Lake effect snow squalls need a few factors to get them going - cold winds that are fairly well lined up with each other with height, but stronger as you go upward (wind shear), blowing over a sufficient amount of open water that's about a 13 degree C warmer than the air 1500 metres above it. That gives enough evaporation from the lake's surface to produce the instability for clouds to form and eventually produce precipitation that will freeze into snowflakes in the cold air. At the same time, it provides the right push from the winds to keep the clouds rolling along over more open lake surface to gather more moisture and keep them moving along after they reach land (and thus lose their connection to the moisture supply). The last piece of the puzzle falls into place when the 'fetch' - the amount of open lake water the winds have to blow over before they reach land again - is at least 100 kilometres long. As well, Buffalo is between two great lakes.
Now that they know exactly what causes it they need to figure out how to ameliorate it. That has to be a lot easier than landing a spacecraft on an asteroid.
Now that they know exactly what causes it they need to figure out how to ameliorate it. That has to be a lot easier than landing a spacecraft on an asteroid.

