从人力资源管理探讨防雷工作的发展

人力资源管理是现代企业管理的重要内容,对企业的发展至关重要。防雷产业的发展同样离不开人力资源管理,从人力资源管理的角度探讨防雷产业的发展。     

气象企业如何发挥人力资源管理的作用

随着市场竞争和气象产业的集团化发展趋势,一方面是对人才的高需求,另一方面由于体制改革尚不彻底和企业不完全竞争等多种因素所造成的人员过多和人才短缺,企业人员包袱过重,成为制约气象产业发展的“瓶颈”。气象企业如何扬长避短,最大限度地开发和利用现有人才资源,已成为我们必须深入研究的问题。1　气象企业的人力资源管理与现代知识经济要求的差距在知识经济的时代,企业领导人要迅速转变观念,要意识到人力资源管理将成为企业的一条腿,在市场经济中带动企业去跑。怎样求才、知才、用才、育才是每个成功企业管理者必需重视的问题。合…     

人力资源信息采集统计系统操作的实用技巧

<正>1引言随着信息化时代的发展,无论是机关、事业单位、还是企业单位,人力资源管理对于其生存与长远发展所起的作用日趋重要化。中国气象局以现代信息技术为平台,研发了《人力资源信息采集统计系统》,在系统内实现了人力资源的信息化管理。它主要的功能是信息的采集,归类,以及采集后的反查;可以服务于任何具有层次关系的单位和部门,能够同时完成对人事、教育和劳资3种资源的信息采集,极大地方便了用户对信息采集工作的管理。     

气象部门国有企业人才队伍建设问题及对策研究——以华云和华风集团为例

对人的管理是现代企业管理的核心,人力资源管理是企业核心竞争力的重要方面。对气象部门国有企业人才队伍进行分析研究,有利于深化气象部门国有企业改革,对于提高企业核心竞争力和人力资本的有效利用具有重要意义。1气象部门国有企业总体情况2018年气象部门所属法人企业共1227户,主要经营业务包括专业气象服务、气象仪器设备研发生产销售、防雷、气象信息服务、广告等,从业人员共计12309人。     

气象部门企业人力资源外包的动因、风险和防范策略

随着气象部门企业的发展,管理方式的变化,国内人力资源外包应运而生,以便降低成本,提高效率,提高气象部门企业的竞争力,本文从分析目前气象部门企业的人力资源管理现状、外包的风险及防范策略,提出外包的项目.     

关于气象部门引进人才的量化测评方法的研究

现代人才测评是综合运用定量与定性的方法，对人才进行客观、准确评价的一种社会活动。本文在对国内外人才测评的发展、现代人才测评理论和方法进行必要阐述的基础上，提出如何在我国气象事业人才战略发展中引入人才测评机制，同时，尝试提出建立具有针对性的测评体系的设想，旨在推进中国气象局有关部门在人才资源管理上，适度引进和应用一些比较成熟的人力资源管理理论、方法和技术，以满足实施人才战略的需要。     

关于考核反馈的思考

1人力资源管理关于绩效考核的理论 1．1绩效考核的内容和目的 人力资源管理理论认为，绩效考核是组织的内部管理活动，是组织在执行经营战略、进行人力资源管理中的日常活动。根据实际情况和职务要求，对员工的实际贡献进行评价，强调每个人、每个岗位的特殊性。从执行结果看，它包含对人的管理、监督、指导、教育、激励和帮助等功能。     

创新基层气象部门人力资源管理模式实现人才效益最大开发

我国基层气象部门尤其是经济欠发达地区的气象部门，由于历史原因和事业单位长期处在计划经济体制下形成的人事管理的思想和方法，使得大多数单位的人力资源管理工作，无论是在理念上还是在操作上都存在诸多问题，从而形成了制约事业发展的樊篱。因此，必须清醒地认识目前基层气象部门人力资源管理中现有矛盾，牢固树立人力资源是气象事业快速发展的第一资源理念。本文针对目前基层气象部门人力资源管理的新变化以及存在的矛盾进行了分析，提出了解决问题的六点建议。     

陕西多普勒天气雷达监测信息发布系统的开发与应用

气象科技型企业是顺应发展需要,在气象事业结构调整中产生的按公司化运行的创收实体。本文分析了该类企业人力资源开发与管理的现状和存在问题,并针对性地提出了对策建议。     

简析人事档案在人力资源管理中的作用

简要介绍了人事档案与人力资源管理的关系及其在人力资源管理中的作用,结合气象部门人力资源信息采集统计系统的应用,分析总结了人力资源管理中人事档案资料信息化过程中存在的不足,以期引起关注。     

加强业务管理提高测报质量

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.     

On the forecast of the onset and end of the convective season in the Amazon

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     

准两年振荡对大气中微量气体分布的影响

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。     

Comparing the theoretical versions of the Beaufort scale, the T-Scale and the Fujita scale

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.     

Quantifying the uncertainty of the annular mode time scale and the role of the stratosphere

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.     

Analysis of the Characteristics of the Low-level Jets in the Middle Reaches of the Yangtze River during the Mei-yu Season

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...     

流场配置及地形对西南低涡形成的动力作用

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.     

由中国历史气候记录对季风导致唐朝灭亡说的质疑

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.