1) mesospheric and lower thermospheric wind field
中间层/低热层风场
2) Mesosphere and Lower Thermosphere(MLT)
中间层和低热层
3) Mesosphere and lower thermosphere
中间层-低热层
4) low wind
低层风场
1.
Nino3 SSTA in the previous winter affects Guangzhou spring rainfall through North Pacific subtropical high and low wind in spring.
前冬Ni?o3区海温异常对广州春季降水的影响是通过影响春季北太平洋副热带高压和低层风场异常实现的。
5) disturbance of low-wind field
低层风场扰动
6) low level strong wind
低层大风
1.
Based on the improved definition of the low level jets(LLJs) in China,the southwesterly low level strong winds are divided into low level jets that have vertical axes in low level and low level strong winds(LLSWs) that have no wind axes, and the differences of the climatic and synoptic characteristics between them are discussed.
通过从垂直切变角度对中国低空急流的定义,表明西南低层大风现象有两类:有垂直轴的低空急流和无垂直轴的西南低层大风(简称低层大风),并揭示了二者的气候学和天气学特征差异。
2.
The low level south-westerly strong wind (LLSW) includes the low level jet (LLJ) that has the independent axis and the no-axis low level strong wind (NALLSW).
西南低层大风现象，基本可以分为两类，一类具有独立的低层大风核结构，另一类则不具有独立的大风核结构。
补充资料：中间层
从平流层顶至约85千米高度的大气层。层内温度随高度的增加而迅速递减。大气虽极其稀薄，但有相当强烈的铅直对流。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条