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1.
王远超 《广西气象》1999,20(3):45-46
介绍Novell与UNIX网络互连的硬件连接方法,常用于Novell与UNIX网络互连的四种软悠扬的安装和使用方法。  相似文献   

2.
随着9210工程网络的建成及投入业务使用,如何有效地发挥其作用,并与原网络系统协同运作,解决新旧网络的互连已成为一个亟待解决的课题。气象部门省、地两级各业务系统大都建在NOVELL平台上,在短期内还难以全部移植到UNIX平台,在很长一段时间内会形成多...  相似文献   

3.
本文阐述了民航气象网络的应用和维护中的一些问题,着重介绍了UNIX系统的维护和常见故障的处理。  相似文献   

4.
随着 92 1 0工程业务化运行 ,广东省气象通信体制由原来的以地面线路为主的格局 ,转向以卫星信道通信为主 ,地面X 2 5通讯网为辅的新通信体制。AXP2 0 0 0的服务器操作系统 ,也由原来的VMS转向性能稳定的UNIX。要做好AXP2 0 0 0气象业务系统的开发应用 ,需要掌握好UNIX下的Shell编程。原来以VMS操作系统为主的气象信息的传输方式也将有所改变 ,旧的业务程序要移植到UNIX系统上 ,新的业务应用也要结合 92 1 0工程的特点和UNIX操作系统的特点来进行设计开发。在此背景下 ,实现气象预报指导产品打包及上星广…  相似文献   

5.
针对人民银行计算机网络的应用一状,采用服务器/客户机模式,在UNIX系统下,实现了一种”快通工程”系统软件的设计。  相似文献   

6.
介绍了UNIX系统下的各类文件及其操作方法。  相似文献   

7.
介绍了SOCKET的基本概念和编程原理。UNIX网络下如何利用面向连接的SOCKET程实现客户机、服务器进程间通信进行了分析并给出了程序实例。  相似文献   

8.
谢海文  罗慧妮 《气象》1998,24(10):2-2
引言各地市“9210”工程中,与PES相连的节点机运行的操作系统是SCOUNIX,MI-CAPS系统运行于Windows95之上,MI-CAPS系统需要从节点机存取气象资料文件,这就涉及到Windows95访问SCOUNIX主机中的文件的问题。应用A...  相似文献   

9.
1 几种操作系统平台的特点当代计算机世界 ,尤其是PC机世界 ,作为主流操作系统的只有 4大类 :DOS、UNIX、OS/2和WINDOWS系列 ,如果从实时处理多任务的能力来看 ,它们各具特点 :DOS :作为PC机的第一代操作系统 ,从系统的本质上来讲 ,它既不是实时系统 ,也不能处理多任务。虽然一些资料和文章介绍了“DOS下任务切换”的方法 ,它们所采取的方法和技巧被DOS系统内核的缺陷所束缚 ,程序的性能和功能也受限制。UNIX :客观上说 ,UNIX从设计上就是为实时多任务处理而设计的 ,实时多任务处理已经包含在它的系…  相似文献   

10.
介绍了9210工程网站的访问方法、UNIX系统中文支撑环境安装步骤、代理服务器软件参数配置以及电子信箱的申请方法。这些经验可直接为他人借鉴,能尽快发挥9210工程的效益。  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.
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  
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   

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.
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   

16.
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   

17.
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   

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   

19.
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   

20.
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