Here is a gif of a tubular cloud formation along the Lake Michigan shoreline at Sleeping Bear Dunes National Lakeshore, in June (2017).
This phenomenon is a type of arcus cloud and is commonly (and regrettably) referred to as “The Morning Glory” cloud.
Despite being studied extensively, this cloud formation is not yet fully understood. However, it is determined that the main cause is probably due to mesoscale circulations.
In the front of the cloud, there is strong vertical motion that transports air up through the cloud and creates the rolling appearance, while the air in the middle and rear of the cloud becomes turbulent and sinks.
The formations can be up to 1000 kilometres long, 1 to 2 kilometres high, and can move at speeds up to 60 kilometres per hour. It is often accompanied by sudden wind gusts, intense low-level wind shear, a rapid increase in the vertical displacement of air parcels, and a sharp pressure jump at the surface, making these clouds problematic to air traffic.