The air within the warm sector is generally stable (Tropical Maritime). Nevertheless, it could become unstable during summer - where possible Air mass Thunderstorms may form.
Air mass thunderstorms are isolated thunderstorms produced by local convection within a conditionally unstable air mass. Often form in the afternoon when there is maximum heating at the surface. Rarely reach severe criteria.
- The lifting mechanism for these thunderstorms is not a frontal boundary but rising thermals off the hot surface.
- Usually found in the warm sector and in the tropics.
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