Large‐Scale Seasonal Changes in Glacier Thickness Across High Mountain Asia

Recently, increased efforts have been made to estimate the mass budgets of glaciers in High Mountain Asia (HMA). However, seasonal changes in glaciers are poorly understood, despite the fact that seasonal meltwater released from glaciers is a crucial local water resource in HMA. Utilizing satellite altimetry and gravimetry data, we constructed annual changes in glacier elevation and identified two general patterns of the seasonality of glacier elevation changes. Glaciers in the periphery of HMA (except for those in the eastern Himalayas) thicken from approximately December to April–June, thus exhibiting winter and spring accumulation. Glaciers in the inner Tibetan Plateau, especially those in Western Kunlun and Tanggula, accumulate from approximately March to approximately August, thus exhibiting spring and summer accumulation. The amounts of seasonal glacier ablation were obtained using a new approach of direct observations of glacier changes, rather than inferring changes using a climate model. Key Points We construct continuous annual changes in glacier elevation across the High Mountain Asia by direct satellite observations of glaciers We identify two general patterns of the seasonality of glacier elevations: winter‐spring accumulation and spring‐summer accumulation We roughly estimate the contributions from seasonal glacier ablation to the cryosphere and downstream hydrology