查询词典 wind-broken
- 与 wind-broken 相关的网络例句 [注:此内容来源于网络,仅供参考]
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Wind speed simulation is one of the most important means in wind power generation studies.
风速仿真是风力发电研究的重要手段之一。
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This text has considered the impracticable circuit is as collecting the wind electric field equivalence model behind the road to the electric wire, change, take the place of to including wind electric field node model go on, punish according to PQ at the modest trend foundation that calculate of law in Newton - pressgang.
本文考虑了架空线路作为集电线路后的风电场等值模型,在牛顿-拉夫逊法的潮流计算的基础上对含风电场的节点按照PQ迭代模型进行处理。
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Charge example in whom five node form, 4 node adopt Newton - pressgang modest law go on trend calculate, another node to contain wind-driven generator adopt PQ change, take the place of model go on trend calculate, change, take the place of with ordinary trend computing method first, judge revision wind electrical machinery nodal voltage error go on for the second time changing and taking the place of in establishing range.
在五个节点构成的算例中,4个节点采用牛顿-拉夫逊法进行潮流计算,另外一个含有风力发电机的节点采用PQ迭代模型进行潮流计算,先用普通潮流计算法迭代,后经过修正风电机节点电压判定误差是否在设定范围内进行第二次迭代。
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It observed elements of the marine environment are:(1) physical parameters, such as water temperature, salinity, currents, tide, wave and so on;(2) weather station network-related physics parameters, such as sea surface wind, temperature and dew point, pressure, sea ice, wind and waves and swell;(3) other parameters, such as solar radiation and rainfall;(4) non-physical parameters, such as pollution physical, chemical and biological parameters such as volume.
它所观测的海洋环境要素主要有:(1)物理学参量,如海水温度、盐度、海流、潮位、波浪等;(2)与天气站网有关的物理学参量,如海面风、气温及露点、气压、海冰、风浪和涌浪;(3)其他参量,如太阳辐射和降雨量;(4)非物理参量,如污染物质、化学和生物量参量等。
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These wind roses show the probability of occurrence of wind speeds for sixteen compass points.
这些风的图形揭示了十六分圆盘上风速出现的概率。
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CHANCE WIND: A pung of the Chance Wind, awarded 1 fan.
正风:以正风牌组成的刻子,得1番。
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The wind sang in the taut weather-rigging, and blustered around Bush's ears as he stood on the starboard side of the quarterdeck, balancing to the roll as the roaring wind sent one massive grey wave after another hurrying at the ship; the starboard bow received the wave first, beginning a leisurely climb, heaving the bowsprit up towards the sky, but before the pitch was in any way completed the ship began her roll, heaving slowly over, slowly, slowly, while the bowsprit rose still more steeply.
布什站在右舷后甲板,在风浪中努力保持着平衡。一波波的灰色巨浪扑来,右舷的船首最先被浪冲到,缓缓爬升,将船首斜桅举向了空中;然后船身开始摇晃,慢慢的抬升着,船首斜桅的角度更高了;终于船身摇晃着越过了巨浪,船首腾在半空,伴随着大量的泡沫往下直坠;船首斜桅开始下指,船身则笨重的达到了短暂的平衡;接下来整个船身携着泡沫被大海推到风中,船尾被浪峰抬高;最后船头又回到水中。
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It consists of three procedures: radiometric calibration of SAR image, wind direction determination and wind speed calculation.
该方法包括SAR图像辐射定标、海面风向确定和风速计算。
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The wind profiler worked from April 08,2004 to Sep 05, 2004. Compared with radiosonde data in the same period, the data of wind profiler is high reliable.
风廓线仪探测资料与同期探空资料比较表明,风廓线仪资料具有较高的可靠性。
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In order to investigate the excitation mechanism and response characteristics of wind-rain induced vibration of stay cable,an instrumentation system of wind-rain induced vibration measurement,which consists of anemometer,rain gauge and accelerometer,was installed on the Dongting Lake Bridge,Yueyang,China.
为了研究斜拉桥拉索风雨振的机理及响应特征,在岳阳洞庭湖大桥建立了由风速仪、雨量计、加速度传感器组成的风雨振现场观测系统,观测到了多次拉索风雨振现象;得到了发生拉索风雨振时风速、风向及雨量的基本条件,分析了风雨振时拉索振动的幅值、主振频率、模态参与特性及空气动力负阻尼比等响应特征。
- 相关中文对照歌词
- Blowing Kisses In The Wind
- When That Wild Wind Blows
- Chase The Wind
- The Weight Of The Wind
- Strong Strong Wind
- Blow Wind Blow
- Roll With The Wind
- It's Hard To Get Around The Wind
- Wind Is Calling (Hush The Wind)
- The Wind, The Wind
- 推荐网络例句
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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.
最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。
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Only person height weeds and the fierce looks stone idles were there.
只有半人深的荒草和龇牙咧嘴的神像。
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This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.
这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。