| 1. | Such reactions are called non-adiabatic .
这种反应叫做非绝热反应。 |
| 2. | It is found that the non - adiabatic heating plays an important role in the position variation of wpsh
结果表明，副热带地区的非绝热加热对副高位置变化有很重要的作用。 |
| 3. | Method for calculation of thermally permissible short - circuit currents , taking into account non - adiabatic heating effects
考虑非绝热效应因素的允许热短路电流的计算方法 |
| 4. | Simulation results for a non - isothermal cstr process demonstrate the effectiveness and efficiency of the proposed method
通过非绝热连续反应釜的仿真验证了本方法的有效性。 |
| 5. | It accords with its attribute of analytical solution . the results show that nonadiabtic heating strengthen kelvin cat " s eyes . cooling effect is adversed
结果表明非绝热加热强迫加强“ kelvin ”猫眼强度，冷却则相反，耗散则缓和流场演变。 |
| 6. | In comparison with climatic mean status , the vertical change of non - adiabatic heating is stronger in the north side of wpsh in june 1998 , but weaker in the south side of wpsh
与气候平均状况相比， 1998年6月副高北侧的非绝热加热垂直变化较常年偏强，而南侧较常年偏弱。 |
| 7. | ( 5 ) based on the complete form of vertical vorticity tendency equation , the effect of spatially non - uniform heating on the formation and variation of subtropical high is discussed
( 5 )运用全型垂直涡度倾向方程理论，研究了空间非绝热加热在垂直方向的变化对副高强度和位置变异的影响。 |
| 8. | First , in the field of atmospheric dynamics the developments in dynamics of diabatic waves and low - frequency waves , the dispersive effects of turbulence and nonlinear atmospheric waves are re - viewed
在大气动力学领域，主要介绍了非绝热波和大气低频动力学、湍流的频散效应和大气非线性波动等方向的研究进展。 |
| 9. | In order to study geometric phase expediently in chapter 3 and 4 , we have discussed the berry phase of quantum state evolving adiabatically and the aharnonov - anandan phase of quantum state evolving nonadiabatically
为了便于第三章和第四章中的几何量子计算问题的讨论，我们还在第二章中对量子态的绝热演化过程的berry相以及量子态的非绝热演化过程的aharnonov - anandan相作了概述。 |
| 10. | Results show that subtropical high in june 1998 is more intensive and westerly and than normal , leading to the floods in yangtze river valley . vertical diabatic heating has stronger impacts on the variation of intensity and location of western pacific subtropical high
结果表明： 1998年6 - 7月西太平洋副高较常年同期偏强偏西，从而导致了我国长江流域持续暴雨洪涝天气的发生；副热带地区的非绝热加热对副高的强度和位置的变化有极其重要影响。 |
