inertial instability meaning in Chinese
惯性不稳定性
惯性不稳度
Examples
- The mcc develops mechanism is analyzed based on moist thermal wind theory , relatively mesoscale convectively generated vortex , potential vorticity thinking , inertial instability theory and so on
用湿热成风、相对中层涡旋、等熵位涡、惯性稳定度等讨论了mcc的发生发展机理。 - Inertial instability barotropic advection of potential vorticity the subsidence of the large value of potential vorticity above cyclone and geostrophic adjustment process is dynamical factors which make the cyclone developed violently
惯性不稳定，正压位涡平流以及正压位涡大值下沉至气旋上空和地转适应过程是气旋强烈发展的动力因子。 - Wet and dry numerical simulation tests for explosive cyclone over western pacific were performed . by contrast the results show that : tropopause and constant temperature surface were raised by latent heat release in upper level and disturbance trough was produced because air flow ascended and became cold . owing to this process adaption , inertial instability emergenced
对气旋强烈爆发的过程进行干湿对比数值模拟试验，得出：潜热释放使对流层项和等温面抬高，气流在高层的上升冷却形成扰动槽，其适应过程使高层出现惯性不稳定。 - Inertial instability always existed in strong inertial stability area , furthermore , acceleration field caused these two factors can give rise to air convergence and divergence in upper level , which made cyclone strengthened and precipitation enlarged . reinforced precipitation caused latent heat enlarged again , which led to inertial instability augmented
惯性不稳定总是伴随强惯性稳定区存在，这两者产生的加速度场可形成高层的辐合、辐散引起气旋加强以及降水加大，降水加强又可使潜热进一步加大和扰动槽加强，从而导致惯性不稳定加剧。 - The analyses suggest that the first and second categories of rainstorms are associated commonly with the strong inertial instability in the upper troposphere , as well as respectively with symmetry and convective instabilities , and their rainfall is large ; and the third and fourth categories generally produce stable precipitation with a small rainfall , and their upper tropospheres are usually inertially stable
分析湿位涡与梅雨暴雨中的惯性不稳定、对称不稳定、对流不稳定的关系发现：第1类暴雨往往与对称不稳定有关，第2类暴雨与对流不稳定有关，且这两类暴雨高层多具有强惯性不稳定，降水相对较大；第3 、第4类暴雨是稳定性降雨，高层一般不具备惯性不稳定，雨量一般较小。