BODY FORCES AND FLUID STABILITY: A THEORETICAL FRAMEWORK FOR ENERGY TRANSFORMATION AND STRATIFIED ATMOSPHERES

Abstract

This paper investigates the role of body forces-such as gravity, electromagnetism, and inertia-in influencing the kinetic energy and stability of fluid systems. It develops a theoretical framework for quantifying energy transformations and resistance mechanisms arising from these forces in a fluid. The analysis introduces a model describing how internal, thermal, and potential energies are converted into kinetic energy under body forces, accounting for losses through decay or dispersion. The study extends to the Navier-Stokes equation, incorporating density-dependent body force terms with quantum-like characteristics. It explores conditions under which body forces enhance stability, particularly in stratified atmospheric layers. A notable phenomenon discussed is the formation of a theoretical substance formed under extreme thermal conditions in the atmosphere, termed “Angamaton”, hypothesized to occur in a highly stratified region between 15⁰ and 30⁰ latitude (desert regions of the world). This substance is suggested to enhance atmospheric smoothness and resistance to turbulence. The findings have potential applications in fluid dynamics, atmospheric modeling, and aerospace route optimization, and they open new avenues for research on quantum-fluid interactions and stratified flow behaviour.