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强迫耗散
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  forced dissipative
     A Forced Dissipative Nonlinear Critical Layer and Numerical Experiments of Subtropical High
     强迫耗散非线性临界层与副高演变的数值试验
短句来源
     Forced dissipative nonlinear evolution equation and complete square conservative difference scheme
     强迫耗散非线性发展方程与完全平方守恒格式
短句来源
     Computational Stability of Explicit Difference Schemes of Forced Dissipative Nonlinear Evolution Equations
     强迫耗散非线性发展方程显式差分格式的计算稳定性
短句来源
     PRELIMINARY RESEARCH OF DYNAMICS FOR A FORCED DISSIPATIVE NONLINEAR CRITICAL LAYER
     强迫耗散非线性临界层动力学的初步研究
短句来源
     Computational Stability of the Explicit Difference Schemes of the Forced Dissipative Nonlinear Evolution Equations
     强迫耗散非线性发展方程显式差分格式的计算稳定性(英文)
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  force dissipation
     Ordered structure and system development of the force dissipation system(Ⅱ), Minimal value principle of generalized energy and system development
     强迫耗散系统的有序结构和系统的发展(Ⅱ),广义能量极小值原理和系统的发展
短句来源
     Ordered structure and system development of the force dissipation system(Ⅰ), Principle of minimum entropy production and ordered structure
     强迫耗散系统的有序结构和系统的发展(Ⅰ),最小熵产生原理和有序结构
短句来源
     The minimal value principle shows that the generalized energy at the final state of a force dissipation dynamic system reaches a minimal value.
     前者表明 ,强迫耗散动力系统的终态广义能量达极小值 ;
短句来源
  “强迫耗散”译为未确定词的双语例句
     At last, some theory analysis on wave quasi-resonance in forced and dissipative barotropic atmosphere is analysed in theoretics, which further proved the results of diagnosis and numerical experiments is understated.
     最后,对强迫耗散正压大气波动准共振进行了理论分析,进一步证实了本文的诊断分析和数值试验结果。
短句来源
     Envelope Solitary Rossby waves and Their Interactions Under the Influence of Forcing and Dissipation
     强迫耗散作用下的Rossby包络孤立波及其相互作用
短句来源
     Based on the complete dynamical equations of the moist atmospheric motion, the qualitative theory of nonlinear atmosphere with dissipation and external forcing and its applications are systematically discussed by new theories and methods on the infinite dimensional dynamical system.
     基于完整的湿大气动力学方程组,利用无穷维动力系统的新理论和新方法,系统讨论了强迫耗散的非线性大气系统的定性理论及其应用。
短句来源
     The barotropic vorticity equation is reduced to a KDV one containing the terms of forcing and dissipation, of which a stationary solution is obtained.
     本文将正压涡度方程约化为强迫耗散的KdV方程,求得了该方程的一个定常解.
短句来源
     LOCAL BLOCKING FLOW PATTERN IN A FORCED AND DISSIPATIVE NONLINEAR SYSTEM
     强迫耗散非线性系统的局域阻塞流型
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  forced dissipative
Computational stability of the forced dissipative nonlinear atmospheric equations
      
A new concept of computational quasi-stability (CQS) is introduced to study the computational stability (CS) of the forced dissipative nonlinear (FDN) evolution equations.
      
Construction of explicit quasi-Complete square conservative difference schemes of forced dissipative nonlinear evolution equatio
      
On the stability of forced dissipative nonlinear system
      
This paper, applying the stratification theory, proves the instability of certain initial (boundary) value problem of forced dissipative nonlinear system in atmospheric dynamics.
      
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  force dissipation
Next, we analyse in a similar way the motion of an electron in a dynamically disordered continuum where the effect of a classical friction force (dissipation) is taken into account.
      
This mode of failure is less common than the first two due to the efficient force dissipation that occurs through the insertional zone.
      


Using an eighth-order set of determinate, forced, dissipative, and nonlinear autonomous equations, which governs the dynamics of a quasi-geostrophic flow of the baroclinic atmosphere, the chaotic forms of large-scale atmospheric motion are investigated numerically. In certain ranges of the thermal forced parameters, the chaotic forms of the variations of the flow patterns are exhibited distinctly. Along with gradual change of the thermal forced parameter, transformations between periodic and chaotic motion forms...

Using an eighth-order set of determinate, forced, dissipative, and nonlinear autonomous equations, which governs the dynamics of a quasi-geostrophic flow of the baroclinic atmosphere, the chaotic forms of large-scale atmospheric motion are investigated numerically. In certain ranges of the thermal forced parameters, the chaotic forms of the variations of the flow patterns are exhibited distinctly. Along with gradual change of the thermal forced parameter, transformations between periodic and chaotic motion forms occur repeatedly. The windows of period-3 and period-6 emerge also in the chaotic regions.The periodic motion forms of the flow patterns corresponde to the periodic low-frequency vacillations of the subtropical high cells along the zonal direction during summer half year. After the transformation from periodic to chaotic form occurs, these regular vacillations are broken immediately. This phenomenon of the establishing and the breaking of the periodic low-frequency vacillation of the subtropical high cells along the zonal direction tallies with observational fact.

本文用一个确定的强迫耗散的八维非线性自治系统描述大尺度斜压大气的运动。在一定的热力强迫范围,流型演变显示出浑沌形态。随着热力强迫的渐变,发生了浑沌形态与周期形态之间的多次转换。在浑沌区内又清楚地显示出周期3和周期6的窗口。 流型演变的周期形态,相应于夏半年对流层上层副热带高压中心沿东西方向的周期的低频振荡。转为浑沌形态后,这种规则性的低频振荡即遭到破坏。这个副热带高压周期性东西振荡的建立与破坏的现象,与实际大气的观测事实十分相似。

By way of a low-order spectral model, the two-layzer quasi-geostrophicmodel is translated into an eighthorder set of nonlinear ordinary dif-ferential equations in which the thermal forcing and dissipative effectare incorporated. Within a certain range of the parameter θ_C~*, whichapproximately describes the S-N thermal forcing between the subtrop-ical continent and the ocean to the south, an equilibrium of the flowpattern is exhibited. When the θ_C~* value exceeds the critical point,a periodical zonal oscillation...

By way of a low-order spectral model, the two-layzer quasi-geostrophicmodel is translated into an eighthorder set of nonlinear ordinary dif-ferential equations in which the thermal forcing and dissipative effectare incorporated. Within a certain range of the parameter θ_C~*, whichapproximately describes the S-N thermal forcing between the subtrop-ical continent and the ocean to the south, an equilibrium of the flowpattern is exhibited. When the θ_C~* value exceeds the critical point,a periodical zonal oscillation of the subtropical high cells can bestimulated showing various oscillational forms.

本文用低谱途径,将二层准地转模式化为一个八维的强迫耗散的非线性系统。沿南北方向除赤道与极地之间的热力强迫外,模式还包含近似描述增温的副热带大陆与其南面海洋之间热力差异的强迫参数θ_c.在θ_c的一定范围内,模式大气显示出多平衡态特征,它们分别对应于对流层上层副热带高压的东部型和西部型流型。θ_c越过临界值后,模式大气又显示出多周期态特征,它们分别对应于对流层上层副热带高压的不同形式的东西振荡。

By the way of the low-order spectrual model, the two-layer quasige-ostrophic model is transformed into an eighth-order forced, dissipative, and nonlinear system. With the gradual changes of the thermal forced parameters, flow patterns of the baroclinic quasigeostrophic current which are represented by the variations of the distance functions, can change from periodic to aperiodic.The Liapunov's indexes corresponding to six different sets of the Poincare's cross-section charts are all positive value. That is...

By the way of the low-order spectrual model, the two-layer quasige-ostrophic model is transformed into an eighth-order forced, dissipative, and nonlinear system. With the gradual changes of the thermal forced parameters, flow patterns of the baroclinic quasigeostrophic current which are represented by the variations of the distance functions, can change from periodic to aperiodic.The Liapunov's indexes corresponding to six different sets of the Poincare's cross-section charts are all positive value. That is just the character of local aperiodic instability.

本文利用低谱途径,将二层准地转模式转化为八维的强迫耗散的非线性系统。随着非绝热强迫参数的渐变,以流场距离函数描述的斜压准地转气流的流型演变从周期态转为非周期态。与六组不同的Poincare截面图相应的指数均为正值,以示非周期的局部不稳定特征。

 
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