LLJ:低空急流
低空急流(Low Level Jet stream,常缩写为LLJ)是气象学领域的专业术语,指对流层中下层出现的强风带。这一简称在科研文献和日常气象分析中被广泛使用,便于快速记录和交流,有助于提升专业场景下的沟通效率。
Low Level Jet stream具体释义
Low Level Jet stream的英文发音
例句
- The conver gence stream field of the upper level jet stream and low level jet stream play an important part in the emergence and development of the MCC.
- 高、低空急流(LLJ)和低层辐合流场对MCC的生成和发展具有重要的作用。
- The features of low level jet stream during a continuous high wind and Hail Event over the South Yunnan
- 云南一次持续性风雹过程中低空急流(LLJ)的若干特征
- Moisture transfer and rainstorms around the large scale low level jet stream a new positive definite advection scheme and the application of it to the moisture equation
- 大尺度低空急流(LLJ)附近的水汽输送与暴雨一种新的正定平流方案及其在水汽预报方程中的应用
- Low level jet stream is strong in 700 hPa aerological diagram, and there is vapor transporting channel, too.
- 700hPa图上有明显强劲的低空急流(LLJ),有水汽输送带。
- Energetic analysis of the southwesterly low - level jet stream
- 西南低空急流(LLJ)的能量学分析
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