伴随登陆热带气旋生成的低空东南急流为暴雨输送了丰富的热量和水汽，成为联系中低纬度系统的纽带。
The low-level southeast jet accompanying the tropical cyclone transports a plenty of heat and moisture for the event.
热带气旋往往沿着赤道，在热带温暖的水域生成，然后向南北移动到亚热带地区。
Tropical cyclones tend to form along the Equator, over the warm waters of the tropics, then move northward or southward into the subtropics.
但是我们担心新的低气压又在内部或外部生成，每年的这个季节，在我们所在的海面上应该由反气旋的天气系统所控制。
But we fear that another depression may be growing within, or between, the great bulk of the anti-cyclone that should be dominating our patch of sea at this time of year.
结果表明，采用不同模式的初始资料生成得到初值集合成员的方法用于集合预报，对南海热带气旋路径预报有一些明显的改进。
The results show that some obvious improvements can be obtained for the track forecasting by using ensemble members formed by the data of initial fields of the 3 different numerical models.
结果显示，西南热低压生成时水平流场表现为明显的气旋性辐合流场，低压环流中心轴线随高度的变化基本上是垂直的；
The central axis of heat low is vertical with the change of height. The heat low develop in local place.
结果显示，西南热低压生成时水平流场表现为明显的气旋性辐合流场，低压环流中心轴线随高度的变化基本上是垂直的；
The central axis of heat low is vertical with the change of height. The heat low develop in local place.
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