While turbulence is commonly regarded as a flow feature pertaining to the planetary boundary layer (PBL). intense turbulent mixing generated by cloud processes also exists above the PBL in the eyewall and rainbands of a tropical cyclone (TC). The in-cloud turbulence above the PBL is intimately involved in the development of convective elements in the eyewall and rainbands and consists... https://herbsdailyes.shop/product-category/bath-mats/
Role of eyewall and rainband eddy forcing in tropical cyclone intensification
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