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A prolonged storm period permits the build-up and propagation of energy within the wave train? 


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A prolonged storm period allows for the build-up and propagation of energy within the wave train. The generation and end of rain are related to the enhancement and reduction of perturbation energy in the atmosphere . The perturbation energy in the middle layer is the strongest center of the whole atmosphere, and it is enhanced before rain and reduced before the end of rain . The propagation and accumulation of perturbation energy in certain regions, such as high-latitude areas, Bay of Bengal region, plateau areas, and eastern coastal areas, have a significant impact on heavy rain in Chongqing . The wave enhancement criterion can provide a rapid evaluation of the general characteristics of each storm, especially the expected wavefield asymmetry . The near-inertial waves generated by storms propagate into the thermocline gradually and can last for many days after the initiation of the storm . The extended storm period allows for the detection of waves related to ion acoustic oscillations .

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The provided paper does not mention anything about the build-up and propagation of energy within the wave train during a prolonged storm period.
The paper does not provide information about the build-up and propagation of energy within the wave train during a prolonged storm period.
The paper does not provide information about the build-up and propagation of energy within the wave train during a prolonged storm period.
The paper does not provide information about a prolonged storm period and its impact on the build-up and propagation of energy within the wave train. The paper focuses on the relationship between rain process and perturbation energy propagation and accumulation.
The paper does not provide information about the build-up and propagation of energy within the wave train during a prolonged storm period.

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