Processed sensible and latent heat flux, friction velocity and stability at EastGRIP site on Greenland Ice Sheet
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| Auteurs principaux: | , , , |
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2022
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| _version_ | 1867171033385009152 |
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| author | Steen-Larsen, Hans Christian Wahl, Sonja Box, Jason E Hubbard, Alun L |
| author_facet | Steen-Larsen, Hans Christian Wahl, Sonja Box, Jason E Hubbard, Alun L |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_946741 |
| institution | PANGAEA |
| language | en |
| publishDate | 2022 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Processed sensible and latent heat flux, friction velocity and stability at EastGRIP site on Greenland Ice Sheet Steen-Larsen, Hans Christian Wahl, Sonja Box, Jason E Hubbard, Alun L DATE/TIME; East Greenland Ice-core Project; Eddy-Covariance; EGRIP; EGRIP_camp; Friction velocity; Greenland; Greenland ice sheet; Heat, flux, latent; Heat, flux, sensible; latent and sensible heat; MULT; Multiple investigations; Signals from the Surface Snow: Post-Depositional Processes Controlling the Ice Core Isotopic Fingerprint; SNOWISO; Stability 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. |
| title | Processed sensible and latent heat flux, friction velocity and stability at EastGRIP site on Greenland Ice Sheet |
| topic | DATE/TIME; East Greenland Ice-core Project; Eddy-Covariance; EGRIP; EGRIP_camp; Friction velocity; Greenland; Greenland ice sheet; Heat, flux, latent; Heat, flux, sensible; latent and sensible heat; MULT; Multiple investigations; Signals from the Surface Snow: Post-Depositional Processes Controlling the Ice Core Isotopic Fingerprint; SNOWISO; Stability |
| url | https://doi.org/10.1594/PANGAEA.946741 |