赤道缓冲带
- 网络equatorial buffer zone
赤道缓冲带-
进一步指出，在经圈平面上，ITCZ云区上空有上升运动，上升气流分别向北到达副热带下沉，向南到达赤道缓冲带下沉。
Furthermore , along the meridional plane there is an ascending motion over the cloud zones of ITCZ , which turns descending while reaching northwards the subtropical zone and southwards the equatorial buffer zone .
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1979年7、8月东亚地区赤道缓冲带的结构及其活动
The structure and activity of equatorial buffer zone over East Asia during July-August 1979
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在赤道附近存在一个异常的反气旋性环流，赤道缓冲带较强，有利于赤道高压的活跃，季风槽被推向较高纬度，从而有利于热带气旋的生成。
The equatorial buffer zone is fortified : it is propitious to the equatorial anticyclones activated and push monsoon trough to higher latitude , this circulation pattern can promote the genesis of TC in NWP .