A method for including night-time refreezing of the top layer of a snowpack in the degree-day method for computing daily snowmelt rates is presented. It is found that during days of large diurnal temperature variations the daily melt is more determined by the day-time conditions than by the daily mean conditions. Applications are made to an open area and a forested area. The refreezing-degree-day method is found to describe the snowmelt process very well, whereas the simple degree-day method shows a too fast snowmelt rate.
Research Article|February 01 1982
The Importance of Refreezing on the Diurnal Snowmelt Cycle with Application to a Northern Swedish Catchment
Lars Bengtsson; The Importance of Refreezing on the Diurnal Snowmelt Cycle with Application to a Northern Swedish Catchment. Hydrology Research 1 February 1982; 13 (1): 1–12. doi: https://doi.org/10.2166/nh.1982.0001
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