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Home > chinese-english > "振荡强度" in English

English translation for "振荡强度"

oscillation intensity

Related Translations:
振荡调制:  modulation of oscillations
载波振荡:  carrier oscillation
振荡波长:  oscillation wavelengthwavelength oscillation
反馈振荡:  feedback oscillation
电路振荡:  circuit oscillation
振荡碰撞:  generating collision
激波振荡:  shock oscillation
过度振荡:  overshoot oscillation
相干振荡:  coherent generationcoherent oscillations
振荡叠加:  oscillation superpositionsuperposition of oscillations
Example Sentences:
1.As the injection current is increased above the threshold value (10.7-24), the laser oscillation intensity builds up .
当注入电流增加到由式(107-24)表示的阈值以上时,激光振荡强度就会增长。
2.As the injection current is increased above the threshold value ( 10 . 7 - 24 ) , the laser oscillation intensity builds up
当注入电流增加到由式( 10 7 - 24 )表示的阈值以上时,激光振荡强度就会增长。
3.When the ecld jumps down , at the first stage , the output power reduces quickly , and then experiences an oscillation process which will appear later , the intensity of the oscillation at the initial stage will increase
在下跳初始阶段经历的衰减过程中,输出衰减变快。对于衰减后的振荡,起振时间将会推迟,初始振荡强度有所增加。
4.2 ) the olr mjo intensity anomaly for the four key areas of the pacific , namely , the tropical western pacific , the middle and eastern pacific , the northwest pacific and the southwest pacific , is significantly and positively related to the local ssta
2 )太平洋四关键区(热带西太平洋、热带东中太平洋、西北太平洋、西南太平洋)的olr季内振荡强度与sst异常呈显著局地同时性正相关关系。
5.When a net flow was introduced , the result seemed to take great changes , but the tendency is the same as that without net flow . the correlation between injection dispersion character and ren reduces with the oscillatory intensity increasing
引入净流量后实验结果发生了很复杂的变化,但总体变化趋势仍与无净流实验一致,当振荡强度加大后,即随振幅、频率的提高,流场注入分散特性与re _ n的联系逐渐减弱。
6.During the el nino ( la nina ) events , the negative ( positive ) sst anomaly occurs and the corresponding the olr mjo intensity weakens ( enhances ) in the tropical western pacific ; at the same time , the positive ( negative ) surface westerly anomaly leads to positive ( negative ) mld anomaly , and the corresponding sst mjo intensity weakens ( enhances ) in the equatorial eastern pacific , 4 ) the interdecadal variation of the atmospheric mjo intensity took place distinctly in 1970s in the tropical western , northwest and eastern pacific , with the stronger intensity in the former than the back stage , and the interdacadal variation of sst is its cause
Elnino ( lanina )事件中热带两太平洋sst出现负(正)异常, olr季内振荡强度出现减弱(增强)的变化。 elnino ( lanina )事件中,赤道太平洋出现地面信风西风分量正(负)异常,并引起热带东太平洋mld出现正(负)异常,造成热带东太平洋sst季内振荡强度出现减弱(增强)的变化。 4 )热带印度洋、热带西太平洋和热带东太平洋季内振荡强度在上世纪70年代发生了明显的年代际变化,均为前弱、后强, sst本身的年代际变化是其原因。
7.The heat transfer enhancement is different under different oscillator . there is the optimum oscillation intensity under which the heat transfer coefficient will be increased by about 30 percent . the change of outlet structure size of a resonance chamber shows little effect on the strength of heat transfer : the pressure of the optional heat transfer coefficient always is between 0 . 4mpa and 0 . 6mpa , and the optional heat transfer coefficient is enhanced by 30 percent or so
不同的振荡强度,强化换热的效果也不同,存在一个最佳强度,此时的强化换热效果最好,可以将表面换热系数提高30 %左右;对于同一共振腔,配合以不同的出口结构尺寸,对于换热效果的强化的影响变化不大:出现最佳强化效果时的压力基本都在0 . 4 - 0 . 6 ,最佳的强化效果也都是将表面换热系数提高30 %左右。
8.It is shown that olr spread eastward more clearly in the eastern hemisphere , and the x is persistently spread eastward in both hemisphere ; the interannual variability of the spread of mjo is evident , with the intensity weakening during el nino events and sometimes spreading westward in individual years
气候上,在沿赤道的传播中, olr东半球较西半球明显, x东、西半球无显著差别;两种要素季内振荡沿向东南路径的传播较向东北路径的传播特征明显。异常表现为季内振荡强度在elnin 。
9.With the exception of the tropical western pacific of large mld . there is negative correlation relationships between the anomaly of the sst mjo intensity and that of the mld in the other three regions in the seasons of the climatic small mld thus the causes of climatic and anomalous characteristics of atmospheric mjo are related to sst identically , and the corresponding features of sst mjo are related to mld , 3 ) enso is the strongest sign and can lead to the distinct sst and mld anomaly , hence the intensity anomaly of the air - sea system inevitably takes place during the enso
Sst季内振荡强度与mld异常的局地同时性相关结果是,热带西太平洋无显著相关(气候mld较大) ,其余三关键区气候mld小的季节均存在sst季内振荡强度与mld异常的负相关联系。因此大气季内振荡气候及异常特征直接成因一致地与sst 、有关;海洋季内振荡相应特征则直接与mld有关。 3 ) enso是海气系统中最强异常信号,在海洋中它引起了sst 、 mld的明显异常,因此,伴随enso必然发生海气系统季内振荡强度的异常。
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