Processed sensible and latent heat flux, friction velocity and stability at EastGRIP site on Greenland Ice Sheet

Processed 30 minute surface sensible and latent heat flux measured at 180cm 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. Friction velocity and Monin-Obukhov stability parameter estimates are provided for convenience. The integration time was 10 minutes which was averaged to 30 minute resolution with the timestamps indicating the beginning of the 30 minute averaging period.