Synoptic and Local Controls on Summer Cooling Explain Diverging Glacier Mass Balance Across High Mountain Asia
This study resolves the Karakoram Anomaly by demonstrating that diverging glacier mass balances across High Mountain Asia are driven by a multi-scale atmospheric coupling where synoptic teleconnections and local katabatic wind feedbacks induce summer cooling in western regions, which, when combined with precipitation regimes, explains 78% of the observed mass balance variance.