Abstract
Even today, with the great progress that has been made in the scientific, technological and computational fields, we are still stunned by the devastating effects brought about by atmospheric phenomena. This paper aims to propose new hypotheses in the field of dynamics to enhance our understanding of the behaviour of atmospheric disturbances caused by rotating winds. I believe that the criteria of classical dynamics that are applied to vortex systems in the atmosphere should be rigorously reviewed. I propose to establish new hypotheses in the field of dynamics, in order to better interpret rotation in nature. These hypotheses have been structured into a new theory that has been tested experimentally by both ourselves and third parties, with positive results. I propose to use the Theory of Dynamic Interactions (TDI) to interpret the behaviour of systems undergoing successive rotations around different axes—which we will refer to as non-coaxial rotations. I hold that this theory applies to air masses and groups of particles in suspension that are accelerated by rotations. Accordingly, it should be used to interpret the behaviour of tornadoes, cyclones and hurricanes. I believe that this proposal could enhance our understanding of these atmospheric phenomena and improve predictions about them.
Highlights
The devastating effects of atmospheric vortex phenomena have been the subject of a great deal of research; our understanding of them is still, imperfect.Every year, the catastrophic consequences of tornadoes, typhoons and cyclones cause loss of life and substantial economic losses
All we have is air rotating in accordance with the Coriolis effect, and the paths we observe are caused by dynamic interactions. Against this background of study and constant progress in unravelling the physical behaviour of nature, we suggest that the criteria of dynamics that have been applied to date in atmospheric science should be reviewed, given that we believe that the principles of classical rotational dynamics may well be inappropriately interpreted
In the light of the above, and in accordance with the Theory of Dynamic Interactions (TDI), we suggest that the arms or spiral cloudrain bands (SCRB) of these atmospheric phenomena are accelerating masses of air subject to dynamic interactions
Summary
The devastating effects of atmospheric vortex phenomena have been the subject of a great deal of research; our understanding of them is still, imperfect. Barceló form a spiral or around an axis, with changing paths In structural terms, these are enormous vertical thermal machines maintained by the combination of atmospheric mechanics and the Earth’s gravity, which generate rotating cloud, wind and/or storm systems. Perhaps we do not fully understand these phenomena because there is something missing in our knowledge of the underlying science and of the factors that affect how they are created and how they change over time Predicting their intensity continues to be one of the goals of atmospheric physics, given that the disaster warning and prevention systems for inhabited areas act on the basis of this information. Against this background of study and constant progress in unravelling the physical behaviour of nature, we suggest that the criteria of dynamics that have been applied to date in atmospheric science should be reviewed, given that we believe that the principles of classical rotational dynamics may well be inappropriately interpreted
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