
I was under the impression (my own thoughts) that these clouds usually preceded a front and the clouds were actually "distorted" by very strong winds at that level. Usually the weather arriving after these clouds will be very warm strong westerly winds with a southern change later. (Well what Dunedin person doesn't know that if we have a warm windy day, it will probably rain the next

Most definitions of Mammatus state that these clouds often form under the anvil of weakening thunderstorms, though I couldn't agree that there were thunderstorm clouds overhead in Dunedin today.
Is this true? Or is it just the cooler air above sinking into the warmer air below without any high winds?