Recent scientific investigations underscore the profound influence of stratocumulus clouds on Earth's climate system, particularly their role in regulating global temperatures. These low-lying clouds, which cover significant oceanic areas, are crucial for reflecting solar radiation back into space, thereby exerting a cooling effect on the planet. However, current global climate models frequently under-represent the strong positive radiative feedback associated with stratocumulus clouds, leading to considerable uncertainties in future climate projections. This under-representation is a major concern as it can significantly affect predictions of warming patterns, equilibrium climate sensitivity, and the dynamics of tropical atmospheric circulation under increasing carbon dioxide concentrations. Studies emphasize that accurately integrating stratocumulus cloud schemes into climate models is paramount for enhancing the reliability of these projections. The choice of stratiform cloud scheme can contribute substantially to the inter-model spread in cloud radiative responses, influencing the magnitude and even the sign of feedback in stratocumulus regions. Furthermore, there is growing concern that unchecked increases in atmospheric CO2 levels could trigger the collapse of stratocumulus cloud decks, potentially leading to an abrupt and severe acceleration of global warming. Such a collapse could result in additional degrees of warming, pushing the Earth towards conditions not seen in millions of years. The MIROC (Model for Interdisciplinary Research On Climate) family, developed in Japan, is a recognized series of global climate models used in such research. The ongoing research highlights the urgent need for refining cloud parameterizations to capture these critical atmospheric processes more accurately, ensuring better predictions of global climate change impacts, which are highly relevant for countries like India facing significant climate vulnerabilities.