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981.
设计了一种基于单片机的小型风力发电机扇叶朝向控制系统,该系统由风向传感器模块、液晶显示模块、驱动模块和扇叶朝向控制装置组成.系统以MSP430F149单片机作为控制核心,利用风向传感器测量风向信息传输给单片机,单片机根据风向信息控制步进电机调节扇叶朝向来风方向,并且风向信息由LCD显示.该系统可以提高风力发电机的工作效率,具有一定的实用意义.  相似文献   
982.
根据IEC61400-3设定工况,采用NREL开发的5 MW风机基础模型,应用FAST,以Aero-Hydro-Servo-Elastic耦合仿真技术对风机进行研究。对时域仿真得到的短期载荷,应用分块极大值法联合Gumbel分布外推计算风机极限载荷;以雨流计数法、线性累积损伤理论和S-N曲线为理论基础应用MLife软件,计算风机疲劳载荷。对比分析不同工况下浮式风机、近海单桩风机和陆上风机的极限载荷与疲劳载荷,进而探讨影响浮式风机动态响应的因素。结果表明,对于陆上风机和近海单桩风机,风是其主要载荷来源;而波浪是浮式风机主要载荷来源。对风机进行设计要根据特定海域统计的海洋气候条件,避免风机及其支撑结构的固有频率与波浪频率近似而产生共振;风机制造装配在一定误差范围内,质量不平衡对风机载荷几乎没有影响。  相似文献   
983.
Damage identification of the offshore floating wind turbine by vibration/dynamic signals is one of the important and new research fields in the Structural Health Monitoring (SHM). In this paper a new damage identification method is proposed based on meta-heuristic algorithms using the dynamic response of the TLP (Tension-Leg Platform) floating wind turbine structure. The Genetic Algorithms (GA), Artificial Immune System (AIS), Particle Swarm Optimization (PSO), and Artificial Bee Colony (ABC) are chosen for minimizing the object function, defined properly for damage identification purpose. In addition to studying the capability of mentioned algorithms in correctly identifying the damage, the effect of the response type on the results of identification is studied. Also, the results of proposed damage identification are investigated with considering possible uncertainties of the structure. Finally, for evaluating the proposed method in real condition, a 1/100 scaled experimental setup of TLP Floating Wind Turbine (TLPFWT) is provided in a laboratory scale and the proposed damage identification method is applied to the scaled turbine.  相似文献   
984.
唐友刚  宋凯  王宾 《海洋工程》2015,29(6):835-846
The floating foundation is designed to support a 1.5 MW wind turbine in 30 m water depth. With consideration of the viscous damping of foundation and heave plates, the amplitude-frequency response characteristics of the foundation are studied. By taking into account the elastic effect of blades and tower, the classic quasi-steady blade-element/momentum (BEM) theory is used to calculate the aerodynamic elastic loads. A coupled dynamic model of the turbine-foundation- mooring lines is established to calculate the motion response of floating foundation under Kaimal wind spectrum and regular wave by using the FAST codes. The model experiment is carried out to test damping characteristics and natural motion behaviors of the wind turbine system. The dynamics response is tested by considering only waves and the joint action of wind and waves. It is shown that the wind turbine system can avoid resonances under the action of wind and waves. In addition, the heave motion of the floating foundation is induced by waves and the surge motion is induced by wind. The action of wind and waves is of significance for pitch.  相似文献   
985.
A model for the Zambezi River plume, the largest on the Indian Ocean coast of Africa, is presented and the results of experiments with different discharges and wind forcings are analysed. Although the river plays an important role in the southern African economy through power generation on large dams, artisanal fisheries, and frequent flooding events that impact greatly on local populations, the plume has not been well studied. Observations during the period 2004–2007, when the winds were mainly easterly or south-easterly, indicated that the plume waters can extend both downstream (equatorwards) and upstream (polewards) of the Zambezi Delta with a recirculating bulge near the river mouth. The model is constructed using the Regional Ocean Modeling System (ROMS), with a 40-km long, 3-km wide river discharging into a rectangular coastal ocean with a linearly sloping bottom. When the model is forced only by a constant river discharge of 1 000?m3 s?1 (typical of observed discharge amounts in summer), the Kelvin and Froude numbers for the resulting plume imply a ‘large-scale’ buoyant discharge with a coastal current that is close to being in geostrophic balance with the across-shore pressure gradient and a recirculating ageostrophic bulge near the mouth. The distributions of the bulge and plume waters are found to be relatively insensitive to the discharge amount. Under constant wind forcing, the plume distribution changes dramatically. Northerly and easterly winds produce the largest changes with the latter able to deflect the plume up to 180° due to Ekman drift. When sea breeze-like winds are imposed, accumulation of water in the bulge occurs with substantial spreading upstream. Stronger sea breezes lead to less downstream spreading of the plume than gentle winds. When the winds are mainly across-shore, Ekman drift dominates, but the dynamics become almost geostrophic when the winds are roughly aligned to the coast. These experiments suggest that the Zambezi River plume is sensitive to the winds on diurnal to synoptic time-scales.  相似文献   
986.
张利平  王春红 《气象科技》2007,35(5):719-722
针对乌鲁木齐机场2002~2005年出现的典型东南大风天气过程,利用常规天气资料和机场跑道自动观测系统采集的实时观测资料,分析了东南大风天气机场跑道附近气象要素及水平风切变的演变特征。结果表明,①东南大风天气时气象要素场特征变化明显,起始和维持阶段具有升温、降压和降湿的特征,结束前具有降温、升压和升湿的特征,气温、场压和湿度变化转折的时间基本一致,这一时间也正是东南大风开始减弱的时间;②同一时刻机场跑道两端会出现风向和风速的不连续,在跑道上形成较强的水平风切变,尤其在起始和结束阶段跑道风切变强度表现得更明显。跑道两端风速差大小及其变化是影响风切变强弱和变化的决定因素。  相似文献   
987.
垂直积分液态水含量在地面大风预报中的应用   总被引:7,自引:0,他引:7  
东高红  吴涛 《气象科技》2007,35(6):877-881
利用天津塘沽的CINRAD-SA型新一代多普勒雷达体扫描垂直积分液态水含量(VIL)产品资料,结合地面大风灾情报告和实况资料,对地面灾害性大风出现前VIL值的演变、发展情况进行了统计分析。结果表明:VIL值达到30kg/m2是地面灾害性大风出现的阈值,VIL值达到或超过40kg/m2则可以看作是大风的一个预警指标;VIL值达到最大后的快速减小意味着将出现地面灾害性大风,VIL值快速减小后的突然跃增则是地面灾害性大风开始的标志。应用评分系统命中率、误警率、临界成功指数检验了上述预警指标,结果表明VIL产品预警地面灾害性大风是可用的,而且随时间调整阈值大小,可以大大提高地面灾害性大风预警的命中率和临界成功指数;地面灾害大风出现前预报员有12~18min的时间用于发布短时、临界大风天气预报和大风预警。  相似文献   
988.
989.
The neutral particle detector (NPD) on board Mars Express has observed energetic neutral atoms (ENAs) from a broad region on the dayside of the martian upper atmosphere. We show one such example for which the observation was conducted at an altitude of 570 km, just above the induced magnetosphere boundary (IMB). The time of flight spectra of these ENAs show that they had energies of 0.2-2 keV/amu, with an average energy of ∼1.1 keV/amu. Both the spatial distribution and the energy of these ENAs are consistent with the backscattered ENAs, produced by an ENA albedo process. This is the first observation of backscattered ENAs from the martian upper atmosphere. The origin of these ENAs is considered to be the solar wind ENAs that are scattered back by collision processes in the martian upper atmosphere. The particle flux and energy flux of the backscattered ENAs are and , respectively.  相似文献   
990.
GNSS-R航空遥感海面风场仿真技术   总被引:2,自引:1,他引:1  
周晓中  邵连军 《遥感学报》2012,16(1):143-153
研究了机载GNSS-R遥感海面风场的仿真原理和技术,以KA-GO相关功率模型为基础,分析海浪谱,海面坡度和风速风向的关系,并针对不同风速、风向、接收机高度和飞行速度海面散射信号相关功率开展了数值仿真分析研究,并建立了仿真软件。仿真研究结果表明,以上因素对海面反射信号的相关功率波形的峰值和后沿斜率均有影响。本文的仿真结论为GNSS-R海面风场反演打下了理论基础,建立的仿真软件为GNSS-R海面风场反演提供研究平台。  相似文献   
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