The 1957 Dallas Tornado might easily be dismissed as just one out of scores of common Texas twisters, each in its time having done some damage and, perhaps, killed a few unfortunate people. The Dallas tornado was no monster to rival, for instance, the F4 that ravaged Wichita Falls in 1979. Retrospectively it has been determined to have been a category F3 (the original Fujita-Pearson scale was not developed until 1971). As it carved a sixteen mile path through Oak Cliff and West Dallas over a time span of about forty minutes, it took the lives of ten people, including three children from a single family (the highest death toll from a tornado to date in the DFW area), injured approximately 200 and left 500 homeless. Five-hundred seventy-four structures were damaged, including between 131 and 154 homes and between 9 and 28 apartment buildings that were completely destroyed. Property losses totaled $4 million (in 1957 dollars). It was one of about twenty-five tornadoes spotted around north central Texas and southern Oklahoma that day.
However, the Dallas tornado historically is quite significant. By the time of its first appearance the rains that preceded it mostly had passed on, so that the air was washed clean and the funnel was not particularly obscured by precipitation. Rainfall from the thunderstorm that gave it life also was generally sparse. Although sky conditions were overcast and threatening, there were no especially low clouds to impede viewing. The tornado did not strike in a sparsely populated rural location, but rather in the middle of a relatively large metropolitan area. It did not strike at night, but late on a Tuesday afternoon when many people were out and about to witness it. It did not come and go quickly, but was deliberate — almost leisurely — in its passage. All of these circumstances conspired to make it by far the most filmed and photographed tornado up to its time.
Photographs were made by 125 persons, and film footage ran to 2000 feet. Much of the latter was of sufficient quality (some of it exceeded only in the past few years as storm chasing and video recording of tornadoes have become common) to allow meteorologists to carefully plot debris movement, and thus, for the first time, obtain reliable estimates of the very high wind velocities associated with severe tornadoes. Also, although most of the damage was to houses, because the tornado struck in a built-up area engineers were able to make the first systematic measurements of the effects of those winds on a number of different types of construction, information that contributed to the later development of the Fujita-Pearson scale.
The 1957 Dallas tornado marked the first major quantitative success for modern scientific research into one of nature’s most incredible phenomena, research that has saved an untold number of lives and that continues today with highly mobile Doppler radar and other sophisticated weather instrumentation which can be moved quickly to sites of severe storms.