The article delves into how different deployment strategies for Marine Cloud Brightening (MCB) can significantly alter the climate response, particularly in Earth's polar regions. MCB is a proposed geoengineering technique designed to combat global warming by spraying fine sea salt particles into marine stratocumulus clouds. This process increases the cloud droplet number concentration, making clouds brighter and more reflective, thereby sending more sunlight back into space and inducing a cooling effect. Research indicates that MCB holds potential for mitigating polar ice loss, contributing to the maintenance or restoration of Arctic and Antarctic sea ice, and potentially stabilizing critical ice sheets like the West Antarctic Ice Sheet. However, the effectiveness and specific outcomes are highly sensitive to the regions where MCB is deployed. While MCB offers a potential pathway to cool the planet, scientists are actively studying its broader environmental impacts. Potential side effects identified in various modeling studies include alterations in global precipitation patterns, with some models suggesting a weak global decrease but localized increases in certain low-latitude land areas. Furthermore, MCB simulations have shown a potential impact on the stratospheric ozone layer, with possible decreases in total column ozone in the Northern Hemisphere mid-latitudes but a surprising boost over Antarctica. The Earth and Space Science Open Archive (ESS Open Archive), where this article is sourced, is a legitimate community server for the rapid dissemination of early research outputs, including preprints. It is important to note that content on ESS Open Archive is not peer-reviewed, though it facilitates open scientific discovery. This highlights the ongoing, complex nature of climate intervention research.