Processed 30 minute surface sensible and latent heat flux measured at 180 cm above snow surface. The eddy covariance system included a Campbell Scientific CSAT3 and a Krypton Hygrometer KH20 which were directed into the mean wind. The latent heat flux was calculated assuming a latent heat of sublimation of 2835 J/g snow. The integration time was 10 minutes which was averaged to 30 minute resolution.
The timestamp refers to the first of the three 10 minute intervals (cf dataset doi:10.1594/PANGAEA.961156), which have been taken for the 30 minute averaging period.