Includes selected variables for the Langtang catchment of the WRF run used in Contrasting meteorological drivers of the glacier mass balance between the Karakoram and central Himalaya, by PNJ Bonekamp, RJ de Kok, E Collier and WW Immerzeel. WRF version 3.8.1 is used for the simulations. The outer domain is forced with 6-hourly ERA-Interim data (0.75 o x0.75o), and grid analysis nudging is applied to the horizontal wind, water vapour mixing ratio and potential temperature fields in the highest 15 vertical levels. In all domains, the land cover dataset is updated using the climate change initiative dataset (CCI, Defourny et al. (2017)) of the European Space Agency (ESA), which has a spatial resolution of 300 m. The soil moisture, soil temperatures and skin temperatures is initialized with the GLDAS dataset (0.25x0.25, Rodell et al. 2004). Important parameter settings are: - One way nesting - Model top pressure - Morrison microphysics -YSU planetary boundary layer scheme wit topo_wind option=1 - Noah-MP scheme -RRTGM radiation scheme -MM5 Similarity Scheme - Rayleigh damping at the top boundary - Diffusion is calculated in physical space Included variables [unit']: Time [hours from 1 December 2010], total simulation time is till 1 January 2014. All data are hourly variables. ALBEDO [-] GLW [Wm-2], longwave downward radiation GRAUPELNC [m], non convective graupel GRDFLX [Wm-2], ground heat flux HFX [Wm-2], Sensible heat flux HGT [m], altitude above sea level LH [Wm-2], latent heat flux LU_INDEX [-] #24 categories LWDNB [Wm-2], longwave downward radiation LWUPB [Wm-2], longwave upward radiation RAINC [m], convective rainfall RAINNC [m], non convective rainfall SNOWC [-], snow cover SNOWNC [-], non convective snowfall SWDOWN [Wm-2], shortwave downwards radiations T2 [K], 2-meter temperature TSK [K], surface temperature U10 [ms-1], wind in U-direction at 10-m V10 [ms-1], wind in V direction at 10-m See for the full description of the variables Chapter 5 of the WRF user guide