... advection effect: 平流效应 horizontal advection: 水平平流 vorticity advection: 涡度平流 ...
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The divergence in the troposphere upper layer and the positive vorticity advection are the main dynamic factors that control the development of the tropical cyclones after it lands.
在北上中，由于中纬度弱冷空气的加入，造成或加剧斜压不稳定，斜压位能转换为动能，是引起热带气旋变性发展的原因。 对流层高层辐散及正涡度平流是气旋发展的主要动力因子。
参考来源 - 渤海大风统计特征及物理机制分析·2,447,543篇论文数据，部分数据来源于NoteExpress
涡度平衡中主要是水平平流累积的正涡度与散度项制造的负涡度相平衡。
Positive vorticity accumulated by horizontal advection was balanced with negative vorticity made by divergence term in vorticity balance.
与副热带锋区上急流相关的平流非线性作用在水热收支与涡度平衡中占优势。
Nonline advection which is connected with jet of subtropical frontal zone occupies a main place in heat and moisture budgets and vorticity balance.
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