Current scientific projections based on climate models suggest that the complete melting of the Antarctic ice sheet could take several centuries to thousands of years if greenhouse gas emissions continue at high levels. However, it is important to note that these projections are subject to uncertainties, and the actual timeline may vary depending on the future trajectory of global emissions and climate policies.
Ongoing scientific research and monitoring are essential for improving our understanding of the dynamic processes that influence the stability of the Antarctic ice sheet and its response to climate change. This knowledge helps inform adaptation strategies and international efforts to mitigate global warming to reduce the potential impacts on Antarctica and other vulnerable regions of the planet.