The new theory on why tornadoes occur suggests that it is a result of the interaction between warm, moist air from the Gulf of Mexico and cold, dry air from the Rockies. This creates a powerful wind shear that can lead to the formation of tornadoes.
This theory differs from previous theories in that it focuses on the specific conditions that lead to tornado formation, rather than just the general atmospheric conditions. It also takes into account the role of different air masses in creating the necessary wind shear.
There is strong evidence to support this new theory, including observations of the specific air mass interactions that occur before tornadoes form, as well as computer simulations and data analysis. This evidence has been reviewed and validated by multiple scientists in the field.
This new theory has the potential to greatly improve tornado prediction and forecasting. By understanding the specific conditions that lead to tornado formation, meteorologists can better identify and track potential tornadoes, giving people more time to prepare and seek shelter.
As with any new theory, there may be some criticisms or limitations that arise as more research is conducted. Some scientists may argue that this theory is too narrow and does not account for all tornado occurrences. Others may question the validity of the evidence or the accuracy of the computer simulations used to support the theory. Further research and analysis will be needed to address these potential criticisms.