位势不稳定 meaning in Chinese
potential instability
Examples
- There were wind shear and maximum wind speed occurred above or below the height of potential instability area and one of them happened before potential instability
位势不稳定区所在高度的上方和下方会有风向切变和风速极大值中心，并且风切变或急流中心会早于位势不稳定的出现。 - Potential instability existed near 0 in the warm area and between - 10 and 0 in the cold area . the occurrence of potential instability was corresponding with maximum rainfall and maximum vapor content
C附近，冷区位势不稳定分布在一10一ooc ，位势不稳定出现的时间与地面强降水、水汽最大累积区出现的时间一致。 - Potential instability that exists with conditional symmetrical stability make the vertical ascend movement in e big value area and slope ascend movement in e surface ( meiyu front area ) produce and maintain
位势不稳定和条件性对称不稳定共存使得在_ e高值区域的垂直上升运动和在_ e面(梅雨锋区)上的斜上升运动得以产生和维持。 - Embedded in a large - scale cold front - cyclone are often meso - and small - scale wet thermal / dynamic structures that are uneven , with a huge cold " cushion " at low levels , frequent meso cold surges and related potentially unstable zones at middle levels
在大尺度冷锋气旋天气系统中，嵌有不均匀的中小尺度湿热力动力结构。表现为低层大尺度冷垫、中空不断出现的中尺度“冷涌”及对应的位势不稳定区。 - It is the important mechanism that middle - level dry and cold air current sunk , low - level warm and wet air current ascended . level direction energy sharp section is important to blaze middle scale hypo - circumfluence . severe convection weather was brought by layer - knot latent instability
上层干冷、下层暖湿的位势不稳定层结可以使对流层中低层出现明显的逆温层，有利于不稳定能量积累，此次天气过程产生的对流不稳定能量大，形成的上升气流深厚。