CTL 713C多普勒天气雷达数字接收处理系统故障诊断分析

通过分析CTL-713C多普勒天气雷达数字接收处理系统硬件构成及工作原理,结合硬件状态指示介绍了该型雷达数字接收处理系统的正常工作状态。将CTL-713C多普勒天气雷达数字接收处理系统分成信号处理器、数字接收机、连接三类故障进行诊断,根据终端显示和系统硬件状态指示综合判断相应类型故障的处理方法,通过焦作CTL-713C多普勒天气雷达数字接收处理系统故障实例分析和诊断结果对处理方法进行了验证,并对雷达数字接收处理系统的故障诊断方法和原则进行了总结。     

宜昌新一代天气雷达运行故障处理及维护方法

从宜昌多普勒天气雷达投入业务试运行两年多的实际出发,结合这一期间该雷达所出现的126次故障,从雷达硬件和软件两个方面分析了各类故障发生原因,并指出了其相应的消除方法。在此基础上,归纳出了新一代天气雷达的常规维护方法。     

上海WSR-88D雷达故障诊断和分析

上海市气象局于1997年从美国引进了一部多普勒天气雷达WSR-88D,该雷达采用24 h连续工作的方式投入日常的业务运行,在天气探测和气象服务中发挥了重要作用。在多年的运行过程中,该雷达也出现了各种不同类型的故障,有些重要故障直接导致了雷达的停机,给气象服务带来了一定影响。文章介绍和总结了该雷达出现的一些主要故障,这些故障集中在雷达发射机部分的射频驱动器、聚焦线圈电源、触发放大器、调制器、后充电调整器等部件上。通过对这些部件的功能和工作原理的分析,详细介绍了分析和排除这些故障的关键技术。     

双线偏振天气雷达监控系统的设计与应用

为提升天气雷达资料传输和故障维修时效，避免双偏振雷达数据量大而造成资料传输异常的情况，利用C#语言开发了适用于雷达台站的监控报警平台。该平台通过监控雷达设备运行情况和资料传输情况，实现出现异常情况时通过4G无线通信及时告警功能，且相关告警信息可通过log日志查询。投入运行以来，系统运行稳定，有助于值班员及时发现并处理雷达故障，提高雷达业务质量。     

CINRAD/CC雷达接收机特性曲线异常诊断

依据新一代天气雷达接收机系统工作原理及接收系统特性曲线关键点参数测量方法,结合对CINRAD/CC新一代天气雷达系统特性曲线异常故障的分析,提出了接收系统特性曲线异常故障诊断流程及处理方法,该方法在排除CINRAD/CC新一代天气雷达接收机特性曲线异常的故障实践中得到验证,结果表明:采用这种诊断流程和处理方法不仅快捷、有效,还具有规范性和稳定性,可为雷达技术保障人员处理各种型号新一代天气雷达接收机特性曲线异常故障提供借鉴.     

新一代天气雷达故障处理和故障标准化平台的研发与应用

新一代天气雷达是一个组成结构复杂的探测平台,各个组合之间比较分散。由于机械运转的持续性,且对运行环境要求严格,所以雷达系统易发故障。对不同类型的雷达故障进行归纳和简析,并进行归类,按照雷达故障产生的原因分类为:雷达部件故障、软件故障、灾害引起的雷达故障、虚假报警、雷达产品图像错误。天气雷达故障处理和故障标准化平台的开发将相应的成果应用于日常的气象探测设备的监控业务中,并集成到综合气象观测系统运行监控平台,以实现天气雷达故障的快速响应和维修。对2007年6月至2010年5月新一代天气雷达的运行能力进行了计算,并抽样其中2种型号的天气雷达,对故障案例进行分析研究,给出了故障的分系统分布情况。     

浅谈伊春3830B雷达的故障与日常维护

<正>1雷达故障个例分析及处理伊春3830B雷达故障主要包括硬件故障和软件故障两个方面。硬件故障即由雷达各分系统中某个部件引起的故障,软件故障是由雷达终端系统监控软件和雷达各服务软件以及计算机系统引起的故障。1.1硬件故障(1)故障现象:预报员无法操作雷达,遥控配电箱也无法控制。分析处理:主端软件重新启动,雷达不可控,遥控配电箱仍无法控制。分段检查雷达网络,发现主端正常,用PING命令测试远端雷达地址,不通,     

新一代天气雷达CINRAD/CC接收系统典型故障分析与处理

分析CINRAD/CC雷达接收系统工作原理,给出了CINRAD/CC雷达接收系统关键点参数表,介绍了雷达接收系统常用的故障分析方法,通过对接收系统故障现象、故障原因分析,归纳总结出6类接收系统典型故障及其处理方法.随着雷达使用年限的增加,雷达设备故障率也在增加,而故障维修工作纷繁复杂,这就需要把雷达故障进行总结、分类,同一种类型的故障对应相应故障处理方法,这样就能大大提高雷达维修的时效性.     

CINRAD/CC天气雷达一例俯仰电源特殊故障分析

CINRAD/CC天气雷达在牡丹江投入业务运行以来,出现了一些故障也积累了很多维修经验.针对CINRAD/CC雷达在使用过程中多次出现报伺服系统俯仰电源22号故障,分析其故障成因并给出处理方法.     

太原新一代多普勒天气雷达故障浅谈

太原新一代天气雷达C IN RA D/CC投入使用以来,经过3年多的实际运行,从中发现了一些常见故障,我们对这些故障进行了分析总结,并给出了相应的处理办法,得到了一些经验。1故障类型1.1虚假故障虚假故障是指雷达终端有故障报警,但是还处于正常工作状态。这类故障对于雷达运行没有影     

加强业务管理提高测报质量

我局从1999～2003年,测报工作连续4年未出现错情,在此期间共有1个250个班,9个百班无错通过上级业务部门验收.在仪器保管、使用、维护上符合要求,对外报送的各种表、簿都能做好出门合格.     

Comparing the theoretical versions of the Beaufort scale, the T-Scale and the Fujita scale

2005 is the bicentenary of the Beaufort Scale and its wind-speed codes: the marine version in 1805 and the land version later. In the 1920s when anemometers had come into general use, the Beaufort Scale was quantified by a formula based on experiment. In the early 1970s two tornado wind-speed scales were proposed: (1) an International T-Scale based on the Beaufort Scale; and (2) Fujita's damage scale developed for North America. The International Beaufort Scale and the T-Scale share a common root in having an integral theoretical relationship with an established scientific basis, whereas Fujita's Scale introduces criteria that make its intensities non-integral with Beaufort. Forces on the T-Scale, where T stands for Tornado force, span the range 0 to 10 which is highly useful world wide. The shorter range of Fujita's Scale (0 to 5) is acceptable for American use but less convenient elsewhere. To illustrate the simplicity of the decimal T-Scale, mean hurricane wind speed of Beaufort 12 is T2 on the T-Scale but F1.121 on the F-Scale; while a tornado wind speed of T9 (= B26) becomes F4.761. However, the three wind scales can be uni-fied by either making F-Scale numbers exactly half the magnitude of T-Scale numbers [i.e. F′half = T / 2 = (B / 4) − 4] or by doubling the numbers of this revised version to give integral equivalence with the T-Scale. The result is a decimal formula F′double = T = (B / 2) − 4 named the TF-Scale where TF stands for Tornado Force. This harmonious 10-digit scale has all the criteria needed for world-wide practical effectiveness.     

准两年振荡对大气中微量气体分布的影响

NCAR的包含化学、辐射、动力相互作用的两维模式（SOCRATES）移植回国后进行了初步的模拟试验,用以研究某些对环境问题重要的微量气体的化学、辐射、动力传输过程。在不考虑极地平流层云和气溶胶表面非均相化学等情况下,模式积分多年,计算结果稳定,模拟的风场、温度场显示出正常的季节变化,模拟的微量气体分布与卫星实测资料对照,结果也比较一致。为了探讨热带平流层风场的准两年周期振荡（QBO）对平流层微量气体分布的影响,我们做了QBO强迫的数值试验,即在模式中加入QBO强迫,并与不考虑QBO强迫的模拟结果对比。结果表明,QBO与其相关的次级环流所引起动力输送的变化,使平流层微量气体分布发生变化。     

Quantifying the uncertainty of the annular mode time scale and the role of the stratosphere

The impact of high resolution modern vegetation cover on the West African climate is examined using the International Centre for Theoretical Physics Regional Climate Model implementing the NCAR Community Land Model. Two high resolution 25 km long-term simulations driven by the output from a coarser 50-km resolution simulation are performed for the period 1998–2010. One high resolution simulation uses an earlier and coarser-resolution version of plant functional type distribution and leaf area index, while the other uses a more recent, higher-quality, and finer-resolution version of the data. The results indicate that the new land cover distribution substantially alters the distribution of temperature with warming in Central Nigeria, northern Gulf of Guinea and part of the Sahel due to the replacement of C4 grass with corn; and cooling along the coastlines of the Gulf of Guinea and in Central Africa due to the replacement of C4 grass with tropical broadleaf evergreen trees. Changes in latent heat flux appear to be largely responsible for these temperature changes with a net decrease (increase) in regions of warming (cooling). The improved land cover distribution also results in a wetter monsoon season. The presence of corn tends to favor larger precipitation amounts via more intense events, while the presence of tropical broadleaf evergreen trees tends to favor the occurrence of both more intense and more frequent events. The wetter conditions appear to be sustained via (1) an enhanced soil moisture feedback; and (2) elevated moisture transport due to increased low-level convergence in regions south of 10N where the most substantial land cover differences are present. Overall the changes induced by the improved vegetation cover improve, to some extent, the performance of the high resolution regional climate model in simulating the main West African summer monsoon features.     

由中国历史气候记录对季风导致唐朝灭亡说的质疑

2007年1月4日杂志发表了Yancheva等10人的题为"Influence of the intertropical convergence zone on the East-Asian monsoon"(热带辐合带对东亚季风的影响)的论文[1],这是德国波兹坦地学研究中心气候动力与沉积学科的主管豪格(G.H.Haug)率领的科研小组的一项成果,认为是季风的变化引起的长期干旱导致了唐朝的灭亡.     

流场配置及地形对西南低涡形成的动力作用

本文采用定常二层模式讨论较小地形及高、低层流场配置对西南低涡形成的动力作用。指出了西南低涡的形成是与盆地、河谷以及其上气流分层有关的一种定常态.在上、下为西风分层时期,低层的浅薄暖湿西风有利于西南低涡的形成.在上、下为东、西风分层时期,上层浅薄东风亦有利于西南低涡的形成.小型的凸起山脉对西南低涡的形成没有作用.     

On the forecast of the onset and end of the convective season in the Amazon

Summary ?Some features of the climate system that can be considered predictors of the onset and end of the convective season over the Amazon were identified using one-month lag correlations and field composites. The fields analyzed were sea surface temperature (SST), outgoing long-wave radiation (OLR), vertical velocity and upper tropospheric winds. Warm (cold) anomalies in the SST in the tropical North Atlantic and the Caribbean Sea tend to be associated with delayed (early) onsets. Likewise, there is a tendency towards a delayed (early) end of the convective season with cold (warm) anomalies in these ocean regions. In addition, the SST in the cold tongue region of the equatorial Pacific is negatively, though weakly correlated with the onset date. The signal of this SST is more evident in the case of the end date, which is earlier with respect to its mean date in most of El Ni?o cases. The convective activity intensity itself conditions the onset and the end of the convective season, as it is evidenced by the behavior of the OLR and the vertical velocity fields. The more (less) intense the convective activity over South America during the preceding month, the earlier the onset and the later the end of the convective season on the Amazon region. The prediction of the onset and end dates of the convective season in the Amazon region was explored using a simple multiple regression technique based on the variables that have shown precursor signals with respect to these dates. The correlation coefficient between the predicted and the observed onset date is 0.81, and in the case of the end date, it is 0.76. The skill to predict early, delayed and normal categories was high, since in more than two thirds of the cases the category was successfully predicted, and there were no predictions of categories opposed to those observed. Received July 23, 2001; revised February 22, 2002; accepted April 26, 2002     

Analysis of the Characteristics of the Low-level Jets in the Middle Reaches of the Yangtze River during the Mei-yu Season

Here, we analyze the characteristics and the formation mechanisms of low-level jets(LLJs) in the middle reaches of the Yangtze River during the 2010 mei-yu season using Wuhan station radiosonde data and the fifth generation of the European Centre for Medium-Range Weather Forecasts(ERA5) reanalysis dataset. Our results show that the vertical structure of LLJs is characterized by a predominance of boundary layer jets(BLJs) concentrated at heights of 900–1200 m.The BLJs occur most frequently at 230...