共查询到20条相似文献，搜索用时 62 毫秒
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１引言随着计算机的普及与发展，气象部门各项业务已离不开计算机。由于计算机业务操作系统的不稳定性，运行一段时间后，会发现速度越来越慢，其原因是经常安装和卸载软件产生的大量垃圾文件造成的。如果任其发展，会导致系统文件丢失，乃至系统崩溃。当然，最终解决这类问题的方法就是重新安装系统。这样即费时，又费力。如果能在第一次装完操作系统和各种软件时做一次系统和软件的备份，只要遇此情况，只需１０几分钟可解决。这里介绍一种功能齐全的硬盘分区备份软件GHOST６．０。有了这个软件，就会解除系统崩溃后的烦恼。２GHOST６… 相似文献
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目前,大多数气象台站都为自动站配备了备份计算机,安装了相应的地面气象测报业务系统软件,但往往由于备份计算机管理不到位,一旦遇到自动站故障,备份机无法在较短的时间内完成替换。为保证自动站能及时恢复正常运行、上传各类气象资料,自动站实时数据的异机同步备份和恢复就显得尤为重要。 相似文献
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介绍了如何利用GHOST软件的硬盘复制功能，对河南省气象影视中心内各种含计算机影视设备的业务软件系统进行备份。这种操作方式简化了设备维护操作，缩短了安装(恢复)软件系统的时间，以确保电视气象节目制作和播出的正常进行。 相似文献
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介绍了如何利用GHOST软件的硬盘复制功能,对河南省气象影视中心内各种含计算机影视设备的业务软件系统进行备份.这种操作方式简化了设备维护操作,缩短了安装(恢复)软件系统的时间,以确保电视气象节目制作和播出的正常进行. 相似文献
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贵州省气象局办公业务自动化的基本目标是依托于气象现代化业务网络，实现各地、州、市气象局以及本局内部办公公文的实时传输；实现网络资源（如硬盘、光驱）及一些昂贵资源（如打印机、扫描仪）的共享；实现业务资料（雨量、温度预报等）与决策部门之间的网上传输；实现电子邮件的发送和接收；实现办公资料的集中式管理和查询。1本局气象业务网络基本状况在建成刃、公自动化之前，气象台已存在基干NetwareVovelf网络操作系统的业务运行网，并由V．32Modem通过X．25公用分组网络交换网与各地、州、市局有业务联系，整个局域网为一个共享… 相似文献
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吉林省气象网络实时业务系统的更新周晓红，张鑫晶１引言“全国气象信息网络系统”是由各级气象部门的计算机局域网，通过长途通信电路互联组成。为保证气象信息传输业务的正常运行，由国家气象中心制定了《气象信息网络系统资料传输业务规程》方案，要求全国各地级气象部... 相似文献
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黑龙江省气象VPN网络的实现 总被引：1，自引：0，他引：1
1引言气象网络是全省气象业务工作的枢纽,承担着大量信息的转发,其特点是信息量大、实时性强。这样在2M光纤数字电路运行的同时,备份网络便显得十分重要了。目前各地采用了宽带网络或远程拨号与黑龙江省气象网络中心内部网络建立VPN通道,该通道用来作为2M数字电路的备份信道。当各地市县2M数字电路故障后,VPN网络可成功接替所有气象信息转发工作。由于VPN网络通讯费用和维护费用低,通信的安全性高、传输速度快,因此,建立VPN连接作为备份网络是一个最佳理想的选择。2 VPN网络的创建2.1 VPNVPN(Virtual Private Network):虚拟专用… 相似文献
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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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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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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
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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
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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
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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：11，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
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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
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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