“…Recent efforts have led to the combined modelling of glacier mass balance, seasonal snow conditions on glaciers and land, as well as runoff across Svalbard under past and future climates (van Pelt et al 2019;Schuler et al 2020 and references therein;Schmidt et al 2023). Of highest importance for snow model calibration and validation are in situ measurements of snow accumulation at glacier mass-balance stakes and of snow/firn density and temperature (e.g., Taurisano et al 2007;Laska et al 2022), as well as weather station records of air temperature and, most importantly, precipitation (snowfall and rainfall). Remote or in situ observations of snow albedo are also critical for accurate estimation of glacier surface energy balance and melt rates.…”