“…Few studies exist that have directly measured turbulent fluxes over mountain glaciers, and all of these studies are restricted to shorter time intervals, e.g., weeks to a couple of months (e.g., Munro, 1989;Forrer and Rotach, 1997;van der Avoird and Duynkerke, 1999;Cullen et al, 2007;Guo et al, 2011;Conway and Cullen, 2013). A more common approach in the studies of SEB on glaciers is to derive the turbulent fluxes through parameterization schemes that utilize the observations of mean meteorological variables such as near-surface air temperature, wind, and relative humidity (e.g., Hock and Holmgren, 2005;Sicart et al, 2005;Mölg et al, 2008;Reijmer and Hock, 2008;Mölg et al, 2009;MacDougall and Flowers, 2011;Sicart et al, 2011;Huintjes et al, 2015;Prinz et al, 2016). The simplest and most widely applied method is the bulk aerodynamic method (bulk method) (e.g., Braithwaite et al, 1998;Oerlemans, 2000).…”