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1.
设计ACTIVE—X控件实现BMP格式的卫星云图在网页中显示   总被引:1,自引:0,他引:1  
李凌  周飞 《广西气象》1999,20(3):43-44
通过对bmp格式的卫星云图显示控件设计分析,介绍activex控件的设计方法,并给出在网页中应用activex控件的方法。  相似文献   

2.
以“青海省三江源人工影响天气系统”开发为例,详细阐述了运用高级程序语言C#和组件WebGIS技术及控件Ma pObjects(MO)进行二次开发的人工影响天气燃烧炉应急系统的设计方法,充分体现了利用控件实现二次开发的优势和特点.  相似文献   

3.
本文介绍了人影作业申请空域的方法和流程,介绍了使用高级程序设计语言VB6.0、第三方控件和操作系统API函数编写的黑龙江省人工影响天气作业空域值班软件的功能、结构和实现方法.  相似文献   

4.
李红艳 《山东气象》2005,25(2):35-36
介绍数据库信息通用查询器的设计思路和原则,以及在PowerBuilder中利用数据窗口控件和用户对象生成通用查询器的方法,并给出实现的关键技术和源程序。  相似文献   

5.
介绍了C Builder中ADO数据库访问控件的属性及其使用方法,并以Access 2000数据库为例,给出了如何利用ADO控件对数据记录进行添加、查询的操作方法。  相似文献   

6.
本文介绍了使用高级程序设计语言VB6.0和第三方控件开发黑龙江省人工影响天气作业报表填报及汇总软件的设计思路和的功能、总体结构和实现的方法.该软件已经在实际业务中试用,该软件将提升本省人工影响天气作业报表填报及汇总的工作效率和数字化水平.  相似文献   

7.
M ICAPS 2.0是在M ICAPS l.0的基础上开发和完善的,在M ICAPS 2.0中增加了一个动态连接库和4个ACT IVEX控件,包括参数检索控件、辅助图表控件、数据分析控件和地理信息控件,增加了气象资料的文本和表格显示功能,增加了单窗口多屏显示功能,提供了新的图形图像操作功能和气象数据  相似文献   

8.
C++ Builder中基于ADO的数据库访问方法   总被引:1,自引:0,他引:1       下载免费PDF全文
介绍了C++ Builder中ADO数据库访问控件的属性及其使用方法,并以Access 2000数据库为例,给出了如何利用ADO控件对数据记录进行添加、查询的操作方法。  相似文献   

9.
潘永地 《浙江气象》2000,21(2):40-42
剖析ActiveX控件的代码结构,举例说明利用Visual Basic开发ActiveX控件的原理和过程以及如何运用自己开发的ActiveX控件在编程中实现特殊功能。  相似文献   

10.
Microsoft Chart Control(简称MSChart)是微软提供的一套强大的绘图控件,对基于微软.NET Framework3.5技术的最新版MSChart的特性、功能、组件和安装方法进行了详细介绍,并就如何应用MSChart控件在绘制丰富生动的气象数据图形中的几个关键技术进行了初步探讨.  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.
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   

14.
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   

15.
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   

16.
17.
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   

18.
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   

19.
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   

20.
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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