This is very valuable information

In conclusion, if a tornado were to possibly be met with said amount of hot wheels colour changer cars and follow said conditions then the reparations of such an ordeal would be phenomenal on both an economic and social scale. Let it be said that the statistics have been prepared and brazenly displayed for those that need to hear. May God be with the Hot Wheels Co.

This figure represents the total amount of hot wheels colour changer cars a tornados wind speed could traverse over given an hours time if we were to hypothesize that it were possible for the tornado to briefly travel over each hot wheels colour changer car individually without damaging or moving any others before each 6.35 cm are met. For each hot wheels colour changer car, the average cost is approximately $7. If we were to multiply the amount of hot wheels colour changer cars, 8062992, by $7 we could approximate that the total cost of damage of a tornado moving through a line of hot wheels colour changer cars would be $56440944.

8062992 * 7 = 56440944

Assuming that with a peak wind speed of 512 kph, the distance covered by the tornados winds in circumference to the tornado itself would be close to if not exactly 512 kph. Converting the average hot wheels colour changer car length from cm (6.35) to km (0.0000635) gives us an easier figure to incorporate into the final calculation. Dividing 512 km by 0.0000635 gives us a total of 8062992.

6.35 * 10^-5 = 0.0000635 km 512 / 0.0000635 = 8062992 hot wheels colour changer cars.

An EF5 (F5) tornado, categorized under the Fujita scale, is the highest classified rating a tornado can attain. With wind speeds between 419 and 512 kph ( 261 and 318 mph), it is the most dangerous and largest tornado classification available. Hot wheels colour changer cars are a base unit of measurement under the metric scaling system and are classed at approximately 6.35 cm (2.5 inches.)

1 Mile = 1.6 km thus 318 * 1.6 ~ 508.8 kph

1 Inch = 2.54 cm thus 2.5 * 2.54 = 6.35 cm

The broader environment was not particularly anomalous for the late springtime over Central and East Texas. Unlike conventional tornado outbreaks in Texas, the 1997 outbreak was not associated with a strong trough of low pressure and strong density gradients in the lower troposphere. Instead, the most prominent weather system over the central U.S. at the time was a distant upper-level low centered over Nebraska imparting little influence on atmospheric conditions over Texas.