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Impact of typhoon-generated gravity waves in the typhoon development

机译:台风产生的重力波对台风发展的影响

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摘要

As a first attempt to understand the impact of typhoon-generated gravity waves (TGWs) on typhoon development, Typhoon Saomai (2006) is simulated and effects of TGWs on background flows are examined by considering momentum flux. The momentum flux of TGWs and its vertical divergence/convergence are larger during the developing stage than during the mature and decaying stages of the typhoon. In the developing and mature (decaying) stages of the typhoon, TGWs act to decrease (increase) vertical wind shear, which is known to inhibit a typhoon's intensification. Thus, TGWs can help a typhoon intensify when the typhoon develops. Upper-level divergence increases notably before a typhoon enters both rapidly-developing and mature stages. A significant portion of upper-level divergence is found to be due to TGWs.
机译:为了了解台风产生的重力波(TGWs)对台风发展的影响,首次模拟了台风Saomai(2006),并通过考虑动量通量研究了TGW对背景气流的影响。与台风的成熟期和衰落期相比,TGWs的动量通量及其垂直发散/会聚在发育阶段要大。在台风的发展和成熟(衰减)阶段,TGW的作用是减少(增加)垂直风切变,已知这会抑制台风的增强。因此,当台风发展时,TGW可以帮助增强台风。在台风进入快速发展和成熟阶段之前,高层差异明显增加。发现高层差异的很大一部分归因于TGW。

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