A low - level jet is a narrow band of strong winds in the lower atmosphere 低空急流是在大气低层出现的狭窄强风带。
A low - level jet is a narrow band of strong winds in the lower atmosphere 低空急流是在大气低层出现的狭窄强风带。
Scientists tried to seek explanations from the dv of low - level jet as a member of the meiyu precipitating system 过去曾从低空急流日变化等一些梅雨系统的内部联系寻求解释。
The low - level jet stream has three vibration processes , which corresponded to the three lows " beginning and developing 低空急流有三次脉动过程,与三个低涡的产生和发展对应。
The low - level jet stream is the result of the spread of the momentum from the upper - level jet stream 低空急流是高空急流的动量向下输送的结果。低空急流的生成先于水汽及降水的爆发。
The positive storm - relative helicity center is accompany with low - level jet in 850 - hpa isobaric surface fields 通过分析我们发现了正的相对螺旋度中心与850hpa低空急流的演变过程是一致的。
Severe convergence brought by low - level jet pulsation , and severe divergence brought by upper - level jet is directly trigger mechanism of this intense rainstorm 低层低空急流脉动产生的强辐合,高空急流诱发的高层强辐散是本次东北地区暴雨天气的直接触发机制。
The results show that the event is directly affected by the formation and evolution of southwest vortex and mcc cloud cluster which locate in the intersection region of the upper - level jet and the low - level jet 结果表明:高、低空急流耦合区中西南低涡及mcc特徵云团的形成和维持是造成此次特大暴雨的直接影响系统。