwards to increasing eastwards, suggesting possible precursor of a large earthquake.

中部地区在集集地震前大致向西北方向位移，车笼埔断层下盘位移速率约在10 mm/yr左右，断层上盘往东侧逐渐增大，在10~30 mm/yr之间；集集地震发生前2年，彰化断层下盘的位移方向由西北西转为偏北的位移型态，位移速度则由南向北增大，转为由西向东增大的趋势；即位移方向与位移速度有明显的改变，可能为地震前兆的相关资讯。

As for coseismic deformation of Chi-Chi earthquake, the footwall of Chelungpu Fault moved southeastwards 0.3-1.5 m, and the value was increasing toward the fault; the hanging wall moved northwestwards 1.4-7.0 m, but the value was smaller south of the Choshui River. After the Chi-Chi earthquake, the hanging wall of Chelungpu Fault was still moving west-northwestwards and kept uplifting, while the footwall gradually changed direction from ESE to WSW or even WNW, clockwise resuming to inter-seismic deformation pattern. It is interesting to notice that despite the largest coseismic deformation in the northernmost segment of Chelungpu Fault, the post-seismic deformation peaked around the epicenter of Chi-Chi earthquake.

集集地震之同震变形，在车笼埔断层下盘向东南方向位移0.30~1.5 m，且越靠近断层位移量越大；车笼埔断层上盘则向西北方向大幅位移约1.4~7.0 m，浊水溪以南的位移量较小；集集地震以后之震后变形型态，以车笼埔断层为分界，上盘在震后向西北西方向位移的型态仍与同震时相同，下盘由同震时一致性的向东南东方向，逐步向西北西或西南西方向位移，亦即在车笼埔断层下盘有逐步依顺时针方向回归至震间的滑移型态；另就位移速率而言，虽然同震变形最大地区在车笼埔断层北端，但其震后的变形量最大地区，却集中於震央位置附近；就地震循环而言，震后的6年期间仍处於地层压密重整阶段，尚未回归至该区震间阶段的位移状态。

Based on the distribution of sand-moving wind direction, the dominant wind direction of Yangqing station is WSW due to the regional terrain, the others are all WN, WNW, NNW, the results indicate that the main sand moving direction in Beijing plain is from northwest to southeast.

从起沙风动力方向分布来看，除延庆站受区域地形影响是西南西为主导风向，其余站点的主导风向都是西北、西北西、北北西三个方向，说明北京平原地区的沙尘运移方向主要是自西北向东南搬运。

Approaching the Brazil coast near Recife the current diverges, the N part continuing WNW towards the Caribbean Sea (see 2.15) and the S part turning S as the warm Brazil Current.

靠近巴西海岸附近的累西腓流开始分叉，北面部分继续以西北西的方向向加勒比海地区（见2.15 ）移动，同时南面部分作为巴西暖流流向南面。

Simulation results indicate that for the Taipei Harbor five wave periods 9.8sec, 5.4sec, 4.1sec, 3.6sec, and 3.2sec incident in WNW direction having resonant impact. Whereas in N and NNE directions there exist no resonance phenomena due to sheltering effects from the north-side breakwater.

在港区码头的共振特性上，结果显示在WNW方向入射的波浪有5个周期T=9.8sec、5.4sec、4.1sec、3.6sec、3.2sec对港区码头的共振影响较为显著，在N向与NNE向则因为有北堤防的遮蔽，因此对於港区码头并没有共振发生。

The moving direction of dune is WNW→ESE, with speed of 7-81meter per year.

沙丘移动方向是WNW→ESE，移动速度大体在7-81米/年。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。