Our research explores how Northern Hemisphere near-surface wind speeds respond to the removal of CO₂ from the atmosphere. Using advanced CESM (Community Earth System Model) simulations, we discovered that wind speeds react differently during periods of increased and decreased carbon dioxide levels. Different responses are attributed to changes in global surface temperature and AMOC (Atlantic Meridional Overturning Circulation). This study not only advances our understanding of climate dynamics but also aids in optimizing strategies for wind energy.