对职工教育培训工作的认识

主要从职工教育培训工作的必要性和思想文化教育、岗位技能培训两方面的内容，谈对职工教育培训工作的认识。     

广西气象部门职工对气象教育培训需求的差异比较及分析

在广西气象部门1500多位职工关于气象教育培训需求调查的基础上,对不同单位(级)类别、不同年龄、不同工作年限、不同学历层次职工的气象教育培训需求差异进行比较分析,探寻其中的不同点和规律,并对如何满足职工的气象教育培训需求提出了若干建议。     

实施人才战略培养一流人才

在信息化迅猛发展、高新技术日新月异的今天,强调建设学习型部门,加强人才工作具有重要的现实意义.南阳市气象局结合本部门工作实际,采取有效措施,强化职工教育培训,努力建设一支一流的气象人才队伍.     

落实人才强局战略 改进教育经费管理

在实现中国气象局党组制定的新世纪各项奋斗目标和发展战略中，如何使气象部门在职职工不断完善自身的知识结构、能力结构．从而提升队伍的总体实力．是各级人事部门面临的一个新课题。职工教育培训作为整个人事人才工作的一个基础环节．在落实自治区气象局党组制定的人才强局战略中。承     

气象远程教育培训系统省级站的构建及应用

概述了气象远程教育培训系统省级站在职工教育培训方面的重要性,介绍了气象远程教育培训系统省级站构建的设计功能与目标,提出了气象远程教育培训系统省级站在网络结构、网络安全、设备选型等方面的技术方法,解读了分布式视频服务器软件、流媒体课件录制软件的功能和实用技术,并通过实例,说明了省级远程教育培训系统在加强气象职工教育培训、提高气象职工素质方面所发挥的积极作用。     

关于改进岗位培训工作的思考与建议—2007年度岗位培训工作调查报告

根据业务技术改革顶层设计确定的工作目标,2007年教育培训体系在实施过程中,把工作重点放在围绕现代气象业务建设开展职工岗位培训工作上,全区各级气象部门充分发挥积极性,先后举办231期培训班,有5400余人参加脱产学习,4000余人参加远程网络教育,教育培训工作呈现出前所未有的大好局面。为了总结经验,改进工作,     

围绕大局 求真务实 努力开创气象教育培训工作新局面——在2005年全国气象教育培训工作会议上的讲话

同志们：上午好!今天我们在这里召开全国气象教育培训工作会议，这是一次专门研究和部署新形势下如何围绕气象事业发展的大局，加强气象教育培训工作的重要会议。这次会议的主题是：认真回顾总结近年来气象教育培训工作取得的成绩和经验，深入分析气象教育培训工作存在的不适应问题；认清气象教育培训工作面临的新形势和新任务，研究部署新形势下加强气象教育培训工作的思路和主要任务，努力开创气象教育培训工作的新局面。     

仿真教学法在气象教育培训中的探索及研究

随着教育培训理念的发展,现代教育培训法在我国职业教育培训中也得到了广泛应用,其中仿真教学法由于注重理论和实践的高度融合,受到各行业的推崇。结合已有的培训研究成果以及气象部门仿真教学法在职业教育培训中的实际应用,设计了仿真教学法在气象教育培训中的培训模型,并进一步分析设计了地面综合气象观测仿真培训模式和流程,为仿真教学法在气象部门职工教育培训中的推广应用提供借鉴作用。     

实施人才战略 培养一流人才

在信息化迅猛发展、高新技术日新月异的今天,强调建设学习型部门,加强人才工作具有重要的现实意义。南阳市气象局结合本部门工作实际,采取有效措施,强化职工教育培训,努力建设一支一流的气象人才队伍。1　人才队伍现状南阳有 11个县市局,在职职工 171人,大专以上学历 61人,占 36% (其中研究生 1人,本科生 14人 );高级职称 11人,占 6%;中级职称 73人,占 43%。存在的主要问题有:一是高层次人才,尤其是在天气气候方面学科带头人缺少;二是高级专业技术人员所占比例偏低,特别是县局的基础业务队伍中没有经过正规培训的人员占从事基础业务人员…     

赴俄罗斯教育培训机构访问总结

为促进培训中心的能力建设,交流气象水文教育培训经验,应俄罗斯联邦水文气象和环境监测局的邀请,以中国气象局培训中心主任高学浩为团长的中国气象局培训中心代表团一行4人,于2008年4月21～26日对俄罗斯水文气象及环境监测局（Roshydromet）及世界气象组织（WMO）俄罗斯区域培训中心（RTC）进行了工作访问。本次访问的任务是了解俄罗斯气象业务及气象教育培训的工作情况,签署中俄气象教育培训合作计划。     

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.     

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.     

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.     

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     

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.     

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。     

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.