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1.
泰安市地面气象资料数据库查询服务系统 总被引：1，自引：0，他引：1
介绍了地面气象资料数据库查询服务系统的开发环境及其主要功能,系统由基础数据库、D文件转换、集成查询和风向频率玫瑰图制作四部分组成,分别介绍了各部分的功能. 相似文献
2.
为了提高通信业务的自动化程度,提高气象报文的上传及时率,开发研制了非常规气象资料上行传输实时监控系统,实现了对各种非常规气象资料上行传输的实时监控、查询、告警等功能。主要介绍了非常规气象资料上行传输实时监控系统的平台概况、功能及其实现方法、开发技巧。 相似文献
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本文针对目前我省上行报文发送情况的现状，说明了建立上行气象报文监控和转发系统的关键技术，包括：使用三层模式、三层模式中各个层次的功能、接收和转发报文的过程、监控系统的运行状态，如何统一处理气象报文等。 相似文献
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为提高气象报文的编发质量和时效,研制了新乡市气象报文编发监控报警系统.该系统包括气象报文数据库设计、智能语音报警、编发报文、查询报文4个功能模块.通过编发报文模块,预报员能迅速编写气象报文,并自动完成报文的上传和下发;系统具有一定纠错能力,还可对发出的气象报文自动登记备案. 相似文献
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气象报文编发监控报警系统设计 总被引：2，自引：0，他引：2
为提高气象报文的编发质量和时效,研制了新乡市气象报文编发监控报警系统。该系统包括气象报文数据库设计、智能语音报警、编发报文、查询报文4个功能模块。通过编发报文模块,预报员能迅速编写气象报文,并自动完成报文的上传和下发;系统具有一定纠错能力,还可对发出的气象报文自动登记备案。 相似文献
6.
针对台站上行的各类气象数据传输质量信息,在Windows操作系统上,以Web方式,使用ASP和VC语言开发了一个基于Sql Server数据库的集统计、查询、管理、报表生成、相关文件规定检索等功能干一体的综合应用管理系统. 相似文献
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为实现日降水量报文实时处理和降水量资料检索查询的自动化，开发研制了山东省级雨情业务服务系统，主要功能包括全省各站日降水量报(SX)的报文采集、甄错、译码、降水量查询统计、不同量级雨日数查询统计、等值线分析、图表制作与输出、服务产品编撰制版、服务产品送网和用户信息管理等，系统业务运行稳定，保证了省级雨情业务服务工作的进一步规范化和流程化。 相似文献
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气象数据上行传输是各类气象业务和服务正常开展的基础。针对气象通信系统切换至CTS以后,台站实时获取上行气象数据传输状况的业务需求,在分析气象数据上行传输流程的基础上,提出了台站上行气象数据传输监控平台的建设思路,设计了平台总体结构,传输日志同步策略和数据个性化显示方案,采用MVC框架、Quartz调度器和jQuery Grid Plugin等技术对平台进行了实现。该平台面向台站用户具有提供上行气象数据传输状态实时监控、传输状态统计和错报查询功能;作为县级综合观测业务集成平台的一个模块投入业务使用,为提高上行气象数据传输质量提供平台支撑。 相似文献
9.
本文介绍了利用SQLServer数据库与ASP.NET技术,设计开发预报业务中报文、格点、图像、中尺度自动站观测及预报信息等多种气象信息查询的设计思路和实现方法. 相似文献
10.
针对台站上行的各类气象数据传输质量信息,在Windows操作系统上,以Web方式,使用ASP和VC语言开发了一个基于Sql Server数据库的集统计、查询、管理、报表生成、相关文件规定检索等功能于一体的综合应用管理系统。 相似文献
11.
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
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准两年振荡对大气中微量气体分布的影响 总被引：6，自引：5，他引：6
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
14.
Comparing the theoretical versions of the Beaufort scale, the T-Scale and the Fujita scale 总被引：1，自引：0，他引：1
G. Terence Meaden S. Kochev L. Kolendowicz A. Kosa-Kiss Izolda Marcinoniene Michalis Sioutas Heino Tooming John Tyrrell 《Atmospheric Research》2007,83(2-4):446-449
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.
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
张德二 《气候变化研究进展》2008,4(2):126-130
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
16.
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
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
17.
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
18.
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
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Chunguang CUI Wen ZHOU Hao YANG Xiaokang WANG Yi DENG Xiaofang WANG Guirong XU Jingyu WANG 《大气科学进展》2023,40(4):711-724
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