西北西

词组短语

west-northwest

与西北西相关的网络例句 [注：此内容来源于网络，仅供参考]

In a major construction project: 20 million yuan investment in dairy production and snow Dayton Naiyuan base construction, investment 19.8 million yuan Yan Jia Ping bases for dairy cattle, 52.5 million yuan investment in Lanzhou Electric Corporation of digital efficient energy-saving electrical production lines, invest 31 million yuan Vacuum Equipment Corporation Technology Center and expansion of computer application software development projects, investment 53.38 million yuan Lanzhou Waitley welding consumables company Loi-of-hardface alloy to strengthen iron-based product line, invest 65.51 million yuan Co.

在建项目主要有：投资2000万元雪顿乳业生产及奶源基地建设、投资1980万元晏家坪奶牛基地建设、投资5250万元兰州电机集团公司数字化高效节能电机生产线、投资3100万元真空设备公司技术中心扩建及计算机应用软件开发项目、投资5338万元兰州威特利焊材公司莱武式相强化铁基硬面合金生产线、投资6551万元百合实业公司百合口服液生产线、投资9亿元年产50万箱卷烟兰州卷烟厂移址改造建设、投资3.8亿元兰州荣茂公司西北民贸大厦建设、投资4亿元兰州理工大学西校区建设、投资11.3亿元西津广场及旧房改造建设、投资2亿元上西园小区建没项目。

It is forecast to move West Northwest at 11 kph.

即在吕宋岛东北方海面，向西北西移动，时速20公里。

A mid-latitude trough will induce a break in the ridge and weaken its western side which will lead to a more northwesterly track after t+24 and a northerly track in the extended taus.

预料一道西风槽将令副高出现弱点，副高届时将转呈西北-东南走向，从而使凤凰在 24 小时后转向西北偏西至西北移动，并於 72 至 96 小时后转向偏北方向移动。

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。

The main rivers are Lechang into the county from the northeast corner, by the flow of Shaoguan Wu Gui Town rivers; originated in the northwest and the Yangshan county border Ah fork top and flows from west to east Nanshui reservoir, through the county, import Beijiang rivers of milk; originated in the north-west county and the junction of Yizhang County, Hunan Province Meng Hang Shi Dong Lu, from northwest to southeast through the Daping, bridges, Bibei, Gui Yang, head into the Wujiang River ; originated in the northern foot of the courtyard of the ant hill rock, from north to south flow through Luoyang, large cloth imported Anglo-German city of Tai Tam River.

主要河流有由乐昌流入县境东北角，经桂头镇流向韶关的武江河；发源于县境西北与阳山交界的丫叉顶，由西向东流入南水水库，穿过县城，汇入北江的乳江河；发源于县境西北面与湖南省宜章县交界的猛坑石东麓，由西北向东南经大坪、大桥、必背、桂头流入武江的杨溪河；发源于天井山北麓的蚁岩，由北向南流经洛阳、大布汇入英德市的大潭河。

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。

By 1840, the early cotton-producing states had been left behind. In 1860, Alabama, Mississippi, and Louisiana were far in the lead. With Mississippi alone producing more cotton than Georgia and South Carolina combined.

到了1840年，最早的产棉州落伍了。1860年，阿拉巴马，密西西北和路易斯安那州遥遥领先，其中密西西北一州的产量超过佐治亚与南卡罗莱纳两个州的产量之和。

The result shows that the crustal deformation is changing a lot in NW China: the deepest Moho is beneath the conjuction of west Kunlun and Karakorum, about 90 km deep, the shallowest Moho is beneath Jayir mountain to the west of Karamay, about 35.5 km; the Moho depth in the western segments of Tien shan is deeper then the mindle and eastern segments; there are Moho offset beneath Altyn fault, central Tien Shan northern margin fault and so on.

结果表明：比起我国其他地区，西北地区莫霍面无论是埋深还是形态均变化最大，反映出受印度板块与欧亚板块碰撞影响，西北地区地壳整体变形强烈。莫霍面最深（约90 km）位于西昆仑与喀喇昆仑构造结合处，最浅处位于准噶尔盆地西缘的克拉玛依（约35.5 km），最深与最浅差约55km。在盆山结合部位及大型走滑断裂，如阿尔金断裂、中天山北缘断裂带等均存在莫霍面错断。

与西北西相关的网络解释 [注：此内容来源于网络，仅供参考]

NNW：西北偏北

二十八、风向:风吹来的风向,气象上常用十六个方位和静风表示,即北(N),东北偏北(NNE),东北(NE),东北偏东(ENE),东(E),东南偏东(ESE),东南(SE),东南偏南(SSE),南(S),西南偏南(SSE),西南(SW),西南偏西(WSW),西(W),西北偏西(WNW),西北(NW),西北偏北(NNW)和静风(C,风速<

North West by West：西北偏西

North West by North 西北偏北 | North West by West 西北偏西 | North West 西北

North-west：西北,西北方

北,北方,北部 north | 西北,西北方 north-west | 西南,西南方 south-west

wind W veering NW：风由西向西北转

eddy, a whirl wind 旋风 | wind W veering NW 风由西向西北转 | wind W backing SW 风由西转向西南

west-northwest：西北西

west 西方 | west-northwest 西北西 | west-southwest 西南西

west-northwest：西北偏西

north-northwest西北偏北 | west-northwest西北偏西 | west-southwest西南偏西

west-southwest：西南西

west-northwest 西北西 | west-southwest 西南西 | westbound 向西进行的

northwest by west：西北偏西

northwest by north 西北偏北 | northwest by west 西北偏西 | northwest monsoon 西北季风

WNW：西-北-西

附件七,八为高雄地区全年及各月风玫瑰图,本区冬季季风期约由每年十月至翌年四月,风向以北北西~西北西(NNW~WNW)向间为主;而五月及六月为转型期,西北西(WNW)向及南南东(SSE)向所占比例率相当高,七至九月则为夏季季风期,

WNW：西北偏西

二十八、风向:风吹来的风向,气象上常用十六个方位和静风表示,即北(N),东北偏北(NNE),东北(NE),东北偏东(ENE),东(E),东南偏东(ESE),东南(SE),东南偏南(SSE),南(S),西南偏南(SSE),西南(SW),西南偏西(WSW),西(W),西北偏西(WNW),西北(NW),西北偏北(NNW)和静风(C,