Overview
- A peer-reviewed study published Aug. 1 integrates NASA GRACE satellite data with hydrological and meteorological records to link glacier mass change to monsoon seasonality.
- Central and western Himalaya losses are tied to increased rainfall during typically snow-accumulating summer periods, while eastern Himalaya losses reflect reduced snowfall.
- Retreat shows repeating 3–4.5 and 5–8 year cycles that align with natural monsoon variability, pointing to predictable swings in melt rates.
- Researchers warn river systems will transition from melt-driven to rainfall-driven flow, heightening drought risk for downstream communities in South and Central Asia.
- Accelerated melt increases the likelihood of glacial lake outburst floods and cascading hazards such as landslides and river flooding, prompting calls for denser climate and cryosphere monitoring.