| 1. | Climb straight up two ( 2 ) meters , hold for five ( 5 ) seconds
垂直上升2公尺，保持静止停悬5秒钟。 |
| 2. | Study on flow pattern identification for air - water two - phase flow in a vertical tube
垂直上升管内气液两相流流型鉴别研究 |
| 3. | Local flow regime transition criteria of gas - liquid two - phase flow in vertical upward tube with a horizontal rod
垂直上升管内有水平柱体时气液两相局部流型转变的研究 |
| 4. | After the take - off , coming to a complete stop with little to no vertical bounce , dip , lateral drifting or wobble
起飞后机体保持完全静止不动，不可有任意的垂直上升或下降，机体不可左右摇晃或漂移。 |
| 5. | Come to a complete stop without any vertical bounce or dip , and little to no lateral wobble or drifting
直升机停止上升后，机体需保持完全静止不动，不可有任何的垂直上升或下降，机体不可左右摇晃或漂移。 |
| 6. | 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。 |
| 7. | Low - level cyclones usually imply horizontally confluent flow and vertically rising air resulting in inclement weather . low - level anti - cyclones bring in fine and stable weather due to horizontally diffluent flow and vertically sinking air
低空气旋表徵水平汇聚、垂直上升的不稳定气流，可以导致恶劣天气产生；低空反气旋则代表水平辐散、垂直下沉的稳定流场，伴随著晴朗的天气。 |
| 8. | The vertical velocity in low troposphere is larger than high troposphere , and vertical velocity in flood year is also larger than that in drought year . the vertical velocity on different levels show that there exists distinct sinking motion from midlevel to uplevel of troposphere in drought years and updraft in whole atmosphere in flood years
垂直分布曲线均呈s形，垂直上升速度在对流层低层大于对流层上层，多雨年大于干旱年;不同层次上垂直速度分布图表明，旱年对流层中上层盛行下沉气流，而涝年整层大气始终表现为上升运动。 |
| 9. | Based on the analysis mentioned above , a conceptual diagram explaining the physical process is put forward : stronger ( weaker ) convective activities in tropical areas stronger upward ( downward ) vertical anomaly stream in tropical areas more ( less ) moisture transports from " key regions " to shandong stronger ( weaker ) hadley and walker circulation stronger ( weaker ) east asian summer monsoon eap ( negative eap ) in 500hpa upward ( downward ) vertical anomaly stream rise in shandong subtropical high abnormally located northward ( southward ) more ( less ) rain in shandong province
弱季风年与山东夏旱年则相反。通过分析山东夏季降水与东亚夏季风以及大气环流异常的物理过程，得出了如下物理概念模型:热带印度洋以及南海-热带西太平洋地区对流加强(减弱)吟热带地区垂直上升(下沉)气流增强峥热带印度洋和南海一西太平洋地区水汽输送通量增加。 |
| 10. | The simulation results reveal that water vapor transportation northward is responsible for the generation of the convective instability in south shandong , and the easterly wind from sea , gravity wave and convergence generated by southward invasion of weak cold air in pbl play main role in trigger , transmission and enhancement of convective systems
定性地给出了中尺度对流系统气流运动的图像，即：在边界层，气流从东南方向斜升流入中对流区，在系统中垂直上升，约在7000米一9000米高空向东北方向流出，形成非闭合的垂直环流。 |
