<p>The Global Warming Potential-star (GWP*) approach is a way to convert the emissions of short-lived climate forcers to CO₂-equivalent emissions while maintaining consistency with temperature outcomes. Here we evaluate the performance of GWP* when it is used to account for non-CO₂ gases within the carbon budget framework. We convert methane (CH₄) emissions to CO₂-equivalent emissions via GWP* and calculate the temperature through simple climate models. We show that GWP* can accurately convert CH₄ emissions to reproduce the temperature until 2100 under a variety of scenarios, including overshoot scenarios, except those with a rapid decline in CH₄ emissions. Beyond 2100, however, the use of GWP* can lead to temperature overestimation since it extends beyond its calibration range. Furthermore, we find that under scenarios designed to achieve identical temperature targets but with varying overshoot profiles, cumulative CO₂-eq budgets (GWP*-basis) generally increase with overshoot length and magnitude. This is driven by the internal dynamics of our model, as characterized by its negative zero-emission commitment. While the use of GWP* enhances such effects with increasing overshoot length, it exerts opposite effects with increasing overshoot magnitude.</p>