- 更多网络例句与再分析相关的网络例句 [注：此内容来源于网络，仅供参考]
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Use 1 ° of NCEP1 °× to analyse data, T213 to analyse data and groovy observation data again, wait for a respect from moisture requirement, heating power condition, motivation condition, to the reason that method of " of Aeolus of " of the 6th typhoon, intensity changed 2008, reach its to undertake an analysis to the influence of Jiangxi.
梗概： 利用NCEP1°×1°再分析资料、T213分析资料和常规观测资料，从水汽条件、热力条件、动力条件等方面，对2008年第6号台风"风神"路径、强度变化的原因，及其对江西的影响进行分析。
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Based on the reanalysis of JEDAC datasets and the assimilation of SODA, the authors studied the variation of the heat status in the West Pacific Warm pool and discussed the ocean temperature variety in the heat content at different depths, the inherent relations between ocean temperatures at surface and subsurface, the eastward propagation of anomalous ocean temperature and the thermocline variation, and the influence of equatorial undercurrent on the eastward propagation.
中文摘要：应用 JEDAC 海温和SODA 再分析资料，分析研究了西太平洋暖池的热状况变化特征，探讨了WPWP 的热含量变化与不同深度海温变化，特别是与表层和次表层海温场之间的内在联系，分析研究了WPWP 异常海温东传过程中与温跃层变化之间的关系，最后讨论了赤道潜流在异常海温东传过程的作用。
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This method is made use of the matrix series expansion to construct modified structure′s vibrating response reanalysis approach based on mechanical impedance method.
而结构振动响应的再分析方法则研究得较少，目前主要有两种方法：一是矩阵摄动法，另一种是从静态位移再分析方法引申得来的方法[1]。
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The advances in reanalysis in China ars introduced simply and some problems on the improvement of the reanalysis in China are discussed.
简单陈述了国内再分析工作的进展，并给出了提高我国再分析工作质量所需要关注和亟待解决的问题。
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A response reanalysis approach of structure under harmonic or periodic excitation has been studied with original vibrating response.
再分析方法已应用到诸多领域，如结构静响应的再分析，结构振动模态的再分析，这些方面的研究已取得很大进展。
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This study tries to reanalyse and revaluate his ideas of education basing research on "The Chronology of Tan Ssu-Tong" and "The Anthology of Tan Ssu-Tong", in the hope of getting a more complete picture of his thoughts on education.
於是本研究基於客观的观点将谭嗣同的教育思想欲以再分析、再评估，并在研究方法上主要采「谭嗣同年谱」及「谭嗣同全集」为轴的文献分析法，以达提高对其教育思想的正确认识。
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Meanwhile the results also showed that the main cause of which the GAME reanalysis data being better than the NCEP reanalysis data is the GAME reanalysis data including the sonde data of the GAME but not the different assimilation modes of the two reanalysis data.
通过对GAME外场试验期和非试验期的GAME与NCEP两组再分析资料进行对比分析，我们得到，GAME再分析资料优于NCEP再分析资料的主要原因是GAME的资料同化系统中加入了包括HUBEX等气象科学试验的探空加密观测资料。
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According to the energy conservation theory, BOM and CSIM4 were coupled. The BOM has no treatment on transmission solar radiation, which is of great importance when the model is adapted to Arctic Ocean. So the treatment was introduced to BOM. Through numerical test on different lead albedos, it was found that sea ice thickness is not so sensitive to lead albedo, which may be contribute to the lead occupies little ratio within multiyear sea ice pack. The reason of summer over-melt of arctic sea ice is the NCEP reanalysis downward solar radiation being larger than its reality. Then the arctic sea ice climate variability was simulated. Results showed that: simulated ice thickness change is in accord with the submarine investigated mean sea-ice draft changes. Simulated annually maximum ice thickness along the Eurasian continental oceans are closely related to the observed ones. The long-term mean simulated ice motion has the same features of the SSM/I derived ice motion. Sea ice extents in differential sub-regions have same trends comparing to the satellite passive-microwave data derived ones. Simulated ice concentration is closely related to the observed in the Arctic sub-regions. Sea ice flux through the Fram Strait involves ice concentration, motion and thickness. It is a composite criterion for sea ice model evaluation. The simulated ice area and volume export through the strait accord with the satellite derived or statistically reconstructed ones.(5) The simulated ice thickness climate variability and mean sea surface current of the coupled model were analyzed, results showed: the total ice volume in the Arctic Ocean has a significant decreasing trend. The volume variability is of a 10-year timescale oscillation, with two major periods of 12-13a and 18-20a. Mean ice thickness in the arctic sub-seas has different tendencies. It has an increasing trend in the Barents-Kara Sea and Baffin Bay-Labrador Sea, and decreasing in the others. The characteristic time scale of 7-10a wherein the river discharges leads the Fram Strait ice volume export is about the period that river water takes to be conveyed across the Arctic Ocean.(6) Using the simulated ice distribution in the Arctic Ocean and China precipitation, air temperature and SST in tropical key regions, the climate teleconnection were studied. Result showed: When the mean sea ice thickness is large in the central Arctic Ocean and Chukchi-Beaufort Sea , and small in the Barents-Kara Sea and Baffin Bay-Labrador Sea , the precipitation in South China, Tibetan Plateau, and the north part of Northeastern China are always smaller than normal, and v. v. When the mean ice thickness is small in CA, BC, East Siberian Sea and Greenland-Iceland-Norwegian Sea , and large in BL, The air temperature in north-eastern China, the southern of Tibetan Plateau, and Hainan Island, are always lower than normal, and v. v. In addition, when the sea ice is thick in BC and BL, the SST is larger in the middle and eastern Pacific Ocean, and is smaller in the tropical Southeastern Indian Ocean.
由于BOM没有考虑透射太阳辐射的物理过程，研究表明透射太阳辐射对北冰洋的能量收支起到重要作用，因此在BOM模式中引入了对透射太阳辐射的处理；通过对不同水道反照率的数值试验表明海冰厚度对水道反照率的敏感性不强，可能与海冰区水道面积占的比率很小有关；而模式模拟的北极海冰夏季&过度融化&主要源于NCEP再分析资料提供了偏大的太阳短波辐射；对北极海冰的气候变率进行了模拟研究，结果表明：模拟的海冰厚度变化与潜艇探测的海冰吃深度变化具有一致性；模拟和观测的亚欧大陆沿海的年内最大海冰厚度有很好的相关；模拟的海冰移速与长期平均的卫星反演的海冰移速具有相同的速度分布特征；模拟的各个海区海冰面积的变化趋势与卫星反演资料分析的结果基本一致；模拟与观测的主要海洋分区的海冰密集度具有很好的相关：弗瑞姆海峡的海冰体积和面积的输送涉及到海冰密集度、厚度和移动速度，是判断模式模拟能力的一个综合的指标，模式模拟的结果与卫星反演或重建的面积输送、体积输送具有很好的一致性；(5)分析了模拟的北极海冰厚度的气候变率及气候平均表层海流场，结果表明：北极海冰的总体积有显著减少的趋势，北极海冰总体积的变化具有10a际尺度振荡的特点，存在18-20a和12-13a两个主周期；北极海冰的平均厚度在各个海区的变化趋势不同，在巴伦支—喀拉海和巴芬湾—拉布拉多海地区海冰厚度有显著的增加趋势，而其它海区存在减少的趋势；通过对模拟的气候平均表层海流的分析表明，北极河流流量超前弗瑞姆海峡海冰流量7-10年的特征时间尺度与表层海流的气候分布存在着必然联系：(6)利用模拟结果以及中国降水、气温和热带关键区SST资料，讨论了北极各海区海冰平均厚度与中国降水、气温以及热带关键区SST的关系，结果表明：在北极中心海区和楚科奇—波弗特海海冰厚度偏大，在巴伦支—喀拉海以及巴芬湾—拉布拉多海海冰厚度偏小，则中国降水在华南地区、青藏高原和东北北部降水偏少，反之相反；在北极中心海区、东西伯利亚海、楚科奇—波弗特海以及格陵兰海海冰厚度偏小，在巴芬湾—拉布拉多海海冰厚度偏大，则在中国东北地区、高原南部地区和海南岛附近气温偏低，反之相反；另外，北极楚科奇—波弗特海和巴芬湾—拉布拉多海海冰厚度偏大时，在热带中东太平洋海温偏高，而在热带东南印度洋海温偏低。
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Based on NCEP/NCAR reanalysis data, the structure and variation of Tropical Easterly Jet and its relationship with the distribution of rainfall in Asia and Africa are analyzed. In addition, the Asian summer monsoon indices are reappraised and the secular variation of monsoon is studied.
本文主要是用NCEP/NCAR再分析资料研究了热带东风急流的结构，多尺度变化特征及其与亚非季风降水的关系，并且在此基础上重新评估亚洲夏季风指数及研究季风的长期变化，最后比较了NCEP/NCAR与ERA-40再分析资料的差异。
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objective the overall quantity of the examination section management and the establishment of the system is the key to guarantee the quantity and raise the examination level,which is needed by laboratory management and actual work.methods overall quality management of laboratory was divided into 3 parts,that was quality control before,during and after analysis.examination process was made standard in the construction and uparading of laboratory information management system,which ensured the optimal examination was chosed and samples quality control before analysis,perfect quailty control system and standardized management were used throughout the analysis,re-analysis and re-ensurance of the examination results were performed.results lims was constructed with the characteistics of perfect function,easy performing and effective management.conclusion lims rums smoothly and realize the overall quality management successfully.
在医学检验中，全实验室质量管理分为3个阶段，即分析前质量控制、分析中质量控制和分析后质量控制。在临床检验信息管理系统的网络建设、网络改造升级中规范检验流程，确保分析前医生从循证医学的角度选择最合理、最经济的项目检测，并控制护士标本的采集、保存与运送的质量；分析中，完整的质量体系和标准化、规范化管理始终贯穿于检验科的检测中。分析后，实验结果的再分析，再确认，保证合格报告的发出，保证实验结果及时发给临床后，临床医生能合理地分析报告，正确的运用数据，用于诊断和治疗。结果功能齐全、操作简便、高效管理的临床检验信息管理系统建立。结论该系统运行效果良好，更新完善了检验科的管理模式，较好的实现了全实验室质量管理。
- 更多网络解释与再分析相关的网络解释 [注：此内容来源于网络，仅供参考]
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correlation analysis：相关分析
建立及管理这样一个好配置的方法有二:相关分析(correlation analysis)和再平衡(rebalancing). 麦氏的贡献在於科学配置法:对诸种资产的历史风险及回报做相关分析. 目标是找到表现不同的资产来建造组合. 最基本的分析是两种资产(例如美国股票和美国债券)的历史相关,
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dipole：偶极子
[摘要]用1955年1月-2001年12月美国Scripps海洋研究所的海温再分析资料、美国NCEP再分析资料和美国气候预测中心(CPC)资料,讨论了热带太平洋ENSO与热带印度洋海温距平以及与印度洋偶极子(Dipole)的关系,研究结果发现:在垂直最大温度距平曲面(MTAL)上,
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Discriminant analysis：差别分析
在一到十的尺度上 ,为自己的属性评级.我们再运用因素分析(factor analysis)、群集分析(cluster analys is)和差别分析(discriminant analysis)等多变数统计技术,将消费者区隔成十种消费族群 ,
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event tree analysis：事件树分析法
此图为事件树分析法(event tree analysis)与鱼刺图分析结合而成,即包含了2种完全对立的状态,也分析了质量特性结果与可能影响质量结果特性的因素,如果能加入事故树分析的完整门规则和与非门规则的,同时能再把出现各种状态的概率进行测算的话,
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morphological analysis：形态分析法
形态分析法(morphological analysis)是兹维基(Zwicky)和艾伦(Allen)所提倡. 以结构分析为基础,再使用组合技术,来产生更多的新观念. 实施时,下列的步骤可供参考.
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pedigree analysis：系谱分析法
系谱分析法(pedigree analysis)是了解遗传病的一个常用的方法. 其基本程序是先对某家族各成员出现的某种遗传病的情况进行详细的调查,再以特定的符号和格式绘制成反映家族各成员相互关系和发病情况的图解,然后根据孟德尔定律对各成员的表型和基因型进行分析.
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pedigree analysis：系谱分析
系谱分析(pedigree analysis)是了解遗传病的一个常用的方法.其基本程序是先对某家族各成员出现的某种遗传病的情况进行详细的调查,再以特定的符号和格式绘制成反映家族各成员相互关系和发生情况的图解,然后根据孟德尔定律对各成员的表现型和基因型进行分析.通过这样的分析,
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reanalysis：再分析
ancova 共變數分析 | reanalysis 再分析 | re-cutting 再切分;重切段
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reproducibility：再生性
答:GRR是指量测的再现性(Repeatability)与再生性(Reproducibility)再生性(Reproducibility)则希望获知不同条件下的变异,因此取得数据时应符合下列条件:方差分析法(ANOVA)是一种标准的统计技术,可用来分析测量误差和测量系统分析中数据的其它变异源.方差分析中,
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Re-employment funds：再就业基金
比率分析 ratio analysis | 再就业基金 Re-employment funds | 富余职工再就业 Re-employment of redundant workers