Ms Fedaeff said the concept of instability apllied to all fluids including the atmosphere, “which is a fluid”.
“ When the air at the top of the cloud is moving faster than at the bottom of the cloud and pushes the cloud tops, it creates a wave shape,” she said.
Such a formation could be seen on windy days or when there were differences in air densities — such as near sunrise/sunset when the bottom of the clouds are cooler and air above is warmer.
Ms Fedaeff says while NIWA did not have an official way to keep a track of the occurence, the phenomenon tends to be short lived -with the wave shape breaking down rapidly.
“I would consider them to be uncommon and have only personally seen them twice in my life,” she says.