Source: A Guide to F-Scale Damage Assessment
I. The Fujita scale of tornado intensity (condensed)
A. A short history
Prior to the adoption of T. Theodore Fujita’s (1971) tornado intensity rating scale by the National Weather Service (NWS), there was no formal way to attempt to differentiate one tornado from another. With the interest and support of Allen Pearson, then Director of the National Severe Storms Forecast Center, the Fujita scale became the standard for estimating the intensity of tornadoes in the mid-1970s.
In addition, Fujita used a set of damage photographs to illustrate the intensity categories. With the introduction of these materials, it became possible for someone surveying the damage from a tornado to estimate the F-scale (implying an estimate of the range of windspeeds).
Further, using newspaper accounts and photographs, it became possible to assign an F-scale to historical events, a project which was undertaken by the National Severe Storms Forecast Center (NSSFC), with the support of the Nuclear Regulatory Agency in 1976.
Students were hired to do the necessary research into old newspapers and other accounts of storms. They assigned an F-scale rating to as many historical events as possible based mostly on newspaper accounts and photographs.
In 1973, the official authority for doing Storm Data passed from the state climatologists to the NWS offices. From the late 1970s to the present, it has been expected that all tornadoes that become part of the Storm Data record will have an Fscale number assigned to them, as well as estimates of the path length and width. In actual practice, the rating of tornado intensity is necessarily done by assessing the damage, rather than by windspeed estimates