Bill,
I'm going to agree with Danny's suggestion that she was given an out-of-context theoretical explanation based on boundary layer physics, or perhaps misunderstood the explanation and took it out of context herself. The "1 inch" figure probably refers to what is known as the "roughness length", which is basically the height above ground level where air "always" remains still due to the effects of friction.
As one might imagine, the roughness length varies significantly based on the type of vegetation/structures present on the ground. For example, in a grassland it might be around 1 cm, and in a dense forest it might be around 1 m. Keep in mind, though, that the roughness length approximation is only valid in an idealized boundary layer physics framework, which usually assumes a constant vegetation/structure height and distribution, but nevertheless works pretty well for many common atmospheric and land-use situations.
Obviously, a tornado is hardly a "common atmospheric situation". Among other things, a tornado will tear down structures and vegetation, reducing the height of obstructions and sometimes even leaving bare ground. So what is the roughness length of smooth, featureless bare ground? If I'm remembering my boundary layer physics correctly, it's something in the ballpark of 1/10 the height of a grain of sand.