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- W8040092 abstract "Short wave radiation penetrates the top portion of the snowpack and is responsible for both sub-surface heating and fast changing temperature gradients during daytime. This affects snow meta- morphism and hence weak layer formation and can affect mechanical properties of deeper layers. It is thus of crucial importance that snow-cover models represent this process as realistically as possible. Carefully measured near-surface snow temperatures can be used to check model performance in this re- spect. Numerical simulations performed with the Swiss snow-cover model SNOWPACK are thus com- pared to short time series of temperature measurements taken in the top 40 cm of the snowpack on a knoll located in the Columbia Mountains of British Columbia, Canada. In contrast to simpler models, SNOWPACK treats short wave radiation as a volume source of heat, like refreezing. It is shown that a multi-band approach is needed to obtain the best results. Switching off short wave radiation on a sunny day results in a reduction of temperature increase of about 5.2 °C at 15:00 at 10 cm depth while differ- ences below 30 cm are negligible even later in the day." @default.
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- W8040092 date "2008-09-23" @default.
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- W8040092 title "MODELING SHORT WAVE RADIATION PENETRATION INTO THE SNOWPACK: WHAT CAN WE LEARN FROM NEAR-SURFACE SNOW TEMPERATURES?" @default.
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