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1.
自动气象站采集器数据质量控制程序的改进设计   总被引:1,自引:0,他引:1  
讨论自动气象站采集器的数据质量控制问题,以气温、风向、风速和降水量等4个代表性气象要素为例,提出自动气象站采集器数据质量控制程序的改进方案。在遵循向下兼容性、低运算量等要求下,改进设计在现有自动气象站采集器软件整体框架内进行。  相似文献   

2.
自动气象站探测网实时监控关键技术   总被引:2,自引:0,他引:2  
在阐述自动气象站全网远程实时监控系统基本原理和系统架构的基础上,深入分析了站网扩容更新维护算法、在线自动气象站的远程指令控制等关键技术,并根据实时探测数据判断采集器及各传感器工作状态,实现故障信息的自动提取与短信报警.在对广东省近2000个区域自动气象站探测网的监控保障业务应用中,该系统较好地实现了全省自动气象站组网维...  相似文献   

3.
自动气象站编报数据缺测的应急处理方法   总被引:3,自引:2,他引:1  
针对在测报日常工作中,当临近规定编发气象观测报告时次的时候,突遇自动气象站正点数据采集失败、计算机出故障而采集器正常、采集器出故障而计算机正常、采集器和计算机同时发生故障等情况时,经多方探索,得出了如何取得自动气象站的编报数据,以确保气象数据完整、测报业务正常运行。  相似文献   

4.
通过统计新型自动气象站相关设备监测点运行状态信息及同时段地温、气压、气温、湿度、风、降水6要素数据质量的正常或异常频率,对观测要素数据与设备状态信息做了相关性分析,并针对各要素统计了相关状态监测点的命中率、误警率等指标。结果表明通信状态、设备自检状态及传感器3个监测点运行正常时与观测数据间的一致性较好,正常命中率高于96%,而采集器、通信接口、计数器、AD、主板温度等部件状态异常时与观测数据间一致性较差,异常命中率低于3%。利用国内新型自动站运行状态文件来辅助判断相关观测要素质量,虽然在应用中还存在一定问题和需改进方向,但有利于改进数据质量控制方法、提高数据的真实性和可用性。  相似文献   

5.
自动气象站业务运行中的几点注意事项   总被引:10,自引:0,他引:10  
随着气象现代化建设的不断推进,自动气象站已成为各级气象台站的主要观测方式,但在自动气象站的业务运行时,需要注意参数设置,采集器时钟的校对,自动站数据文件的备份,以及自动气象站报文回执检查等事项,处理好了这些注意事项,可以保证自动气象站业务的正常运行,提高自动气象站的测报质量.  相似文献   

6.
自动气象站实时数据丢失的恢复方法   总被引:1,自引:0,他引:1       下载免费PDF全文
自动气象站运行过程中,由于各种原因会造成Z文件中数据丢失:一种是永久性丢失,即自动气象站的采集器、传感器等出现故障造成实时数据完全丢失,无法恢复;另一种是可恢复性丢失,即采集器、传感器工作正常,而由于通讯线路故障、文件读写错误、共享冲突、软件升级等原因造成实时数据丢失,可通过软件操作恢复。  相似文献   

7.
1 硬件设备问题引起的数据异常 1.1 数据全部缺测 (1) 采集器损坏导致无法采集数据,出现数据全部缺测.(2)采集器电源系统故障,致使定时数据无法采集,出现要素全部缺测.(3)通信线路出现故障.当自动气象站的防雷板、终端机的串口或连接卡、串口隔离器被雷击、通信线缆出现断开或其他因素导致开路都是导致自动气象站数据全部缺测的原因.  相似文献   

8.
自动气象站数据质量控制体系设计   总被引:1,自引:0,他引:1       下载免费PDF全文
数据质量是影响自动气象站观测业务发展的一个瓶颈。重新定义了自动气象站数据质量,分析了影响自动气象站数据质量的因素,设计了自动气象站数据质量控制体系,并对体系的各组成部分进行了详细阐述。自动气象站数据质量控制体系由质量控制流程、质量控制标识码、数据质量评估三部分组成,其中,质量控制流程又由数据生产阶段、数据传输阶段、数据检查阶段组成。自动气象站数据质量控制体系的核心是在减少疑误数据产生的前提下,对观测数据进行全生命周期控制和评估。  相似文献   

9.
介绍了一款能够模拟传感器的数据发送给采集器,还可以直接读取传感器的数据的仪器的设计思路.该仪器能够快捷的判断自动气象站的故障,从而缩短整个自动气象站的维护时间,提高维护效率.  相似文献   

10.
自动气象站数据异常因素分析   总被引:2,自引:0,他引:2  
探索自动气象站数据异常的因素,识别自动气象站异常数据类型,在质量控制中把好数据处理关,更有效地保证自动气象站数据正确性.  相似文献   

11.
叶茵  余清 《贵州气象》2004,28(4):37-38
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.  相似文献   

12.
13.
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  相似文献   

14.
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.  相似文献   

15.
准两年振荡对大气中微量气体分布的影响   总被引:11,自引:5,他引:6  
张弘  陈月娟  吴北婴 《大气科学》2000,24(1):103-110
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。  相似文献   

16.
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.  相似文献   

17.
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...  相似文献   

18.
19.
由中国历史气候记录对季风导致唐朝灭亡说的质疑   总被引:1,自引:0,他引:1  
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.  相似文献   

20.
流场配置及地形对西南低涡形成的动力作用   总被引:10,自引:8,他引:10  
高守亭 《大气科学》1987,11(3):263-271
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.  相似文献   

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