The correct option is that the Inter-Tropical Convergence Zone (ITCZ) seldom occurs in the South Atlantic and South-Eastern Pacific regions due to the unique oceanic and atmospheric dynamics in these areas. The ITCZ is crucial for cyclone formation as it facilitates the convergence of trade winds, leading to the development of organized convection and low-pressure systems. In contrast, the absence of a consistently active ITCZ in these regions results in a stable atmospheric condition that inhibits the necessary conditions for cyclone genesis, aligning with the principles covered in standard UPSC-level resources.