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generating     
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  生成
     Research on Generating Technique of Special Effects and Surface Simplification Technique of Object Models in Virtual Battlefield
     虚拟战场中特殊效果生成和实体模型简化技术研究
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     Research on Isomorphism Generating Method of Concept Lattices and Implementation of IsoFCA System
     概念格同构生成方法研究及IsoFCA系统实现
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     GENERATING FUNCTIONAL AND STRUCTURE OF VACUUM
     生成泛函与真空结构
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     A Program for Generating the General N Winograd Fourier Transform Algorithm (WFTA) Program
     一个能生成一般N Winograd傅里叶交换(WFTA)程序的程序
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     THE MINIMAL GENERATING SET OF FUZZY VECTOR CLASS AND THE SCHEIN RANK OF FUZZY MATRIX
     模糊向量组的最小生成集及模糊矩阵的Schein秩
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  产生
     A Method for Generating Uniform Random Number and Its Testing
     均匀随机数的一种产生方法及其检验
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     ON THE THEOREM OF GENERATING HAMILTONIAN CYCLES AND ITS APPLICATIONS
     关于产生哈密顿圈的定理及其应用
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     A Method of Generating the Standard Loran-C Pulse and Envelop Signal
     标准罗兰—C信号及包络信号的一种产生方法
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     A FAST COMBINATION METHOD FOR GENERATING N(0,1)RANDOM VARIABLES
     产生 N(0,1)随机变量的一个快速组合法
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     Generating MSK Signals by Means of SAW Devices——a New Method of MSK Signals Generation
     用声表面波器件直接产生MSK信号——一种产生MSK信号的新方法
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  发电
     Research on Nesting Optimization Principle and Key Techniques for Generating Equipment Manufacturing
     面向发电设备制造的下料优化排样原理与关键技术
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     The Wave Generating System Controlled by Microcomputer
     微机控制波力发电系统
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     Some Problems on Generating System Reliability Evaluation
     关于发电系统可靠性评估的一些问题
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     NEW FERRITIC STAINLESS STEEL FOR ADVANCED GENERATING UNIT
     先进发电设备用的一种新型铁素体不锈钢
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     Study on the Digital Simulation of Reliability of Interconnected Generating System
     互联发电系统可靠性的数字仿真研究
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  发生
     Design of 4.8 × 10~6 m3/a Acetylene Generating Station
     4.8×10~6 m~3/a乙炔发生站设计
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     Design for Acetylene Generating System of 4. 8 × 10~6Nm~3/a Acetylene Station
     4.8×10~6Nm~3/a乙炔站乙炔发生系统设计
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     Approaches to the Methods of Measuring Mercury through FIAS200 - AS90 Hydride Generating
     FIAS200-AS90氢化物发生原子化器测定汞方法探讨
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     The explicit expression of n+1 order matrix A = (αi,j)(n+1)×(n+1) is obtained by using generating function.
     用发生函数法得到了n+1阶矩阵A=(αi,j)(n+1)-(n+1)的精确表达式.
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     This paper deals with the autocorrrelation structure of product seasonal modelsΦ(B)Φ(B~8)x_t=θ(B)■(B~8)a_t by use of autocovariance generating functions,and finds out that for p=o,the model is parametersepar able.
     本文以自协方差发生函数为工具,讨论了乘积型季节性模型。 Φ(B)Φ(B~8)x_t=θ(B)■(B~8)a_t自相关函数的结构,证明了当p=0时,模型是参数可分离的。
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  generating
In the course of the proof we show that one can reduce the study of generating semi-invariants to the case when the quiver has no oriented paths of length greater than one.
      
We shall construct a generating set of a nonfinitely generated Ga-invariant ring given in Freudenburg's counterexample by making use of an integral sequence which was constructed inductively by Freudenburg.
      
This generating set shall be used in describing a generating set of a nonfinitely generated Ga-invariant ring given in Daigle and Freudenburg's counterexample.
      
Using these generating sets, we shall determine the Hilbert series of the above Freudenburg's and Daigle and Freudenburg's nonfinitely generated Ga-invariant rings, and find that these Hilbert series are rational functions.
      
A generating system for the algebra of semi-invariants of mixed representations of a quiver is determined.
      
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A new method of generating electric pulses of short duration with good amplitude and steadiness is devised by superposing two similar and opposite pulses produced with two glow discharge tubes. Confirming experiments are made and fully reported. A useful formula for passing a pulse through a transformer is also derived.

著者新拟一法以发生强大而稳定之短时脉流。其法系用二辉光放电管所发之同样而反向之脉流之较差;并详述其实验证明之结果。且对於脉流经过变压器,推出一适用之算术方式。

The synoptic process on 500mb over Asiatic natural synoptic region have been analized for 5 summers. The results are given below:1.The variation of the position and strength of the maximum westerly wind belt at 500mb surface along four meridians 65°E, 105°E, 120°E, 140°E gives a good index in determing the natural synoptic seasons over Eastern Asiatic synoptic natural region. The disappearence of the low latitude westerly wind maximum along 65°E is the first indication of the beginning of Bai-U period. When...

The synoptic process on 500mb over Asiatic natural synoptic region have been analized for 5 summers. The results are given below:1.The variation of the position and strength of the maximum westerly wind belt at 500mb surface along four meridians 65°E, 105°E, 120°E, 140°E gives a good index in determing the natural synoptic seasons over Eastern Asiatic synoptic natural region. The disappearence of the low latitude westerly wind maximum along 65°E is the first indication of the beginning of Bai-U period. When the westerlies wind maximum belt to the south of 40°N completely disappears along 140°E summer begins. This is accompanied with the filling of the Asiatic main trough over Japan and the Northward shiff of the Pacific subtropical high pressure belt from low latitudes to 30°-40°N. The mean date on which summer begins is nearly on 13th, July. It is also the end of Bai-U over middle Yangtze river. Thence the synoptic process in Bai-U period is the prevailing process before summer season. The precipitation in this period is closely related to the strength of the maximum wind belt i.e. socalled frontal zone.2.When the 600mb maximum westerly wind belt appears again at 30°-40°N along 140°E, begins author. The synoptic process, which associates with it, is the reestablishment of the Asiatic main trough over Japan. And the surface cold continental high comes down to North China from the east of Novaya Zemlya Island. The average time of the arrival of Autumn is nearly on 5th, September. Hence the duration of summer is on the average only 55 days.8. According to the analysis of the time variation of maximum westerlies on 30°-40 °N along each of the four meridians, the westerly maximum generally disappears earlier in west than in east but establishes later in west than in east during autumn. The phenomeanon that the maximum westerly first generates in the east during autumn can hardly be explained by the splitting of the jet stream.4. From the analysis, the prevailing process of the natural summer season largely depends upon the variations in the upper westerlies over Ural region and the west-east relative position of the Pacific subtropical high with respect to the Tibet plateau.

本文根据1951—1955年五年高空和地面的资料,对夏季过程进行了分析,得到下面几点结果: 1.在东亚地区的四个主要经度带上以65°,120°和140°经度带的500毫巴强西风中心的位置和强度变化,对东亚自然天气季节的划分是最良好的指标。东经65°经度带上南边低纬度强西风的消失是梅雨期开始前的征兆。东经140°经度带上强西风在北纬40°以南消失时是夏季开始的征兆。和它相关联的过程是东亚高空大槽的消失和太平洋副热带高压带北移至30°—40°纬度带间,这个期间平均是在7月13日左右,也是江南梅雨结束的时候。故梅雨是夏季以前的盛行过程,它和500毫巴强西风区或锋区是有密切的联系的。 2.东经140°经度带上500毫巴强西风在北纬30°—40°重现时,是夏季结束秋季开始的征兆,和它相关连的天气过程是在该经度带上高空大槽重新建立,地面大陆冷高压从新地岛东部向东南下达华北地区。这个时间平均是在9月5日左右。故东亚夏季的长度平均仅55日。 3.从500毫巴强西风在各经度带上出现的情况来看,一般是西部比东部消失得早,出现得迟,不如冬季那样先在上游首先建立,在春夏之交这种相反的演变,似非地形的分支可以解释的。 4.在夏季自然天...

本文根据1951—1955年五年高空和地面的资料,对夏季过程进行了分析,得到下面几点结果: 1.在东亚地区的四个主要经度带上以65°,120°和140°经度带的500毫巴强西风中心的位置和强度变化,对东亚自然天气季节的划分是最良好的指标。东经65°经度带上南边低纬度强西风的消失是梅雨期开始前的征兆。东经140°经度带上强西风在北纬40°以南消失时是夏季开始的征兆。和它相关联的过程是东亚高空大槽的消失和太平洋副热带高压带北移至30°—40°纬度带间,这个期间平均是在7月13日左右,也是江南梅雨结束的时候。故梅雨是夏季以前的盛行过程,它和500毫巴强西风区或锋区是有密切的联系的。 2.东经140°经度带上500毫巴强西风在北纬30°—40°重现时,是夏季结束秋季开始的征兆,和它相关连的天气过程是在该经度带上高空大槽重新建立,地面大陆冷高压从新地岛东部向东南下达华北地区。这个时间平均是在9月5日左右。故东亚夏季的长度平均仅55日。 3.从500毫巴强西风在各经度带上出现的情况来看,一般是西部比东部消失得早,出现得迟,不如冬季那样先在上游首先建立,在春夏之交这种相反的演变,似非地形的分支可以解释的。 4.在夏季自然天气季节所出现的盛行天气过程主要是表现在太平洋副热带高压随上游气压场的不同,及其和?

Utilizing the latitudinal mean ot upper meridional wind of 1950 given by Buch and Starr and White, mean meridional circulation has been studied. Fig. 1-3 (fig. 1 for whole year, fig. 2 for winter, fig. 3 for summer) reveal three cells: two direct cells in low and high latitudes respectively and one indirect cell in middle latitudes. The average jet stream of 1950 is situated in the middle cell. The yearly average equatorial convergence zone is at about 5°N. From winter to summer all the three cells shift northward....

Utilizing the latitudinal mean ot upper meridional wind of 1950 given by Buch and Starr and White, mean meridional circulation has been studied. Fig. 1-3 (fig. 1 for whole year, fig. 2 for winter, fig. 3 for summer) reveal three cells: two direct cells in low and high latitudes respectively and one indirect cell in middle latitudes. The average jet stream of 1950 is situated in the middle cell. The yearly average equatorial convergence zone is at about 5°N. From winter to summer all the three cells shift northward. The Hadley cell of winter hemisphere extends to summer hemisphere. The intensity of these cells seems to be stronger in winter than in summer.Angular momentum balance for the latitudes 10°N-70°N for the year 1950 was also studied, and figure for stream lines for the transfer of angular momentum was constructed (fig. 5). The most interesting feature in this figure is that through the surface separating easterlies and westerlies the stream lines are vertical. Thus it indicates that the angular momentum generated in the easterlies is transported to the westerlies not in horizontal direction, but transported to upper westerlies in low latitudes by vertical motion. Then from there it is tiansfer-ed to middle latitudes. The mechanism of such transfer is as follows: In Hadley cell the upward motion in equatorial region and southern tropics carries more angular momentum due to earth's rotation, while the downward motion in northern tropics and subtropics carries less angular momentum due to earth's rotation. Thus in the mean angular momentum generated in easterlies is transported to upper levels.Finally the mechanism of maintenance of zonal circulation was discussed. The conclusion is this: In middle arid high latitudes gross disturbances are of primary importance while in low latitudes mean meridional circulation is important in maintaining zonal circulation.

本文利用了Buch和Starr与White所计算的1950年各纬度上空的平均经向风速([V]),绘制了子午面上的平均环流(全年:图1,冬季:图2,夏季:图3),图中显示出三个环型(cell),低纬度和高纬度的两个正环型与中纬度的逆环型。 1950年平均西风急流的位置正好处于中纬度的逆环流之中。全年平均的赤道辐合线位于北纬5°左右。自夏至冬三个环型均向北移,冬季半球Hadley环型伸向夏季半球去。三个环型的强度都是冬季大。 对于1950年北半球10°—70°的角动量平衡也作了分析(图4),并绘制了这个空间中角动量输送流线图(图5),其中应该提出,就是通过东西风的界面流线是铅直的,也就是总的来说,在东风带里产生的角动量不是在水平方向上输送到西风带里去,而是在铅直方向上输送到低纬度的高空西风里去,再由那里在水平方向上送到中高纬度去。 最后对于平均纬圈环流的维持也作了讨论,结论是:在中高纬度大型扰动起着主导作用,在低纬度则平均经圈环流是重要的。

 
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