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://leoners.shop/product-category/upright-freezer/